Paso Yo Bai 43101

NI 43-101 TECHNICAL REPORT ON PASO YOBAI PROJECT, DEPARTMENT GUAIRA, PARAGUAY

PREPARED FOR LATIN AMERICAN MINERALS INC.

FEBRUARY 15, 2008

D. GEORGE CARGILL, PH.D., P.ENG. CONSULTING GEOLOGICAL ENGINEER CARGILL CONSULTING GEOLOGISTS LIMITED SUITE 501, 55 UNIVERSITY AVE., TORONTO, ON M5J 2H7 CANADA

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TABLE OF CONTENTS PAGE

1 SUMMARY.................................................................................................................................................1 EXECUTIVE SUMMARY.........................................................................................................................1

INTRODUCTION ..................................................................................................................................1 INTERPRETATION AND CONCLUSIONS...........................................................................................2 RECOMMENDATIONS.........................................................................................................................3

TECHNICAL SUMMARY ........................................................................................................................4 PROPERTY DESCRIPTION AND LOCATION.....................................................................................4 HISTORY ...............................................................................................................................................5 GEOLOGY.............................................................................................................................................6

2 INTRODUCTION AND TERMS OF REFERENCE .............................................................................9 SOURCES OF INFORMATION................................................................................................................9 LIST OF ABBREVIATIONS ...................................................................................................................10

3 RELIANCE ON OTHER EXPERTS .....................................................................................................11 4 PROPERTY DESCRIPTION AND LOCATION .................................................................................12

MINERA GUAIRA EXPLOITATION CONCESSION (MINING LEASE) ...........................................12 MINAS PARAGUAY EXPLOITATION CONCESSION (MINING LEASE)........................................12 EXPLORATION PERMITS.....................................................................................................................13 MINING LAW AND TAXATION...........................................................................................................15

5 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY ......................................................................................................................................17

ACCESSIBILITY.....................................................................................................................................17 CLIMATE ................................................................................................................................................17 LOCAL RESOURCES .............................................................................................................................17 INFRASTRUCTURE ...............................................................................................................................18 PHYSIOGRAPHY ...................................................................................................................................18

6 HISTORY..................................................................................................................................................18 7 GEOLOGICAL SETTING......................................................................................................................19

REGIONAL GEOLOGY..........................................................................................................................20 LOCAL GEOLOGY.................................................................................................................................20 PROPERTY GEOLOGY..........................................................................................................................23

8 DEPOSIT TYPES.....................................................................................................................................26 9 MINERALIZATION ...............................................................................................................................29

QUARTZ-SULPHIDE AU-STYLE MINERALIZATION ......................................................................29 EPITHERMAL QUARTZ-CARBONATE AU-MN-STYLE LOW SULPHIDATION MINERALIZATION................................................................................................................................29

10 EXPLORATION ....................................................................................................................................30 SATELLITE IMAGERY..........................................................................................................................32 HELICOPTER EM AND MAGNETIC SURVEY ...................................................................................32 MAGNETIC SURVEY ............................................................................................................................32 VERSATILE TIME DOMAIN ELECTRO MAGNETIC (“VTEM”) SURVEY......................................34 MINERALIZATION IN THE PITS .........................................................................................................36 SOIL GEOCHEMICAL SURVEY...........................................................................................................39

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11 DRILLING..............................................................................................................................................42 12 SAMPLING METHOD AND APPROACH ........................................................................................55

SOIL SAMPLES.......................................................................................................................................55 ROCK CHIP SAMPLES...........................................................................................................................55 DRILL CORE SAMPLES ........................................................................................................................55

13 SAMPLE PREPARATION, ANALYSES AND SECURITY .............................................................56 SOIL SAMPLES.......................................................................................................................................56 ROCK CHIP SAMPLES...........................................................................................................................56 DRILL CORE SAMPLES ........................................................................................................................57

METALLIC OR SCREEN FIRE ASSAYS .............................................................................................57 14 DATA VERIFICATION........................................................................................................................57 15 ADJACENT PROPERTIES..................................................................................................................60 16 MINERAL PROCESSING AND METALLURGICAL TESTING...................................................60 17 MINERAL RESERVE ESTIMATES...................................................................................................60 18 RELEVANT DATA AND INFORMATION .......................................................................................61 19 INTERPRETATION AND CONCLUSIONS ......................................................................................61 20 RECOMMENDATIONS .......................................................................................................................62 21 REFERENCES .......................................................................................................................................66 22 SIGNATURE PAGE ..............................................................................................................................68 23 CERTIFICATE OF QUALIFICATIONS............................................................................................69

D. GEORGE CARGILL........................................................................................................................69 APPENDIX 1 ............................................................................................................................................. 1-1

COMPLETE DRILL HOLE GOLD ASSAYS ....................................................................................... 1-1 APPENDIX 2 ............................................................................................................................................. 2-1

EXAMPLES OF DRILL LOGS.............................................................................................................. 2-1

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LIST OF TABLES PAGE

PHASE ONE PROGRAM...............................................................................................................................3 PHASE TWO PROGRAM..............................................................................................................................4 TABLE 7.1 STRATIGRAPHY EASTERN PARAGUAY ..........................................................................23 TABLE 10.1 EXPLORATION EXPENDITURES 2007............................................................................30 TABLE 10.2 SIGNIFICANT ROCK CHIP SAMPLES .............................................................................38 TABLE 10.3 DESCRIPTIVE STATISTICS OF THE SOIL SAMPLE DATABASE ...............................41 TABLE 11.1 DIAMOND DRILL HOLE COORDINATES.......................................................................43 TABLE 11.2 SIGNIFICANT DIAMOND DRILL ASSAYS .....................................................................43 TABLE 14.1 CARGILLS SAMPLES FROM PITS....................................................................................59 TABLE 14.2 CARGILL’S RE-ASSAY OF DRILL CORE........................................................................59 TABLE 14.3 CARGILL’S RE-ASSAY OF PULPS ...................................................................................60 TABLE 20.1 PHASE ONE PROGRAM.....................................................................................................63 TABLE 20.2 PHASE TWO PROGRAM....................................................................................................64

LIST OF FIGURES PAGE

FIGURE 4.1 LOCATION MAP..................................................................................................................14 FIGURE 4.2 MINERAL TITLE..................................................................................................................16 FIGURE 7.1 EASTERN PARAGUAY GEOLOGY...................................................................................21 FIGURE 7.2 PARAGUAY MINERAL OCCURRENCES.........................................................................22 FIGURE 7.3 REGIONAL GEOLOGY .......................................................................................................25 FIGURE 8.1 EXPLORATION MODEL.....................................................................................................28 FIGURE 10.1 SOIL IKONOS AND GEOPHYSICS LOCATION MAP...................................................31 FIGURE 10.2 REDUCED TO POLE MAGNETIC MAP ..........................................................................33 FIGURE 10.3 SHALLOW CONDUCTOR EM ANOMALY MAP...........................................................35 FIGURE 10.4 ROCK CHIP SAMPLES......................................................................................................37 FIGURE 10.5 SOIL SAMPLING PROGRAM...........................................................................................40 FIGURE 11.1 DRILL HOLE LOCATION MAP .......................................................................................46 FIGURE 11.2 DIAMOND DRILL HOLES LAT-1, LAT-2.......................................................................47 FIGURE 11.3 DIAMOND DRILL HOLES LAT-3, LAT-4, LAT-5..........................................................48 FIGURE 11.4 DIAMOND DRILL HOLES LAT-6, LAT-7.......................................................................49 FIGURE 11.5 DIAMOND DRILL HOLE LAT-8 ......................................................................................50 FIGURE 11.6 DIAMOND DRILL HOLE LAT-9 ......................................................................................51 FIGURE 11.7 DIAMOND DRILL HOLE LAT-10 ....................................................................................52 FIGURE 11.8 DIAMOND DRILL HOLE LAT-11 ....................................................................................53 FIGURE 11.9 DIAMOND DRILL HOLE LAT-12 ....................................................................................54 FIGURE 14.1 ASSAYS OF A STANDARD SAMPLE .............................................................................58 FIGURE 14.2 THOMPSON AND HOWATH PLOT OF DUPLICATE ASSAYS ...................................58 FIGURE 20.1 RECOMMENDED DRILL HOLES – PHASE ONE ..........................................................65

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1 SUMMARY EXECUTIVE SUMMARY

INTRODUCTION Cargill Consulting Geologists Limited (Cargill) was retained by Mr. David Wahl,

President and CEO of Latin American Minerals Inc (the “Company”), to prepare a report on the PasaoYobai property (the “Property”) located about 150 km southeast of Asuncion, Paraguay. This report is entitled “NI-43-101 Technical Report on Paso Yobai Property, Department Guaira, Paraguay” and dated February 15, 2008. Technical Report conforms to Canadian NI 43-101 Standards of Disclosure for Mineral Projects.

Latin American Minerals Inc. is an exploration company working in Argentina,

Paraguay and Colombia. It does not have any mine production or advanced stage projects at the present time.

The Paso Yobai Property is an early stage exploration project with surface

geochemical surveys, airborne geophysical surveys and twelve holes drilled prior to December 31, 2007. There has been some artisanal production from several pits and a little mechanical production from other pits, all located on the Property. There has never been a resource estimate for any of these pits and production records are poor to non-existent.

Cargill has not had any prior involvement with the Property, except for two site visits

in support of this report. This report is considered by Cargill to meet the requirements of a Preliminary

Assessment as defined in NI 43-101 regulations. The Property is an early stage exploration project and there is no inferred resource estimated for any of the pits on the Property.

Site visits were carried out by D. George Cargill from October 2 to 4, 2007 and

February 6 to 7, 2008. The information contained in this report is based on information on file in the public

domain including, but not restricted to, Government of Paraguay maps and publications, limited historic data provided from the Property owners, and on data generated by the Company as a result of exploration completed on the Property over the past year. The data collection and compilation was completed by professional geologists and or exploration technicians under the direction of Dr. Perez, P.Geo., the Company’s “Qualified Person” as defined by NI 43-101.

D. George Cargill prepared all parts of this report.

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INTERPRETATION AND CONCLUSIONS 1) Artisanal mining has demonstrated a large zone of gold mineralization in soils and

weathered rocks, on the Property.

2) Geophysical, geochemical, and geological exploration has demonstrated gold mineralization on the Property is related to:

a) A zone of mafic (basalt) dykes (the “Dyke Zone”). b) The Dyke Zone is bounded and cut by faults parallel to the strike and offset

by faults at a high angle to the strike of the zone. c) The Paso Yobai Gold Zone (the “Main Gold Zone”) has been traced 6.5 km

by soil geochemistry and airborne magnetics and is variably exposed on surface by artisan miners for 3.6 km. Very high gold values in soil geochemistry mark the Main Gold Zone, which corresponds to a linear zone of high magnetic values, bounded by zones of low magnetic values.

d) The aeromagnetic and soil surveys show magnetic anomalies with corresponding gold anomalies parallel to the Main Gold Zone, which suggest parallel mineralized dykes.

e) The distribution of the parallel magnetic anomalies, which are interpreted to be dykes, may be controlled by structures at a high angle to the Main Gold Zone.

f) EM anomalies also parallel the Dyke Zone. These EM anomalies are interpreted as derived from deep sources, and are tentatively interpreted as derived from deep-seated bodies of sulphides.

g) Rock samples from the artisanal mine workings indicate gold mineralization is related to quartz veins in altered mafic dyke and altered (silicified) sandstone near the contacts of the dyke.

h) Gold in the artisanal workings appears controlled by post dyke structures. i) Gold occurs in veins associated with sulphides (pyrite) and as coarse

grained, free gold in veins without sulphides. j) Bonanza grades occur when the sulphide-free veins with visible gold are

superimposed on the veins containing pyrite. k) Paso Yobai has many similar characteristics to several large gold and

copper deposits associated with alkaline rocks, such as Porgera, Cripple Creek, Ladolam, and Palabora.

3) The initial drill program of 12 holes totalling 1,989.2 m, has indicated:

a) The dyke ranges from 5 to 40 m thick and continues to at least 100 m depth.

b) Gold occurs in an altered dyke and sandstones controlled by structural zones, breccias, veins, stock-works within the dyke, and within the altered sandstones near the contact of the dyke.

c) Coarse grained free gold giving bonanza assays has been found to depths of about 100 m, which suggests that much of the free gold is primary.

4) Drilling on the aeromagnetic and soil geochemical anomalies has demonstrated

that the gold mineralization is related to carbonate-quartz veins cutting the mafic

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dyke, and altered sandstones near the contact of the dyke. The gold mineralization including the bonanza grades continues to depths of ±100 m.

5) Although there are only 12 widely spaced drill holes, higher grade, gold

mineralization appears related to variations in the position of the dyke along strike that appear to be dilation zones. The current data indicates that the primary targets in the Main Gold Zone are plunging shoots of structurally controlled gold mineralization.

6) The initial work on the parallel aeromagnetic and soil geochemical gold anomalies

suggests that they are similar to the Main Gold Zone and controlled by structures at a high angle to the Main Gold Zone.

7) The parallel zones present targets similar to those on the Main Gold Zone.

However, multiple parallel zones close to the Main Gold Zone, or to each other, could constitute a target of a large volume of structurally controlled gold mineralization.

RECOMMENDATIONS Cargill recommends a two-phase exploration program with the scope and extent of

the second phase contingent on the results of the first phase.

1) The first phase of the exploration will consist of drilling the remaining drill targets (3,000 m) (Figure 20.1) and carrying out soil geochemistry, geology and trenching both to infill the existing grid and to extend the grid to the east and west to explore parallel dyke systems, summarized as follows.

PHASE ONE PROGRAM

Salaries and fees $150,000

Soil sampling 6,000 samples $50,000

Geochemistry and assaying $80,000

Drilling to complete testing of the established drill targets

3,000 m $550,000

Reporting $20,000

Subtotal $850,000.00 Contingencies 10% $85,000

Total $935,000

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2) The current information indicates a second phase of exploration is warranted. However, the exact scope of work will be based on the results of the Phase One Program. As currently envisioned, the Phase Two Program will consist of:

a) Geochemistry, trenching and mapping to better define the parallel dykes and to extend the Main Gold Zone along strike.

b) Drilling to test new targets developed on the parallel zones and along strike on the Main Gold Zone. Approximately 5,000 m of drilling will be required.

c) Definition drilling on the two best zones within the Main Gold Zone. Cargill estimates that about 12 drill sections with about 5,000 m of drilling will be required to test each zone.

PHASE TWO PROGRAM


Soil sampling 4,000 samples $45,000


Drilling to complete testing of the established drill targets

15,000 m $2,700,000

Reporting $50,000

Subtotal $3,395,000.00 Contingencies 10% $339,,500

Total $3,734,500

TECHNICAL SUMMARY

PROPERTY DESCRIPTION AND LOCATION The Paso Yobai Property is located in south central Paraguay, approximately 150 km

southeast of Asuncion (Figure 4.1). The Property consists of two exploitation concessions and four exploration concessions covering an aggregate total of 15,332 ha. The exploitation (mining) concessions, covering 7,200 ha are owned by two private companies, Minera Guaira and Minas Paraguay, but held under an option agreement with the Company. The Company has received approval for exploration concession Rio Verde (1,332 ha) and is awaiting approval of the remaining three exploration concessions covering 6,800 ha. On approval the Company will hold a 100% interest in the exploration concessions.

MINERA GUAIRA EXPLOITATION CONCESSION (MINING LEASE)

The Minera Guaira Mining Lease covers 6,700 ha and was granted by the Republic of Paraguay in 2003 pursuant to its individual Act 2.079/03 (the “Guaira Mining Lease”).

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On February 17, 2007, the Company signed the Contract of Option to Purchase Mining Lease Rights with Minera Guaira S.A. (“Minera Guaira”) as amended on April 18, 2007 and February 5, 2008; which gives, the Company the option to earn a 70% interest in the Guaira Mining Lease by paying escalating cash payments totalling US$2.1 million over 3 years, expending US$500,000 on exploration in Year 1 plus the delivery of 100,000 shares of the Company to Minera Guaira. The Febraury 5, 2008 amendment provided for satisfaction of the $100,000 cash payment due by April 1, 2008 by issuing 114,149 common shares of the Company. On vesting of the 70% interest, a joint venture will be formed. Under the joint venture, if Minera Guaira’s participating interest drops to 15%, 14% of said interest converts to a 3% NSR.

Minera Guaira has been granted an environmental license, required for production,

that is valid through July 2009; however, the Company has temporarily suspended production to fully evaluate the resource of the Guaira Mining Lease.

MINAS PARAGUAY EXPLOITATION CONCESSION (MINING LEASE)

The Minas Paraguay Mining Lease covers 500 ha and was granted by the Republic of Paraguay in 2001 pursuant to its individual Act 1.708/01 (“Minas Mining Lease”). On February 17, 2007 the Company signed the Contract of Option to Purchase Mining Lease Rights with Minas Paraguay S.A. (“Minas Paraguay”) as amended on April 18, 2007, which gives the Company the option to earn a 70% interest in the Minas Mining Lease by paying escalating cash payments totalling US$2.0 million over 3 years, expending US$ 750,000 on exploration over 2 years plus delivering US$ 50,000 in common shares of the Company. On vesting of the 70% interest, a joint venture will be formed and if Minas Paraguay’s participating interest drops to 5%, 4% of said interest converts to a 10% NPI.

Minas Paraguay has been granted an environmental license, required for production,

and exploration through to July 2009. The Company has temporarily suspended production to fully evaluate the resource of the Minas Mining Lease.

EXPLORATION PERMITS

During 2007, the Company dropped several exploration permits, received approval for exploration concession Rio Verde (1,332ha) and submitted application for three new exploration concessions: Block A (4,000ha), Block B (500ha) and Block C (2,300ha). The total area of the exploration concessions under application is 6,800 ha. As of the date of this report approval for the three exploration concession is pending.

The Company holds all permits required to carry out the proposed exploration

on the Properties.

HISTORY The largest reported exploration property in the Paraguay program was between 1978

and 1982 when the Anschutz Corporation carried out an exploration program in the Parana Basin for Colorado Plateau type uranium deposits. After spending about $25 million dollars, Anschutz stopped the program. Recently other companies have been

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acquiring exploration concessions in Paraguay to cover the uranium anomalies defined by Anschutz.

In the late 1990s, Yamana Resources explored for gold in the alkaline rocks of

Paraguay and drilled a prospect about 50 km east of Paso Yobai but abandoned the claims and left the county.

Work done on the Property consists of:

1996 - Original discovery of the gold occurrence on the Minas Paraguay property by Daniel Benitez.

2001 - Daniel Benitez staked ground and hired a geologist, Juan Carlos Benitez, no

relation. 2002 - Juan Carlos Benitez wrote a geological report summarizing his surface work

and Beitez sold 78% of the property to Ortellado, a construction company. Ortellado purchased a gravity mill in Brazil and used a backhoe and trucks to open up an area 1.2 km long, 20 to 40 m wide, and 5 to 50 m deep on top of the main dyke. Production is not documented but a mine production of 150 oz/month is reported but not supported. Ortellado did no grade or process control and did not assay the ore or the tailings.

2002 - Ortellado hired Dr. Schalamuk from La Plata University in Argentina. He

described the deposits exposed in the pits and did some geochemical sampling. He recommended magnetic and resistivity surveys.

2002 - Sr. Iske completed a magnetometer survey on the adjacent Minera Guaira

Property and mapped the exposures in the pits. 2003 - Sr. Tessone from the La Plata University Group reported the results of the

magnetometer survey that mapped the dike. 2007 - The Company optioned the Minera Guaira Mining Lease and the Minas

Paraguay Mining Lease. 2007 - The Company began the first modern exploration program on the Property .

GEOLOGY Paraguay’s geological framework consists of three cratons ranging in age from 3,800

to 2,700 Ma, composed of gneisses, granulites and greenstone belts, surrounded by 950-550 Ma old metamorphic rocks broadly referred to as the Brazilian Shield. These rocks are covered by intra-cratonic red beds of Carboniferous and Permian age. The geologic evolution of Paraguay to this point was related to the Gondwana Super Continent. With the beginning of the break-up of Gondwana in the Mesozoic, northwest rifts were generated in Eastern Paraguay and related basins filled with Triassic and Jurassic, fluvial and aeolian sandstones. The sedimentary units are intruded by two mafic units: the Alto

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Parana Magmatic Suite and the Sapucai Magamatic Suite. Both units intrude as dikes, sills and extrusive rocks along northwest regional structures. The Sapucai Suite is alkali while the Alto Parana Suite is tholeitic. Radiometric ages for the Sapucai Suite range from 165 Ma to 115 Ma.

The Paso Yobai area is covered by Carboniferous and Permian sediments that outcrop

20 km to the northwest. They are covered by sub-horizontal, Triassic-Jurassic, red, aeolian sandstones with local layers of mudstones. Three mafic units intrude the sedimentary rocks: 1.) Tholeitic-alkalic basalts; 2.) Alkalic basalts of the Sapucai Suite; and 3.) Mafic dikes. As the distinction between tholeitic and alkaline basalts is based on the K20 content; it is difficult to establish which are alkalic and which tholeiitic in the field. However, all intrusive rocks are intruded along northwest structures, which were part of the Mesozoic rifting process.

The Property displays Mesozoic north-south, northwest and northeast elements in the

structural grain, possibly projected through the cover sequence from the underlying older basement. The northwest structures are interpreted to have been active as extensional structures and the northeast as orthogonal fractures during the Cretaceous opening of the Atlantic Ocean. Deep crustal fractures could tap deep mafic intrusion source rocks for gold mineralization.

The mafic dyke and its enclosed mineralization occur in a synistral normal fault as

evidenced by sub-horizontal slickensides in the vicinity of the flexures. Where steep slickensides are recognized on surface, mineralization seems to improve or at least visible gold seems to be more common.

Based on outcrop and drilling data the northwest trending mafic dykes apprear to dip

to the northeast. In addition to the dykes, a pencil-shaped stock on the Property is believed to occur at

the Cerro Mboy occurrence, where a knob like feature results from erosion of marginally softer, kaolin-pyrite (FeO) altered rocks. The scree of mafic rock rich in spherulites is typical of material developed by the concentration of volatiles in the uppermost portion of a blind magma chamber. Marginal silicified sandstones contain well-developed quartz veins, changing to quartz filled breccias at the top of the hill. These features are typical of alteration associated with a buried intrusion.

Gold mineralization occurs in association with the northwest trending, mafic dikes

interpreted as filling pre-existing structures active as normal faults. In detail the northwest dike trend is disturbed by small-scale structures that have:

• Local dextral offsets in dyke segments on intervening north-south cross faults.

• Better gold mineralization occurring where the northwest structures display

flexures to the west-northwest to east-west, or where veins following this trend overprint the general northwest structures.

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• More steeply dipping fault zones displaying better gold mineralization evidenced by more extensive open space, quartz-crystal growth.

High-grade gold shoots occur as flexures where the dikes trend more towards the

west. These vein portions generally dip more steeply which is typical of a dilatant setting in normal faults.

While most slickensides on faults within the mineralized structural corridor are sub-

vertical near the flexures, inclined slickensides occur. The environment is characterized by overall normal fault extension, with local components of strike-slip faulting. The localized sinistral, strike-slip, fault movement is responsible for the development of mineralized shoots in fault flexures and the shoots are interpreted to dip (plunge?) steeply. Normal fault activation would provide flat plunging shoots within the steep dipping fault portions, and inclined shoots could result from mixed components of dip-slip and strike-slip fault activation.

Corbett (2007) identified two types of vein mineralization in Paso Yobai: quartz-

sulphide gold-style mineralization and epithermal quartz-carbonate gold-manganese with low sulphidation mineralization.

QUARTZ-SULPHIDE AU-STYLE MINERALIZATION

Quartz-sulphide gold-(Au)-style mineralization commonly forms early in the paragenetic sequence of the development of intrusion-related gold deposits and comprises gold within crystalline pyrite. Drill holes demonstrate that mineralization in these veins contains high pyrite, kaolin and smectite.

EPITHERMAL QUARTZ-CARBONATE AU-MN-STYLE LOW SULPHIDATION MINERALIZATION

At Paso Yobai epithermal mineralization comprises several mm wide open carbonate, mangano-calcite and minor quartz veins, veinlets and stockworks. These veins are best developed as sheeted veins in the dilatant structural zones defined by west-northwest flexures in the northwest structural corridor. Better developed open carbonate veins are also apparent at outcrop scale on steeper dipping portions of moderately dipping faults. Minor, open-space breccias lined with fine-crystalline pyrite are interpreted to represent mineralization of this type. Many quartz-MnO veins contain wire like free gold growing in open space. These veins are associated with bonanza Au grades, commonly overprinting earlier auriferous pyrite.

The Paso Yobai Gold Project has many similar characteristic of several large gold and

copper deposits associated with alkaline rocks, such as Porgera, Cripple Creek, Ladolam, and Palabora (Corbett, 2007).

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2 INTRODUCTION AND TERMS OF REFERENCE

Cargill Consulting Geologists Limited (Cargill) was retained by Mr. David Wahl, President and CEO of Latin American Minerals Inc. (the “Company”), to prepare a report on the Pasao Yobai property (the “Property”) 150 km southeast of Asuncion, Paraguay. This report is entitled “NI-43-101 Technical Report on Paso Yobai Property, Department Guaira, Paraguay” (the “Property”) and dated February 15, 2008. The Technical Report conforms to Canadian NI 43-101 Standards of Disclosure for Mineral Projects.

The Company is an exploration company working in Argentina, Paraguay and

Colombia. It does not have any mine production or advanced stage projects at the present time.

The Property is an early stage exploration project. There has been surface mapping,

rock sampling, geochemical and airborne geophysical surveys. There have also been 12 holes drilled to December 31, 2007. There has been some artisanal production from several pits on the Property and a little mechanical production from other pits. However, there has never been a resource estimate for any of the pits on the Property and production records are practically nonexistent.

Cargill has not had any prior involvement with the Property, except for two site visits

in support of this report. This report is considered by Cargill to meet the requirements of a Preliminary

Assessment as defined in Canadian NI 43-101 regulations. The Property is an early stage exploration property with no resource estimated for any of the pits.

SOURCES OF INFORMATION

The information contained in this report is based on information on file in the public domain including, Government of Paraguay maps and publications, limited historic data provided from the Property owners and data generated by the Company as a result of exploration completed on the Property over the past year. The data collection and compilation was completed by professional geologists and exploration technicians under the supervision of Mr. Juan Carlos Benitez, General Manager Latin American Minerals Paraguay S.A. and Dr. Waldo Perez, the Company’s “Qualified Person”. The documentation reviewed, and other sources of information, are listed at the end of this report in References.

Discussions were held with the following personnel from Latin American Minerals

Inc.

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• Mr. David G. Wahl, “Engineer of Mines”, P. Eng., P.Geo., President, CEO and Director.

• Dr. Waldo Perez, Ph.D. Sr. Vice President of Exploration and Director. • Mr. Juan Carlos Benitez, B.Sc., General Manager, Paraguay. • Carlos Gustavo Fernandez, M.Sc., Sr. Geologist. • Mina Medina, B.Sc. Senior Geologist.

D. George Cargill prepared all parts of this report. Dr. Cargill visited the Property on

October 4 to 6, 2007 and February 6 to 7, 2008.

LIST OF ABBREVIATIONS

Units of measurement used in this report conform to the SI (metric) system. All currency in this report is American dollars ($) unless otherwise noted.

μ Micron kPa kilopascal

°C degree Celsius kVA kilovolt-amperes

°F degree Fahrenheit kW kilowatt

μg Microgram kWh kilowatt-hour

A Ampere L liter

A Annum L/s litres per second

Bbl Barrels M metre

Btu British thermal units M mega (million)

C$ Canadian dollars m2 square metre

Cal Calorie m3 cubic metre

Cfm cubic metres per minute Min minute

Cm Centimeter MASL metres above sea level

cm2 square centimeter Mm millimetre

D Day Mph miles per hour

dia. Diameter MVA megavolt-amperes

Dmt dry metric tone MW megawatt

Dwt dead-weight ton MWh megawatt-hour

Ft Foot m3/h cubic metres per hour

ft/s foot per second opt, oz/st ounce per short ton

ft2 square foot Oz Troy ounce (31.1035g)

ft3 cubic foot oz/dmt ounce per dry metric tonne

G Gram Ppm part per million

G giga (billion) Psia pound per square inch absolute

Gal Imperial gallon Psig pound per square inch gauge

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g/L gram per litre RL relative elevation

g/t gram per tone S second

Gpm Imperial gallons per minute St short ton

gr/ft3 grain per cubic foot Stpa short ton per year

gr/m3 grain per cubic metre Stpd short ton per day

Hr Hour T metric tonne

Ha Hectare Tpa metric tonne per year

Hp Horsepower Tpd metric tonne per day

In Inch US$ United States dollar

in2 square inch USg United States gallon

J Joule USgpm US gallon per minute

K kilo (thousand) V volt

Kcal Kilocalorie W watt

Kg Kilogram Wmt wet metric tonne

Km Kilometer yd3 cubic yard

km/h kilometre per hour Yr year

km2 square kilometer

3 RELIANCE ON OTHER EXPERTS This report has been prepared by Cargill Consulting Geologists Limited (Cargill) for

the Company. The information, conclusions, opinions, and estimates contained herein are based on:

• Information available to Cargill at the time of preparation of this report,

• Assumptions, conditions, and qualifications as set forth in this report, and

• Data, reports, and other information supplied by the Company and other third party sources.

For the purpose of this report, Cargill has relied on ownership information provided

by the Company. Cargill has not researched Property title or mineral rights for the Paso Yobai Project and expresses no legal opinion as to the ownership status of the Property.

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4 PROPERTY DESCRIPTION AND LOCATION The Paso Yobai Property is in south central Paraguay, about 150 km southeast of

Asuncion (Figure 4.1). The Propery consists of two mining leases and four exploration concessions covering approximately 15,332 ha (Figure 4.2). The exploitation (mining) concessions are owned by two private companies Minera Guaira and Minas Paraguay, but held under option by the Company. The Company has received approval for exploration concession Rio Verde (1,332ha) and has submitted applications to acquire three (3) exploration concessions which, on approval will be wholly owned by the Company.

MINERA GUAIRA EXPLOITATION CONCESSION (MINING LEASE)

The Minera Guaira Mining Lease covers 6,700 ha and was granted by the Republic of Paraguay in 2003 pursuant to its individual Act 2.079/03 (the “Guaira Mining Lease”). On February 17, 2007, the Company signed the Contract of Option to Purchase Mining Lease Rights with Minera Guaira S.A. (“Minera Guaira”) as amended on April 18, 2007 and February 5, 2008; which gives the Company the option to earn a 70% interest in the Guaira Mining Lease by paying escalating cash payments totalling US$2.1 million over 3 years, expending US$500,000 on exploration in Year 1 plus the delivery of 100,000 shares of the Company to Minera Guaira. The Febraury 5, 2008 amendment provided for satisfaction of the $100,000 cash payment due by April 1, 2008 by issuing 114,149 common shares of the Company. On vesting of the 70% interest, a joint venture will be formed. Under the joint venture, if Minera Guaira’s participating interest drops to 15%, 14% of said interest converts to a 3% NSR.

The Company has filed the required Quarterly Reports and paid Annual Canon Fees

totalling $3,400. On or before the first anniversary of the Agreement the Company will have spent more than the $500,000 required on exploration.

Minera Guaira has been granted an environmental license, required for production,

that is valid through July 2009; however, the Company has temporarily suspended production to fully evaluate the resource of the Mining Lease.

MINAS PARAGUAY EXPLOITATION CONCESSION (MINING LEASE)

The Minas Paraguay Mining Lease covers 500 ha and was granted by the Republic of Paraguay in 2001 pursuant to its individual Act 1.708/01 (“Minas Mining Lease”). On February 17, 2007 the Company signed the Contract of Option to Purchase Mining Lease Rights with Minas Paraguay S.A. (“Minas Paraguay”) as amended on April 18, 2007, which gives the Company the option to earn a 70% interest in the Minas Mining Lease by paying escalating cash payments totalling US$2.0 million over 3 years, expending US$

13

750,000 on exploration over 2 years plus delivering US$ 50,000 in common shares of the Company. On vesting of the 70% interest, a joint venture will be formed and if Minas Paraguay’s participating interest drops to 5%, 4% of said interest converts to a 10% NPI.

The Company has filed the required Quarterly Reports and has paid Annual Canon

fees totalling $750.00. On or before the first anniversary of the Agreement the Company will have expended in excess of the $500,000 required on exploration of the Mining Lease.

Minas Paraguay has been granted an environmental license, required for production,

and exploration through to July 2009. The Company has temporarily suspended production to fully evaluate the resource of the Mining Lease.

EXPLORATION PERMITS

During 2007, the Company dropped several exploration permits, received approval for exploration concession Rio Verde (1,332 ha) and submitted application for three new exploration concessions: Block A (4,000 ha), Block B (500 ha) and Block C (2,300 ha). The total area of the exploration concessions under application is 6,800 ha. As of the date of this report approval for the three exploration concession is pending.

As the Company has not received formal approval for the exploration permits, no

Canon fees have been paid. When the permits are formally approved payments of $0.85/ha ($6,715) will be required.

The Company holds all permits required to carry out the proposed exploration

on the Properties.

15

MINING LAW AND TAXATION

Paraguay has no significant history of mining. On May 3, 2007, Sr. Hector Ruiz Dias, Deputy Mining Minister, Republic of Paraguay introduced the new Mining Law, assuring security of title and defining exploration and exploitation (mining) rights. Under the Mining Law, the mining royalty previously payable to the Government was eliminated as a means of encouraging mining investment in the country and to stimulate a fledgling exploration and mining industry. The VAT is 10% and the maximum income tax payable is 27.5%.

Claims are granted as Prospecting Permits and are good for a period of one (1) year

with the right for a six (6) month extension, or claims can be recorded as Exploration Concessions.

Exploration Permits are granted for a period of two (2) years, with the right for a one

(1) year extension. To maintain the concessions in good standing, Canon Fees are paid annually, payments range depending on the size and age of the concession. After the three (3) year exploration period the exploration concession can be converted to an Exploitation Permit.

Exploitation Permits are granted when the Prospecting and Exploration phases have

been completed and are granted for 25 years, renewable every 5 years. The exploitation permits are surveyed and the corners marked by concrete monuments. To maintain the concessions in good standing, quarterly technical reports must be filed with the Government and annual Canon Fees paid.

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5 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY ACCESSIBILITY

Paraguay is a small land-locked country covering 406,752 km2. The population is 5.7 million with 57% living in the rural areas and 43% in the urban areas. The capital of Paraguay is Asuncion, a modern city with a population of approximately 2 million. Paraguay has a modern system of highways, railroads and an international airport in Asuncion with many daily flights to neighbouring countries. Paraguay is one of the largest power exporters in South America.

The Property is located about 150 km east-southeast of Asuncion, Paraguay (55°

55’W; 24° 42”S). It can be reached from Asuncion by car along paved national highways and county roads (Figure 4.1). The drive from Asuncion to Paso Yobai takes about 4 hours. The Property is in the Paraneňa Region of Paraguay, east of the Paraguay River.

CLIMATE

The Paraneňa Region has a subtropical climate. It is humid with abundant precipitation throughout the year and moderate seasonal changes in temperature. The region has two distinct seasons: summer, October to March and winter, May to August. During winter, July is the coldest month with mean temperatures of about 17° C. There is no significant north-south variation and the number of days below freezing ranges from three to sixteen. However, no part of Paraneňa is free from the possibility of frost and crop damage. In the summer, October through March, the seasonal average is about 21° C with January, the hottest month, having a mean temperature of 27° C. During the daytime in the summer temperatures reaching 38° C are fairly common. Rainfall in the Paraneňa region is fairly evenly distributed. The least rain falls in August, 2 to 10 cm, and the two periods of maximum precipitation are March to May and October to November. The average annual rainfall is 152 to 165 cm.

LOCAL RESOURCES

Paraguay’s primary resource is agriculture with arable land forming about 6 % of the surface area and permanent pastures 55 %. Other resources include hydroelectric power, forestry, forests form 32% of surface area,, and the mining of limestone.

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INFRASTRUCTURE

Asuncion has the typical resources of a modern city. There is no history of mining in the country, but there is a strong construction industry, which supports a growing quarry, aggregate industry. Heavy road construction equipment is available in Asuncion and to a lesser extent locally. Paso Yobai is a small community having a population of 22,500. There is a small community hospital, police and fire station in Paso Yobai. There is labour locally available, which is largely agriculturally based, but there is a small but active group of local “miners” who are currently mining gold from prospect pits on the Property. The Company is working with these miners and training them in various modern exploration methods to advance the project. The Company office in Asuncion and the field office on the Property have the resources of modern offices including internet connections at both locations.

The Company has a small, grass landing strip on the Property that is currently being

re-approved for use by small aircraft. There is a 500 kv power line to the Property that supplies power to Alex Stewart Laboratories (“Alex Stewart Assayer’s”), sample preparation, laboratory.

PHYSIOGRAPHY

The area is a rolling plateau about 200 m above sea level. It has an overall slope to the east and the south. The principal rivers trend east-west and drain to the Paraguay River to the west and to the Paraná River to the east. The ground surface has relatively low topography, 50 to 75 m. Most of the land has been cleared for agriculture but there are patches of forest between farms and near rivers.

6 HISTORY Paraguay is a country with no history of mining although it has good exploration

potential. The largest reported program was between 1978 and 1982 when Anschutz Corporation, a private American company, carried out an exploration program for oil, gas and minerals. After spending about $25 million dollars Anschutz defined an area with the potential to host a new uranium province. At this point Anschutz ceased exploration probably due to a drop in the price of uranium. Recently other companies have been acquiring exploration concessions in Paraguay to cover the uranium anomalies defined by Anschutz.

In the late 1990s Yamana Resources explored for gold in the alkaline rocks of

Paraguay and drilled a prospect about 50 km east of the Property, but subsequently abandoned the claims and left the county.

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Work done on the Property includes: 1996 - Original discovery of the gold occurrence on the Minas Paraguay property

by Daniel Benitez. 2001 - David Benitez staked ground and hired a geologist, Juan Carlos Benitez, who

is no relation, to carry out a reconnaissance survey of the area. This survey found gold bearing veinlets in sandstones associated with a mafic dyke.

2002 - Juan Carlos Benitez wrote a geological report summarizing his surface work.

Daniel Beitez sold 78% of the property to Ortellado, a construction company. Ortellado purchased a gravity mill and used a backhoe and trucks to open up an area 1.2 km long, 20 to 40 m wide, and 5 to 50 m deep on top of the main dyke. The production is not documented. A mine production of 150 oz per month is reported but not supported. Ortellado did no grade or process control and did not assay the ore or the tailings.

2002 - Ortellado hired Dr. Schalamuk from La Plata University in Argentina.

Schalamuk described the deposits exposed in the pits and did some geochemical sampling which returned values of 1.93g/t Au, 2.84g/t Au, and 2.08g/t Au. Magnetic surveys were recommended.

2002 - Sr.Iske completed a magnetometer survey on the Minera Guaira property.

This survey defined the mafic dyke. Sr. Iske also mapped the exposures in the pits.

2003 - Sr. Tessone, from the La Plata University Group, reported that their

magnetometer survey had mapped the location of the mafic dike. 2007 - The Company optioned the Minera Guaira Mining Lease and the Minas

Paraguay Mining Lease. 2007 - The Company began the first modern exploration program on the Property .

7 GEOLOGICAL SETTING Paraguay has limited information about its mineral wealth and geologic setting.

There is no Government Geologic Survey and information is either private, company generated, or in scattered scientific reports. The only complete geological map of the country is at 1:1,000,000 scale produced in 1986 by Fulfaro and Alvarenga. The metallogenic map of Paraguay was completed by Caceres and Palmieri in 1986. These geologic and metallogenic maps summarize the regional work done in Paraguay between 1979 and 1983 by Anshustz Corporation who staked 64,000 m2, in eastern Paraguay, and performed a reconnaissance exploration program of mapping, Landsat image analysis,

20

and radiometric and magnetic airborne surveys. Anshustz Corporation left Paraguay in 1987, leaving an excellent database with samples, geophysical data, maps and descriptions of numerous showings and mineral occurrences. Most of this data has been lost and only scattered reports are found now in the Mining Department library. Figures7.1 and 7.2 show the geology and mineral occurrences of eastern Paraguay. There are no active metal mines in Paraguay and the only mining activity is in quarries.

A program, sponsored by the German Government, exists to map Paraguay at

1:100,000 scale but only 4 sheets of 79 have been completed. The Property is partially covered by the “1:100,000 Villa Rica” geology sheet by Gonzalez and Cubas (2001). This map, plus the geologic work of the Company’s exploration team and interpretation of magnetic surveys and satellite imagery, produced the regional geology map for the Paso Yobai region (Figure 7.3).

REGIONAL GEOLOGY

Paraguay’s geological framework consists of three cratons ranging in age from 3.800 to 2,7 Ma, composed of gneisses, granulites and greenstone belts, surrounded by 950-550 Ma old metamorphic rocks broadly referred to as the Brazilian Shield. These rocks are covered by intra-cratonic red beds of Carboniferous and Permian age, the Coronel Oviedo Formation and Independencia Group (Table 7.1). The geologic evolution of Paraguay to this time was related to the Gondwana Super Continent, which consisted of Africa, Australia and South America. With the beginning of the break-up of Gondwana in the Mesozoic large northwesterly oriented rifts were generated in Eastern Paraguay and the related basins filled with Triassic and Jurassic, fluvial and aeolian sandstones, the Misiones Formation. The sedimentary rocks are intruded by two rift related, mafic units, the Alto Parana Magmatic Suite and the Sapucai Magamatic Suite. Both units intrude as dikes and sills and outcrop as extrusive rocks along northwest regional structures. The Sapucai Suite is alkali and consists of carbonatites, tephrites, nepheline syenites, shonkonites, malignites, phonolites, essexites, kimberlites and alkaline trachytes. The Alto Parana Suite consists of tholeitic and alkalic basalts and lamprophides (Gonzalez Nunez and Cubas Villalba, 2001). K-Ar radiometric ages for the Sapucai Suite range from 165 Ma to 115 Ma.

LOCAL GEOLOGY

The Paso Yobai area is covered by Carboniferous and Permian sediments that outcrop 20 km to the northwest (Figure 7.3). These sediments are covered by the Misiones Formation, which consists of sub-horizontal Triassic-Jurassic red, aeolian sandstones with local mudstone interbeds. There are three mafic intrusive units cutting these sedimentary units: 1.) tholeitic-alkalic basalts (Alto Parana Suite); 2.) alkalic basalts (Sapucai Suite); and 3.) mafic dikes. As the distinction between tholeitic and alkaline basalts is based on the K20 content it is difficult to establish in the field which are alkaline and which are tholeiites. However, all intrusive rocks intrude along northwest structures of the Mesozoic rifting process.

Figure 7.1

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TABLE 7.1 STRATIGRAPHY EASTERN PARAGUAY

Latin American Minerals Inc – Paso Yobai Project

Age Formation Rock Type Type of Intrusive

Rock type

Quaternary-Tertiary

Unconsolidated sediments

Tertiary Intrusions Stocks and dykes

Sodic- Alkaline

Late Early Cretaceous

San Juan Bautista Gp

Basalts

Intrusions Stocks and dykes

K-Alkaline rocks

Paraná Basin Thoeliitic basalts

Early Cretaceous

Intrusions Stocks and dykes

K-Alkaline rocks

Jurassic-Cretaceous

Misiones Fm Sedimentary rocks including sandstones

Permian Independencia Gp Sedimentary rocks

Permian-Carboniferous

Coronel Oviedo Gp Sedimentary rocks

Ordovician-Silurian

Caacupé and Itacurubi Gps

Sedimentary rocks

Cambro-Ordovician

Itacupumi Gp Platform carbonate rocks

Archaean to Proterozoic

Crystalline Basement

High to low grade metasedimentary rocks

PROPERTY GEOLOGY

The Property displays Mesozoic structural elements trending north-south, northwest and northeast. These may be projected through the cover sequence from structures in the basement. Northwest structures are interpreted as extensional structures and the northeast as orthogonal fractures formed during the Cretaceous opening of the Atlantic Ocean. As

24

deep crustal fractures they may be related to deep mafic intrusions, which are possible source rocks for gold.

The mafic dyke and its associated mineralization occur in a sinistral normal fault

marked by horizontal slickensides (Corbett, 2007). Where steep slickensides are recognized on surface, visible gold is more common.

Although many northwest trending mafic dykes dip to the northeast in outcrop and

drilling data, southwest dips have been determined from the aeromagnetic data. In addition to the dykes, a pencil-shaped stock is interpreted at the Cerro Mboy area

on the Property (Figure 10.4), where a knob-like feature results from erosion of marginal, softer, kaolin-pyrite (FeOx) altered rocks. The talus of mafic rock rich in spherulites is characteristic of rock textures developed in the upper portion of blind magma chambers. Marginal silicified sandstones contain well developed quartz-veins, changing to quartz-fill breccias at the top of the hill. These features are typical of alteration associated with a buried intrusion.

Gold mineralization occurs associated with the northwest trending, normal-fault

filling, mafic dykes. The northwest dyke trend is disturbed by small-scale structures believed to be local, dextral offsets in dyke segments on north-south cross faults. Other cross faults such as the northeast structures shown on the remote sensing data may also offset the main, northwest structures.

In several instances, better gold mineralization within dilational sheeted-veins occurs

where the northwest structures display flexures to the west-northwest to east-west, or where veins following this trend overprint the general northwest structures. More steeply-dipping fault portions than the general moderate dip display better mineralization apparent as more extensive, open-space quartz-crystal growth.

High-grade gold shoots are interpreted to occur in flexures where the dykes trend

more towards the west. These vein portions generally dip more steeply, as is typical of a dilated setting in normal faults.

While most slickensides on faults, within the mineralized structural corridor, have

sub-vertical trends, near the flexures inclined slickensides occur. The Paso Yobai environment is characterized by normal-fault extension, with local components of strike-slip faulting. The localized, sinistral, strike-slip fault movement is probably responsible for the development of mineralized shoots in fault flexures and the shoots are interpreted to dip (plunge?) steeply. Normal fault activation would create flat, plunging shoots within the steep-dipping faults, and inclined shoots could result from mixed dip-slip and strike-slip fault movements.

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8 DEPOSIT TYPES Sillitoe (2002) pointed out that most gold deposits associated with alkaline rocks are

broadly similar to those hosted by their cal-alkaline counterparts. However, alkaline suites were deficient in high-sulphidation epithermal-gold deposits. The characteristics of several large gold and copper deposits associated with alkaline rocks, Porgera, Cripple Creek, Ladolam, and Palabora, diverge from their most closely related deposit types making them “unique”. Most types of gold and copper deposits developed in calc-alkaline provinces constitute exploration targets in and around alkaline igneous centres. Sillitoe (2002) thought that the possibility of encountering unconventional giant alkaline deposits lacking analogous calc-alkaline examples might be of greater interest. He also pointed out that while the greatest exploration potential was in or behind calc-alkaline arcs at convergent plate boundaries, an anorogenic, intra-continental setting should not be ignored.

The model for Paso Yobai is part of the intra-continental rift environment (Figure

8.1). All known heat sources for the brines and mineralizing events are mafic to ultramafic, alkalic rocks. Alkalic rocks are known as important sources of mineralization, from the mafic and ultramafic to the felsic end of the spectrum. The Paso Yobai mineralization has similar characteristics to intra-continental rifts including:

• Mineralization hosted in veins and stockwork of calcite, minor quartz,

mangano-calcite and fluorite.

• Mineralization spatially related to mafic dykes.

• Fluid inclusions show temperatures between 180 and 240° C and salinities of 2.5 Wt% NaCl.

• PIMA (Portable Infrared Spectrometer) measurements show smectite-calcite-

silica alteration assemblages, characteristic of low temperature, neutral brines.

• The geochemical signature of the stockworks has anomalous gold, vanadium, copper, arsenic and phosphorous.

• Gold present as fine-gold (<0.1 mm) grains and coarse-gold grains (up to 50

mm) in the carbonate veins. There is little silver in the gold. These characteristics are typical of low sulphidation, epithermal, gold mineralization

defined by Corbett and Leach, (1998), Corbett (2005) and Hedenquist et. al. (1996). Intrusion-related epithermal-gold mineralization often has supergene-gold

enrichment, particularly in climates characterized by wet/dry cycles and tropical environments of deep weathering. At Paso Yobai, the questions as to whether gold enrichment at surface generated the gold, soil anomaly and the presence of high-grade

27

gold in rock chip samples at surface represented a supergene enrichment of low, primary-gold grades was important to resolve. Drilling has demonstrated high-grade gold-mineralization occurs at depths of up to 200 m below surface oxidation. The Company has concluded that although supergene enrichment might exist in the area, it is not a major concern from the exploration perspective.

Green, smectite-clay alteration commonly recognized in the vein system on surface

and in all drill holes, suggests Paso Yobai is eroded to expose the top of an epithermal vein system. As a poorly eroded epithermal system, Paso Yobai is likely to have depth potential.

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9 MINERALIZATION Corbett (2007) identified two types of vein mineralization in Paso Yobai: quartz-

sulphide gold-style mineralization and epithermal quartz-carbonate gold-manganese with low sulphidation mineralization.

QUARTZ-SULPHIDE AU-STYLE MINERALIZATION

Quartz-sulphide style, gold (Au) mineralization commonly forms early in the paragenetic sequence of the development of intrusion-related gold deposits and comprises gold within crystalline pyrite. Drill holes have demonstrated that mineralization of this type is associated with high pyrite, kaolin and smectite.

Quartz-sulphide style, gold mineralization forms early in the paragenetic sequence of

the development of intrusion-related gold-deposits and comprises pyrite, now oxidized to iron oxides (FeOx). Forms of quartz-sulphide mineralization recognized on the Property include:

• Disseminated pyrite within the dykes and wall rocks.

• Pyrite veins with local, coarse crystalline, tightly packed, quartz, as individual

veins or packages of sheeted arrays.

• Shears and breccia zones with matrix of FeO and similar tightly packed, crystalline quartz.

EPITHERMAL QUARTZ-CARBONATE AU-MN-STYLE LOW SULPHIDATION MINERALIZATION

At Paso Yobai epithermal mineralization comprises several mm wide open carbonate, mangano-calcite and minor quartz- veins, veinlets and stockworks. This mineralization is best developed as sheeted veins in the dilated, structural zones defined by west-northwest flexures in the northwest structural corridor. The sheeted veins have better developed open carbonate veins. Minor, open-space breccias lined with fine-crystalline pyrite are believed to be this type of mineralization. Many quartz-MnO veins contain wire-like, free gold growing in open space. These veins are associated with bonanza gold grades and commonly overprint earlier auriferous-pyrite rich, quartz veins.

At Cerro Mboy, minor, open-space breccias, lined with fine-crystalline pyrite are

interpreted as this style of epithermal mineralization.

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Artisanal miners at the Granada pit (Figure 10.4) report the highest gold grades occur with kaolin in contact with jarosite. The kaolin-jarosite association suggests that quartz-pyrite gold mineralization may have been upgraded by fluid mixing.

10 EXPLORATION The major exploration programs on the Property include: interpretation of satellite

imagery, airborne geophysics, soil geochemistry, rock chip sampling in artisanal workings, and limited mechanical trenching (Figure 10.1). The airborne geophysical survey was conducted by a contractor under the field supervision of Mr. John Kieley, P.Geo, the Company’s independent consulting geophysicist and a “Qualified Person”. Sample preparation and analyses for soil samples, rock samples and drill core samples were carried out under the supervision of professionals from Alex Stewart Assayers a company of certified assayers in Mendoza, Argentina. The other aspects of the exploration program were carried out by company personnel under the supervision of the Company’s Qualified Person, Dr. Waldo Perez. The costs of the work to the end of December 31, 2004 are summarized in Table 10.1.

TABLE 10.1 EXPLORATION EXPENDITURES 2007 Latin American Minerals Inc. – Paso Yobai Project

Category Amount Costs (US $)

Drilling 2,000 m $450,000

Airborne Geophysics 3,546 km $475,000

Property Payments $326,000

Geochemistry $100,000

Lab Construction $180,000

Contracting: Cat work, trenching, water $149,000

Salaries/fees $320,000

Total $2,000,000.00

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SATELLITE IMAGERY

The Company acquired IKONOS satellite imagery with a pixel definition of 50 cm covering an area of approximately 10 km x 10 km. This image has been used to help locate the drill holes, preliminary surface mapping of structures, there is limited or no outcrops, as well as to locate surface property boundaries, rivers, etcetera. The location of the area covered by the IKONOS image with respect to the mineral properties is shown in Figure 10.1.

HELICOPTER EM AND MAGNETIC SURVEY

On May 4, 2007, the Company signed a contract with Geotech Airborne Limited (“Geotech”) to carry out a helicopter-borne geophysical survey for about 2,500 line-km over the Paso Yobai Area. The airborne survey was carried out under the direct field supervision of Mr. John Kieley, P.Geo, the Company’s independent consulting geophysicist and “Qualified Person”.

Between June 18 and July 2, 2007, Geotech completed a survey of 3,546.1 line

kilometers covering the Property (Anon, 2007). The principal geophysical sensors included a time domain, electro-magnetic (VTEM) system, and a cesium magnetometer. Ancillary equipment included a GPS navigation system and a radar altimeter. In-field data processing, which included quality control and compilation of data, was done at Paso Yobai. The final data processing including generation of final, digital-data products was done at Geotech’s office in Aurora Ontario. End products of the survey included a total-magnetic field-contour map and electromagnetic, stacked-profiles map. The contractor concluded that “a number of EM anomaly groupings were identified and that ground follow-up of those anomalies should be carried out if they were supported by other geoscientific data”.

MAGNETIC SURVEY

The Company’s analysis of the airborne magnetic-data identified a strong, linear magnetic-anomaly previously discussed and related to the Main Gold Zone, as well as several additional and untested, linear magnetic-anomalies, inferred to be parallel dykes on the Property (Figure 10.2). The 6.5 km long Main Gold Zone traced by soil geochemistry and exposed intermittently along strike by artisanal miners for 3.7 km, has a distinct, high magnetic-signature bounded by two magnetic lows, which the Company believes reflects the alteration around the mineralized system. The magnetic survey also indicated that the dyke continues to the northwest beyond the limits of the gold soil-anomaly for at least 2.7 km. To the southeast this linear magnetic feature is displaced by a north-easterly trending, magnetic lineament probably representing a northeast trending, conjugate-fault zone. After the displacement, the magnetic anomaly associated with the Main Gold Zone, soil anomaly can be traced to the southeast along strike for an addition 2.7 km. The total length of the linear magnetic anomaly locally

34

associated with the Main Gold Zone is approximately 11.9 km. The survey confirmed the regional, northwest, structural trend identifying numerous lenticular, magnetic anomalies trending northwest-southeast. The survey also identified several circular anomalies interpreted to be intrusive stocks.

VERSATILE TIME DOMAIN ELECTRO MAGNETIC (“VTEM”) SURVEY

The VTEM system is a new airborne, electromagnetic system. Key features include:

• Superior exploration depth – over 400 metres.

• Low base frequency (25 or 30 Hz) for penetration through conductive cover.

• High spatial resolution – 2 to 3 metres receiver-transmitter symmetry.

• Spotting drill targets directly off of the airborne results.

• Excellent resistivity discrimination and detection of weak anomalies.

• Virtually impervious to power line interference. The VTEM survey identified numerous, variably conductive units associated with

potentially significant structural and geological features on the Property. The shallow conductors on the apparent conductivity map (Figure 10.3) show a chargeable trend, about 4 km long, sub-parallel to the Main Gold Zone. Thirteen (13) structural features have been identified and are characterized by variably magnetic, linear conductors reflecting five (5) shallow-response conductors and eight (8) deep-response conductors, which typically trend north-westerly across the Property. The shallow response conductors range from 1 km to 2 km in length for an aggregate total strike length of 8 km. The deep response conductors range for from 1 km to 3 km long for an aggregate total strike length of 17 km. The Company believes that the conductors reflect shallow and deep seated structural features and/or mafic-alkalic dykes, and may contain sulphide mineralization.

A large, VTEM anomaly located immediately south of the mafic-alkalic dyke is of

unique size and shape and is coincident with an area of low magnetic values on the south side of the Main Gold Zone. The Company believes that this coincidence reflects an “alteration finger print” around the dyke. However, this coincidence does not exist on the north side of the dyke, which indicates that there is no conductivity associated with this area of low magnetic values. Drilling will be required to determine the cause of this unique VTEM anomaly.

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MINERALIZATION IN THE PITS

Rock chip data was obtained from sampling completed at Minera Guaira and Minas Paraguay pits, with additional sampling from the numerous pits excavated by the local miners (Figure 10.4). The sampling environment was hazardous due to the very unstable nature of the pit slopes in the workings. Extreme care was taken to collect the minimum amount of sample necessary so as not to disturb the stability of the pit walls. The extensive weathering profile and the extensive alteration of the rock also presented challenges.

A total of 584 rock chip samples were collected in 2007. Table 10.2 presents the

most significant rock chip assays. Typically, 3 kilos of material would be taken over 1 m. Because of the scale of the project, the sample numbers are tied to a geographic location, such as the name of a mine or pit and the results shown on the satellite image of the region.

All sample preparation and analyses were carried out under the supervision of

professionals from Alex Stewart Assayers.

February 2008

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TABLE 10.2 SIGNIFICANT ROCK CHIP SAMPLES

Latin American Minerals Inc. – Paso Yobai Project

Target Sample Number

Sample Width (m) Au (g/t)

DELFIN 187370 Grab 1.66

10172 2.00 1.73

125 3.48 1.97

104 Grab 10.61

187362 Grab 28.60

GRANADA 144 Grab 2.22

187366 Grab 2.80

10396 2.00 2.94

150 Grab 4.00

10008 0.40 4.32

10400 2.00 4.78

10288 2.00 5.28

10397 2.00 6.66

10009 0.50 11.32

10007 0.40 12.09

10399 2.00 31.81

187369 Grab 32.10

GUAIRA 10048 0.50 1.10

143 Grab 1.19

10001 0.50 1.19

1998-W 0.20 1.19

10043 0.50 1.38

187347 Grab 1.76

1999-W 0.20 2.43

10119 2.00 2.52

10049 0.50 2.88

10090 1.00 2.91

141 1.00 3.59

10087 1.00 6.12

10004 0.50 9.13

187348 Grab 10.40

187351 Grab 15.10

10088 1.00 21.47

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TABLE 10.2 SIGNIFICANT ROCK CHIP SAMPLES Latin American Minerals Inc. – Paso Yobai Project

Target Sample Number

Sample Width (m) Au (g/t)

10002 0.50 98.27

TONY 118 4.01 1.06

117 1.20 1.11

42 0.15 1.43

187383 Grab 1.47

41 0.2 2.25

187308 Grab 2.28

187397 Grab 3.03

187392 Grab 4.83 The rock chip results confirm the presence of significant gold values in weathered

bedrock corresponding to the gold soil anomaly (Figure 10.5).

SOIL GEOCHEMICAL SURVEY

Based on the trend of the mineralized zone defined by the artisanal pits and on geological observations the geochemical survey grid was established with a baseline tending 135° and with grid lines every 200 m trending 045°. Soil sample stations were established every 25 m along the grid lines. The location of the survey grid and the sample stations were GPS controlled.

Based on the soil profile exposed in the pits, it was determined the best sample

medium was at the A-B soil-horizon contact which is at a depth of between 0.5 m and 1.0 m. It was also determined that a 2.5 kg sample should be collected. A total of 8,500 samples will be collected on completion of the survey. The samples are tagged with a pre-numbered tag and bagged in micropore bags to allow humidity to evaporate. The samples were sent to the preparation facility on site operated by Alex Stewart Assayers. About 5,694 samples were collected in 2007.

Results of the soil survey are shown on Figure 10.5. The basic statistical analysis of

the current soil sampling database (5,694) is given in Table 10.3.

February 2008

41

TABLE 10.3 DESCRIPTIVE STATISTICS OF

THE SOIL SAMPLE DATABASE Latin American Minerals Inc. – Paso Yobai Project

Au (ppb)

Valid cases 5,694

Mean 9.83

Std. error of mean 0.44

Variance 1,087.33

Std. Deviation 32.97

Variation Coefficient 3.36

rel. V.coefficient(%) 4.45

Skew 16.05

Kurtosis 399.27

Minimum -2

Maximum 1,065

Range 1,067

Sum 55,960

1st percentile -2

5th percentile -2

10th percentile -2

25th percentile -2

Median 4

75th percentile 9

90th percentile 23

95th percentile 45

99th percentile 112.05

Geom. mean ---- The gold soil, geochemical results are a valuable exploration tool. The survey

defined the gold-bearing trend exposed by the local mineral and past producing mines of Minas Paraguay and Minera Guaira referred to as the Main Gold Zone, which has been traced along strike for 6.5 km and is variably up to 2 km wide.

The diagnostic features of the Main Gold Zone anomaly are:

1) Statistically, the gold content in the soils is extremely high, ranging from 75 ppb to 1,100 ppb Au;

42

2) The strike length of the anomaly as currently defined is 6.5 km;

3) The width of the soil anomaly is up to 1,500 m especially in the undisturbed forested area to the northwest. The magnitude of this anomaly is >50 ppb over 225 m, including nine continuous sample sites that average 243 ppb;

4) The anomaly is repeated on multiple adjacent lines 200 m apart;

5) The areal extent of the anomaly is regional covering in excess of 400 ha.

The anomaly in the area exploited by the local miners has an entirely different soil

geochemical finger print. It is poorly defined and erratic. The soil-geochemical survey outlined several parallel zones that correspond to some

of the magnetic highs parallel to the Main Gold Zone magnetic anomaly. Ongoing sampling will further define these new anomalies.

11 DRILLING In October 2007, the Company signed a drill contract with Patagonia Drilling, based

in Mendoza, Argentina, for 5,000 m of HQ diamond-core drilling using a truck-mounted UDR coring drill. Drilling commenced on November 1, 2007. The program comprises a series of diamond drill cross-sections at right angles to the trend of the gold-bearing zone designed to test the zone to depths up to 200 m. Twelve (12) holes, totalling 1,989.2 m, were drilled in 2007. The drill-hole locations and depths are presented in Table 11.1 and on Figure 11.1. Drill hole assays for gold are given in Appendix 1 and examples of the drill logs are presented in Appendix 2.

During the 2008 drill program three holes have been completed. As of the date of this

report assays are pending.

43

TABLE 11.1 DIAMOND DRILL HOLE COORDINATES

Latin American Minerals Inc. – Paso Yobai Project

Hole Depth (m) Azimuth (°) Inclination (°) X Y

LAT-1 137.90 215 -50 599302 7148307

LAT-2 165.30 218 -65 599302 7148307

LAT-3 128.30 205 -50 599759 7147792

LAT-4 152.70 204 -65 599760 7147792

LAT-5 243.40 205 -70 599770 7147844

LAT-6 143.50 211 -50 599703 7147834

LAT-7 263.90 220 -70 599732 7147882

LAT-8 310.20 200 -65 599863 7148702

LAT-9 153.00 220 -50 599153 7148688

LAT-10 56.90 230 -60 599011 7148864

LAT-11 129.00 220 -60 599560 7147952

LAT-12 129.00 220 -60 599560 7147952 Assays have been received for drill holes LAT 1 through LAT 12 inclusive. Gold

assays are included in Appendix 1. Significant gold assays are summarized in Table 11.2.

TABLE 11.2 SIGNIFICANT DIAMOND DRILL ASSAYS Latin American Minerals Inc. – Paso Yobai Project

From To Interval Au (g/t)* Au (g/t) (m) (m) (m) Classic Fire Assay Metallic Fire Assay

DDH-LAT-1 92.00 102.00 10.00 1.64

Including:

92.00 94.00 2.00 4.23 5.96

DDH-LAT-3 Gold Bearing Zone Intersected over 1m from 112.00m to 113.00m

112.00 113.00 1.00 12.60 13.00

DDH-LAT-6 Gold Bearing Zone Intersected over 6m from 112.00m to 118.00m

112.00 118.00 6.00 11.00 15.30

Including:

44



112.00 113.00 1.00 7.87 9.13

113.00 114.00 1.00 30.77 37.86

114.00 115.00 1.00 1.84 1.11

115.00 116.00 1.00 24.59 25.22

which includes:

112.00 116.00 4.00 18.51

Gold Bearing Zone Intersected over 6.50m from 99.00 m to 105.50 m

99.00 105.50 6.50 26.64

Including:

100.50 104.00 4.00 43.08

100.50 101.00 0.50 138.39

104.00 104.50 0.50 105.51

88.20 92.80 4.60 3.20

DDH-LAT-11 Gold Bearing Zone Intersected over 3.60 m from 89.20 m to 92.80 m

89.20 89.70 0.50 9.55

89.70 90.20 0.50 11.87

90.20 91.00 0.80 0.03

91.00 91.80 0.80 0.70

91.80 92.30 0.50 4.57

92.30 92.80 0.50 3.08

Gold Bearing Zone Intersected over 6.50 m from 99.00 m to 105.50 m

99.00 100.00 1.00 0.56

100.00 100.50 0.50 0.28

100.50 101.00 0.50 139.39

101.00 101.30 0.30 28.49

101.30 101.80 0.50 24.48

101.80 102.30 0.50 6.72

102.30 103.50 1.20 2.38

103.50 104.00 0.50 15.41

104.00 104.50 0.50 105.51

104.50 105.00 0.50 3.93

105.00 105.50 0.50 0.24

45



DDH-LAT-12 Gold Bearing Zone Intersected over 1.05 m

85.90 86.95 1.05 3.49 Figures 11.2 to 11.9 show drill sections for all the holes. Drilling has to date traced

the dyke for about 1.3 km. The geology is essentially the same along this distance and there are significant gold intersections in five of the twelve widely spaced holes. Existing results indicate the need for follow up drilling in the 600 m zone between diamond drill hole LAT-6 and LAT-2.

The intersections are structurally controlled in widely spaced drill holes. As the

mineralized zones and the controlling structures are defined by the same drill holes it is difficult to provide a global estimate of true thickness. The geological sections suggest true thickness is about 75% of the down-hole length but this is a very preliminary estimate.

55

12 SAMPLING METHOD AND APPROACH The soil, rock chip and drill core sampling programs were designed by Dr. Waldo

Perez, P. Geo., the Company’s “Qualified Person” responsible for the project. The various programs were carried out by experienced geologists and or exploration specialists under the supervision of Perez.

SOIL SAMPLES

Samples were collected on lines 200 m apart perpendicular to the known gold-bearing zones at the contact between the A and B soil horizons. The samples were collected at 25 m intervals along the lines and consisted of 2.5 kg of material collected at depths ranging from 50 cm to 100 cm. The samples were collected in pre-numbered micropore bags which allowed humidity to evaporate. The samples were sent to the preparation facility operated by Alex Stewart Assayers. Approximately 5,694 samples or 67 % of the 8,500 samples planned for the program have been collected.

The analytical results have undergone statistical interpretation to determine

background, threshold and anomalous values and the results are presented and discussed in Section 10 Exploration.

ROCK CHIP SAMPLES

The lack of outcrop on the Property made rock chip sampling difficult. Rock chip samples were collected from existing pits on the property. Details of this sampling on the Property are given in Section 10 Exploration, the sampling environment was usually hazardous and extreme care was taken to collect the minimum amount of sample necessary to avoid disturbing the pit walls.

A total of 603 rock chip samples were collected in 2007 and the significant assay

results are presented in Section 10.

DRILL CORE SAMPLES

At the drill site, the core was placed in core boxes and delivered to a secure, field, core processing centre. The core was “split” using a diamond saw operated by experienced exploration technicians and logged by professional geologists. The typical sample interval was 1 m but the intervals varied from 2 m to 0.5 m as determined by the geologist logging the core. When visible gold was observed the sample was assayed by “metallic” assay procedures. Half of the core remains in the core box as a permanent reference of the interval sampled. The other half formed the samples and was delivered

56

to the sample preparation facility, operated under the direct supervision of professionals from Alex Stewart Assayers.

As of December 31, 2007, a total of 12 holes have been drilled and a total of 708

samples have been taken for analysis.

13 SAMPLE PREPARATION, ANALYSES AND SECURITY

The soil, rock chip and drill core samples were prepared on site under the supervision and QA/QC provided by professionals from Alex Stewart Assayers. This company is an ISO 9001-certified laboratory with laboratory facilities in Mendoza, Argentina and headquarters in England.

SOIL SAMPLES

The soil samples were delivered to Alex Stewart Assayers’ supervised, preparation facility on the Property in pre-numbered micropore bags. The samples are dried in stainless steel containers at 80° C and sieved at -140 mesh. When small pellets formed during drying they were crushed by hand using a stainless steel ball. After drying and sieving the sample was split to obtain a 200 g pulp which was shipped by truck to Asuncion and by a bonded international courier to Alex Stewart in Mendoza. All samples were analyzed for gold and multi-elements. Gold was analyzed by Fire Assay with AA finish using 50 g sample. Accuracy of results is tested through the systematic inclusion of blanks and certified reference standards. The multi-element assays were done using ICP.

ROCK CHIP SAMPLES

The rock chip samples were collected in pre-numbered bags. The samples were dried, crushed and part of the sample was tagged and archived as coarse reject and the remaining part was ground to <200 mesh and shipped by bonded courier to Alex Stewart Assayers in Mendoza, Argentina. All samples were assayed for gold using fire assay and multi-elements by ICP. Accuracy of results is tested through the systematic inclusion of blanks, duplicates and certified reference standards.

In 2007, approximately 603 rock chip samples were collected and assayed.

57

DRILL CORE SAMPLES

The core samples were crushed, dried and split under the on site supervision and QA/QC provided by professionals from Alex Stewart Assayers.

When the split sample was crushed most was archived as coarse reject and 800 g was

pulverized to <200 mesh and shipped by bonded courier to Alex Stewart Assayers in Mendoza. All samples were fire assayed for gold using a 50 g sample. For the multi-elements the samples were analyzed using ICP.

METALLIC OR SCREEN FIRE ASSAYS Some core samples exhibit a pronounced "nugget" effect due to the presence of

coarse grained, particulate gold. The result is a scatter in the gold analytical results making it difficult to assess the true gold concentration. To improve the analytical reproducibility a metallic or “screen” assay was carried out on samples where gold was observed. For the metallic fire assay the sample is crushed, 400 g of pulp sieved and the >100 micron (150 mesh) portion of the sample is collected and assayed in its entirety. The <100 micron (150 mesh) portion of the sample is homogenized and a 50 g sample is assayed. The final assay reported is the weighted average of the coarse and fine fractions.

14 DATA VERIFICATION The company includes one blank, one standard and one duplicate in every thirty

samples to maintain quality control. Duplicates are prepared by cutting the remaining half core into a quarter for the assay interval and re-assaying the quartered core. Blanks are a local sandstone collected from a quarry. Standards are from CDN Resource Laboratories and represent high, medium and low gold values. Standards are purchased in 400 g bags and the entire bag is sent to Alex Stewart Assayers. Examples of the assay results for the Company’s standards and duplicates are given in Figures 14.1 and 14.2.

58

FIGURE 14.1 ASSAYS OF A STANDARD SAMPLE

FIGURE 14.2 THOMPSON AND HOWATH PLOT OF DUPLICATE ASSAYS

59

On the initial visit (2007), Cargill collected three samples from the artisanal pits which were analyzed for gold using FA and multi-elements using ICP by SGS Laboratories in Toronto. The results are given in Table 14.1

TABLE 14.1 CARGILL’S SAMPLES FROM PITS


Sample Au (ppb) Au (ppm)

1 >10,000 284.00

2 751 0.075

3 15 0.002 On the second visit (2008) Cargill duplicated six core samples by quartering the core

and collecting pulps of five of the quartered core samples. No pulp was available on site for the sixth sample. These verification samples were assayed using a 50 g sample by fire assay at ALS-Chemex in Mendoza, Argentina.

TABLE 14.2 CARGILL’S RE-ASSAY OF DRILL CORE Latin American Minerals Inc – Paso Yobai Project

Drill Hole From To Alex Stewart ALS-Chemex

(m) (m) Au (ppm) Au (ppm)

1 96.00 98.00 0.56 0.136

3 112.00 113.00 12.83 0.005

4 130.00 131.00 1.66 0.165

6 113.00 114.00 30.77 11.32

6 115.00 116.00 24.59 5.35

11 101.80 102.30 Fine 3.31

Coarse 26.42

Average 6.72 6.32 Some of the variance in assays is because Cargill’s samples (ALS-Chemex) are ¼ core and LAM’s samples (Alex Stewart) are ½ core.

60

TABLE 14.3 CARGILL’S RE-ASSAY OF PULPS Latin American Minerals Inc – Paso Yobai Project

Drill Hole From

(m) To (m)

Alex Stewart Au (g/t)

ALS-Chemex Au (g/t)

1 96.00 98.00 0.56 0.567

3 112.00 113.00 12.83 13.95

4 130.00 131.00 1.66 0.152

6 114.00 114.00 30.77 33.10

6 115.00 116.00 24.59 26.00

11 101.80 102.30 No Pulp No Pulp

The re-assays (ALS-Chemex) compare very well with the LAM assays (Alex Stewart)

15 ADJACENT PROPERTIES Most of the adjacent ground has been taken as exploration permits. There are no

reported mineral occurrences or exploration activity on these permits.

16 MINERAL PROCESSING AND METALLURGICAL TESTING

The Property is an early stage exploration property. No metallurgical testing has been undertaken.

17 MINERAL RESERVE ESTIMATES The Property is an early stage exploration property. No mineral resource or reserve

estimates have been made.

61

18 RELEVANT DATA AND INFORMATION The Property is an early stage exploration property. There is no additional relevant

data and information.

19 INTERPRETATION AND CONCLUSIONS 1) Artisanal mining has demonstrated a large zone of gold mineralization in soils and

weathered rocks, on the Property.

2) Geophysical, geochemical, and geological exploration has demonstrated gold mineralization on the Property is related to:

a) A zone of mafic (basalt) dykes (the “Dyke Zone”). b) The Dyke Zone is bounded and cut by faults parallel to the strike and offset

by faults at a high angle to the strike of the zone. c) The Paso Yobai Gold Zone (the “Main Gold Zone”) has been traced 6.5 km

by soil geochemistry and airborne magnetics and is variably exposed on surface by artisan miners for 3.6 km. Very high gold values in soil geochemistry mark the Main Gold Zone, which corresponds to a linear zone of high magnetic values, bounded by zones of low magnetic values.

d) The aeromagnetic and soil surveys show magnetic anomalies with corresponding gold anomalies parallel to the Main Gold Zone, which suggest parallel mineralized dykes.

e) The distribution of the parallel magnetic anomalies, which are interpreted to be dykes, may be controlled by structures at a high angle to the Main Gold Zone.

f) EM anomalies also parallel the Dyke Zone. These EM anomalies are interpreted as derived from deep sources, and are tentatively interpreted as derived from deep-seated bodies of sulphides.

g) Rock samples from the artisanal mine workings indicate gold mineralization is related to quartz veins in altered mafic dyke and altered (silicified) sandstone near the contacts of the dyke.

h) Gold in the artisanal workings appears controlled by post dyke structures. i) Gold occurs in veins associated with sulphides (pyrite) and as coarse

grained, free gold in veins without sulphides. j) Bonanza grades occur when the sulphide-free veins with visible gold are

superimposed on the veins containing pyrite. k) Paso Yobai has many similar characteristics to several large gold and

copper deposits associated with alkaline rocks, such as Porgera, Cripple Creek, Ladolam, and Palabora.

3) The initial drill program of 12 holes totalling 1,989.2 m, has indicated:

62

a) The dyke ranges from 5 to 40 m thick and continues to at least 100 m depth.

b) Gold occurs in an altered dyke and sandstones controlled by structural zones, breccias, veins, stock-works within the dyke, and within the altered sandstones near the contact of the dyke.

c) Coarse grained free gold giving bonanza assays has been found to depths of about 100 m, which suggests that much of the free gold is primary.

4) Drilling on the aeromagnetic and soil geochemical anomalies has demonstrated

that the gold mineralization is related to carbonate-quartz veins cutting the mafic dyke, and altered sandstones near the contact of the dyke. The gold mineralization including the bonanza grades continues to depths of ±100 m.

5) Although there are only 12 widely spaced drill holes, higher grade, gold

mineralization appears related to variations in the position of the dyke along strike that appear to be dilation zones. The current data indicates that the primary targets in the Main Gold Zone are plunging shoots of structurally controlled gold mineralization.

6) The initial work on the parallel aeromagnetic and soil geochemical gold anomalies

suggests that they are similar to the Main Gold Zone and controlled by structures at a high angle to the Main Gold Zone.

7) The parallel zones present targets similar to those on the Main Gold Zone.

However, multiple parallel zones close to the Main Gold Zone, or to each other, could constitute a target of a large volume of structurally controlled gold mineralization.

20 RECOMMENDATIONS Cargill recommends a two-phase exploration program with the scope and extent of

the second phase contingent on the results of the first phase.

1) The first phase of the exploration will consist of drilling the remaining drill targets (3,000 m) (Figure 20.1) and carrying out soil geochemistry, geology and trenching both to infill the existing grid and to extend the grid to the east and west to explore parallel dyke systems, summarized as follows.

63

TABLE 20.1 PHASE ONE PROGRAM



Soil Sampling 6,000 Samples $50,000


Drilling to complete testing of the established drill targets.

3,000 m $550,000

Reporting $20,000

Subtotal $850,000.00 Contingencies 10% $85,000

Total $935,000

2) The current information indicates a second phase of exploration is warranted. However, the exact scope of work will be based on the results of the Phase One Program. As currently envisioned, the Phase Two Program will consist of:

a) Geochemistry, trenching and mapping to better define the parallel dykes and to extend the Main Gold Zone along strike.

b) Drilling to test new targets developed on the parallel zones and along strike on the Main Gold Zone. Approximately 5,000 m of drilling will be required.

c) Definition drilling on the two best zones within the Main Gold Zone. Cargill estimates that about 12 drill sections with about 5,000 m of drilling will be required to test each zone.

64

TABLE 20.2 PHASE TWO PROGRAM



Soil Sampling 4,000 Samples $45,000 Geochemistry and assaying $150,000

Drilling to complete testing of the established drill targets.

15,000 m $2,700,000

Reporting $50,000

Subtotal $3,395,000.00 Contingencies 10% $339,,500

Total $3,734,500

February 2008

66

21 REFERENCES ANON, 2007, Report on a Helicopter-Borne Versatile Time Domain Electromgnetic

(VTEM) Geophysical Survey; Unpublished report for LAMPSA by Geotech Ltd. CARRASQUERO, S.; CANFOGLIA, M. E.; SHALAMUK B.; 1999. A Hydrothermal

Event Associated with the Alkaline Complex in Cerro Sarambi, Amancay, Paraguay. Mineral Deposits: Processing, Stanley et al.(eds). 1999 Balkema, Rotterdam.

COMIN/CHIARAMONTI, P.; CUNDARI, A.; GOMES, C.B.; PICCIRILLO, E.M.;

CENSI, P.; DE MIN, A; BELLIENI, G; VELAZQUEZ, V.F.; ORUE, D. 1992. Potassic Dyke Swarm in the Sapucai Graben, eastern Paraguay: Petrographical, Mineralogical and Geochemical Outlines. (283-301).

COMIN-CHIARAMONTI, P, et al., 2004, Plumes Beneath the Parana Basin, Eastern

Paraguay: Fact of Fiction?: in www.MantlePlumes.org. CONRADO, C.; PALMIERI,J. Paraguay 1986. Mapa Metalogenico del Paraguay.

Comisión Nacional de Desarrollo Integrado del Chaco/ Naciones Unidas. CORBETT, G.J., 2007, Report on the Paso Yobai Property: Unpublished Report for

Latin American Minerals Inc. CORBETT, G.J., 2005, Epithermal Au-Ag deposit types – implications for exploration:

Pro Explo Conference Peru May 2005, published on CD. CORBETT, G.J., and LEACH, T.M., 1998, Southwest Pacific gold-copper systems:

Structure, alteration and mineralization: Special Publication 6, Society of Economic Geologists, 238 p.

ECKEL, E. Igneous and Metamorphic Rocks. SULSONA, P. UNITED STATES 1959.

Geology and Mineral Resources of Paraguay- A Reconnaissance. Geological Survey Professional Paper 327.

FULFARO, J.; ALVARENA, D.; CONRADO, C. Paraguay 1986. Mapa Geológico de la

Republica del Paraguay. Proyecto par 83/00 GONZALEZ, M.; VILLALBA, N. San Lorenzo 2001. Mapa Geológico de la Republica

del Paraguay. HARRINGTON, H. Buenos Aires, 1950. Geología del Paraguay Oriental. HEDENQUIST, J.; IZAWA, E.; ARRIBAS, A.; WHITE, C.; 1996. Epithermal Gold

Deposits: Styles, Characteristics, and Exploration: The Society of Resource Geology: Resource Geology Special Publication number 1,70p.

67

LATIN AMERICAN MINERALS INC, 2008. Petrographic Examination of Six Drill

Core Samples from the Paso Yobai Project. NUŇEZ, M.E.; Asunción 1999, Mapa Geológico de la Republica del Paraguay, Texto

explicativo. SHINAGAWA, Y.; 1996-2002. Reciente Exploración de Recursos Minerales en el

Paraguay Oriental. THE ANSCHUTZ CORPORATION, Thomas & Associates 1976. Denver, Colorado.

Preliminary ERTS Interpretation South-eastern Paraguay.

68

22 SIGNATURE PAGE This report titled “Technical Report on Paso Yobai Project, Uraguay” prepared for

Latin American Minerals Inc. and dated February 15, 2008 was prepared by and signed by:

(Signed and sealed) Dated at Toronto, Ontario D. George Cargill, Ph.D., P.Eng February 15, 2008 Consulting Geological Engineer

69

23 CERTIFICATE OF QUALIFICATIONS D. GEORGE CARGILL

I, D. George Cargill, as author of this report entitled “Technical Report on Paso Yobai Project, Uraguay” prepared for Latin American Minerals Inc. and dated February 15, 2008 do hereby certify that:

1. I am President with Cargill Consulting Geologists Limited

of Suite 501, 55 University Ave Toronto, ON, M5J 2H7.

2. I am a graduate of University of Toronto 1967 B.ASc. Queens University 1970 M.Sc. University of B.C.. 1975 Ph.D.

3. I am registered as a Professional Engineer in the Provinces of Ontario (Reg.#

06870018) and British Columbia (Reg. #8109). I have worked as a geological engineer for more than 35 years since my graduation. My relevant experience for the purpose of the Technical Report is:

Island Copper, Cu-Mo-Au Property B.C Technical Reports Expo Cu-Mo-Au Property B.C. Technical and Exploration Reports Catface Property, Cu-Mo Property, B.C. Due Diligence Report Tulsequah Chief Au Property B.C. Due Diligence Report Oyu Tolgoy, Cu Property, Mongolia NI 43-101 Report Ivanhoe Cu-Au Properties, Inner Mongolia NI 43-101 Report RTB Bor Cu-Au Property Serbia Due Diligence Report Aurora Au Property, Guyana NI 43-101 Report Peters Au Property, Guyana NI 43-101 Report Zalantun Au Project, China NI 43-101 Report Cu- Au Porphyry, Inner Mongolia NI 43-101 Report Cu-Au Porphyry , Heilongjinag Due Diligence Examination

4. I have read the definition of "qualified person" set out in National Instrument 43-101 (NI43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of NI43-101.

5. I visited the Paso Yobai Project on October 2 to 4, 2007 and on January 5 to 9, 2008.

6. I am responsible for overall preparation/preparation of the Technical Report.

70

7. I am independent of the Issuer applying the test set out in Section 1.4 of National Instrument 43-101.

8. I have had no prior involvement with the property that is the subject of the Technical Report.

9. I have read National Instrument 43-101, and the Technical Report has been prepared in compliance with National Instrument 43-101 and Form 43-101F1.

10. To the best of my knowledge, information, and belief, the Technical Report contains all scientific and technical information that is required to be disclosed to make the technical report not misleading. Dated 15th day of February, 2008 (Signed) D. George Cargill, Ph.D., P.Eng.

1-1

APPENDIX 1 COMPLETE DRILL HOLE GOLD ASSAYS

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_01

1618

2000

920

07-0

.01

DD

H_L

AT_

0118

2020

010

2007

-0.0

1D

DH

_LA

T_01

2022

2001

120

07-0

.01

DD

H_L

AT_

0120

012

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_01

2224

2001

320

07-0

.01

DD

H_L

AT_

0124

2620

014

2007

-0.0

1-0

.01

DD

H_L

AT_

0126

2820

015

2007

-0.0

1D

DH

_LA

T_01

2830

2001

620

07-0

.01

DD

H_L

AT_

010

220

001

2007

0.03

DD

H_L

AT_

012

420

002

2007

0.01

DD

H_L

AT_

014

620

003

2007

-0.0

1D

DH

_LA

T_01

68

2000

420

070.

01-0

.01

DD

H_L

AT_

018

1020

005

2007

0.03

DD

H_L

AT_

0110

1220

006

2007

0.03

0.05

DD

H_L

AT_

0112

1420

007

2007

0.39

0.41

DD

H_L

AT_

0114

1620

008

2007

0.08

0.06

DD

H_L

AT_

0130

3220

017

2007

-0.0

1D

DH

_LA

T_01

3234

2001

820

07-0

.01

DD

H_L

AT_

0134

3620

019

2007

-0.0

1D

DH

_LA

T_01

3638

2002

020

07-0

.01

DD

H_L

AT_

0138

4020

021

2007

0.02

DD

H_L

AT_

0140

4220

022

2007

-0.0

1D

DH

_LA

T_01

4244

2002

320

07-0

.01

DD

H_L

AT_

0144

4620

024

2007

-0.0

1D

DH

_LA

T_01

2002

5B

LAN

CO

2007

-0.0

1-0

.01

DD

H_L

AT_

0146

4820

026

2007

-0.0

1D

DH

_LA

T_01

4850

2002

720

07-0

.01

DD

H_L

AT_

0150

5220

028

2007

-0.0

1D

DH

_LA

T_01

5254

2002

920

07-0

.01

DD

H_L

AT_

0154

5620

030

2007

0.01

DD

H_L

AT_

0120

031

STD

-CD

N-G

S-2

B20

072.

08D

DH

_LA

T_01

5658

2003

220

07-0

.01

DD

H_L

AT_

0158

6020

033

2007

-0.0

1D

DH

_LA

T_01

6062

2003

420

07-0

.01

-0.0

1D

DH

_LA

T_01

6264

2003

520

07-0

.01

DD

H_L

AT_

0164

6620

036

2007

-0.0

1D

DH

_LA

T_01

6668

2003

720

07-0

.01

DD

H_L

AT_

0168

7020

038

2007

-0.0

1

Pag

e 1

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_01

7072

2003

920

07-0

.01

DD

H_L

AT_

0172

7420

040

2007

-0.0

1D

DH

_LA

T_01

7476

2004

120

07-0

.01

DD

H_L

AT_

0176

7820

042

2007

-0.0

1D

DH

_LA

T_01

7880

2004

320

07-0

.01

DD

H_L

AT_

0180

8220

044

2007

0.16

0.17

DD

H_L

AT_

0182

8420

045

2007

0.07

DD

H_L

AT_

0184

8620

046

2007

0.05

DD

H_L

AT_

0186

8820

047

2007

-0.0

1D

DH

_LA

T_01

8890

2004

820

070.

09D

DH

_LA

T_01

9092

2004

920

070.

01D

DH

_LA

T_01

9294

2005

020

075.

966.

29

DD

H_L

AT_

0120

051

DU

PLI

CA

DO

2007

0.66

0.68

DD

H_L

AT_

0194

9620

052

2007

0.05

0.1

DD

H_L

AT_

0196

9820

053

2007

0.51

0.6

DD

H_L

AT_

0198

100

2005

420

070.

020.

03D

DH

_LA

T_01

100

102

2005

520

070.

410.

63D

DH

_LA

T_01

102

104

2005

620

07-0

.01

DD

H_L

AT_

0110

410

620

057

2007

-0.0

1D

DH

_LA

T_01

106

108

2005

820

07-0

.01

DD

H_L

AT_

0110

811

020

059

2007

-0.0

1D

DH

_LA

T_01

110

112

2006

020

07-0

.01

DD

H_L

AT_

0111

211

420

061

2007

-0.0

1D

DH

_LA

T_01

114

116

2006

220

07-0

.01

DD

H_L

AT_

0111

611

820

063

2007

-0.0

1-0

.01

DD

H_L

AT_

0111

812

020

064

2007

0.01

DD

H_L

AT_

0120

065

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0120

066

STD

-CD

N-G

S-

1P5B

2007

1.57

DD

H_L

AT_

0112

012

220

067

2007

-0.0

1D

DH

_LA

T_01

122

124

2006

820

07-0

.01

DD

H_L

AT_

0112

412

620

069

2007

-0.0

1D

DH

_LA

T_01

126

128

2007

020

07-0

.01

DD

H_L

AT_

0112

813

020

071

2007

-0.0

1D

DH

_LA

T_01

130

132

2007

220

07-0

.01

DD

H_L

AT_

0113

213

420

073

2007

-0.0

1D

DH

_LA

T_01

134

136

2007

420

07-0

.01

-0.0

1D

DH

_LA

T_01

136

137.

920

075

2007

-0.0

1

Pag

e 2

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_02

02

2007

620

070.

02D

DH

_LA

T_02

24

2007

720

070.

01D

DH

_LA

T_02

46

2007

820

07-0

.01

DD

H_L

AT_

026

820

079

2007

0.02

DD

H_L

AT_

028

1020

080

2007

0.08

DD

H_L

AT_

0210

1220

081

2007

0.16

DD

H_L

AT_

0212

1420

082

2007

-0.0

1D

DH

_LA

T_02

1416

.720

083

2007

-0.0

10.

01D

DH

_LA

T_02

16.7

18.3

2008

420

07-0

.01

DD

H_L

AT_

0218

.319

.45

2008

520

07-0

.01

DD

H_L

AT_

0219

.45

20.4

2008

620

070.

03D

DH

_LA

T_02

20.4

21.3

2008

720

070.

09D

DH

_LA

T_02

21.3

23.3

2008

820

07-0

.01

DD

H_L

AT_

0220

089

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_02

23.3

25.1

2009

020

07-0

.01

DD

H_L

AT_

0225

.127

.15

2009

120

07-0

.01

DD

H_L

AT_

0220

092

BLA

NC

O20

07-0

.01

-0.0

1D

DH

_LA

T_02

27.1

529

2009

320

07-0

.01

DD

H_L

AT_

0229

31.1

2009

420

070.

04D

DH

_LA

T_02

2009

5S

TD-C

DN

-GS

-2B

2007

2.13

DD

H_L

AT_

0231

.133

.120

096

2007

-0.0

1D

DH

_LA

T_02

33.1

3520

097

2007

-0.0

1D

DH

_LA

T_02

35.1

3720

098

2007

-0.0

1D

DH

_LA

T_02

3739

2009

920

07-0

.01

DD

H_L

AT_

0239

4120

100

2007

-0.0

1D

DH

_LA

T_02

4143

2010

120

07-0

.01

DD

H_L

AT_

0243

4520

102

2007

-0.0

1D

DH

_LA

T_02

4547

2010

320

07-0

.01

DD

H_L

AT_

0247

4920

104

2007

-0.0

1D

DH

_LA

T_02

4951

2010

520

07-0

.01

-0.0

1D

DH

_LA

T_02

5153

2010

620

07-0

.01

DD

H_L

AT_

0253

5520

107

2007

-0.0

1D

DH

_LA

T_02

5557

2010

820

07-0

.01

DD

H_L

AT_

0257

5920

109

2007

-0.0

1D

DH

_LA

T_02

5961

2011

020

07-0

.01

DD

H_L

AT_

0261

6320

111

2007

-0.0

1D

DH

_LA

T_02

6365

2011

220

07-0

.01

DD

H_L

AT_

0265

6720

113

2007

-0.0

1-0

.01

DD

H_L

AT_

0267

6920

114

2007

-0.0

1

Pag

e 1

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_02

2011

5D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0269

7120

116

2007

-0.0

1D

DH

_LA

T_02

7173

2011

720

07-0

.01

DD

H_L

AT_

0273

7520

118

2007

-0.0

1D

DH

_LA

T_02

7577

2011

920

07-0

.01

DD

H_L

AT_

0277

7920

120

2007

-0.0

1D

DH

_LA

T_02

7981

2012

120

07-0

.01

DD

H_L

AT_

0220

122

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0281

8320

123

2007

-0.0

1D

DH

_LA

T_02

8385

2012

420

07-0

.01

DD

H_L

AT_

0285

8720

125

2007

-0.0

1D

DH

_LA

T_02

8789

2012

620

070.

010.

01D

DH

_LA

T_02

8991

2012

720

07-0

.01

DD

H_L

AT_

0291

9320

128

2007

-0.0

1

DD

H_L

AT_

0220

129

STD

-CD

N-G

S-

1P5B

2007

1.56

1.58

DD

H_L

AT_

0293

9520

130

2007

-0.0

1D

DH

_LA

T_02

9597

2013

120

07-0

.01

DD

H_L

AT_

0297

9920

132

2007

-0.0

1D

DH

_LA

T_02

9910

120

133

2007

-0.0

1D

DH

_LA

T_02

101

103

2013

420

070.

01D

DH

_LA

T_02

103

104

2013

520

07-0

.01

DD

H_L

AT_

0210

510

520

136

2007

-0.0

1D

DH

_LA

T_02

105

106

2013

720

07-0

.01

DD

H_L

AT_

0210

610

720

138

2007

-0.0

1D

DH

_LA

T_02

107

108

2013

920

07-0

.01

0.01

DD

H_L

AT_

0210

810

920

140

2007

0.04

DD

H_L

AT_

0210

910

9.5

2014

120

070.

04D

DH

_LA

T_02

109.

511

120

142

2007

-0.0

1D

DH

_LA

T_02

111

112

2014

320

07-0

.01

DD

H_L

AT_

0211

211

320

144

2007

-0.0

1D

DH

_LA

T_02

113

114

2014

520

07-0

.01

DD

H_L

AT_

0211

411

520

146

2007

-0.0

1

DD

H_L

AT_

0220

147

STD

-CD

N-G

S-P

5B20

070.

46D

DH

_LA

T_02

115

116

2014

820

07-0

.01

-0.0

1D

DH

_LA

T_02

116

117

2014

920

07-0

.01

DD

H_L

AT_

0211

711

820

150

2007

-0.0

1D

DH

_LA

T_02

119

120

2015

120

07-0

.01

Pag

e 2

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_02

120

121

2015

220

07-0

.01

DD

H_L

AT_

0212

112

220

153

2007

-0.0

1D

DH

_LA

T_02

122

123

2015

420

07-0

.01

DD

H_L

AT_

0212

312

420

155

2007

-0.0

1D

DH

_LA

T_02

2015

6B

LAN

CO

2007

-0.0

1D

DH

_LA

T_02

124

125

2015

720

070.

04D

DH

_LA

T_02

125

126

2015

820

07-0

.01

DD

H_L

AT_

0212

612

720

159

2007

0.09

DD

H_L

AT_

0212

712

820

160

2007

-0.0

1D

DH

_LA

T_02

128

129

2016

120

07-0

.01

-0.0

1D

DH

_LA

T_02

129

130

2016

220

07-0

.01

DD

H_L

AT_

0213

013

120

163

2007

-0.0

1D

DH

_LA

T_02

131

132

2016

420

07-0

.01

DD

H_L

AT_

0220

165

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_02

132

133

2016

620

07-0

.01

DD

H_L

AT_

0213

313

420

167

2007

0.04

DD

H_L

AT_

0213

413

520

168

2007

-0.0

1-0

.01

DD

H_L

AT_

0213

513

620

169

2007

-0.0

1D

DH

_LA

T_02

136

137

2017

020

07-0

.01

DD

H_L

AT_

0213

713

920

171

2007

-0.0

1D

DH

_LA

T_02

139

141

2017

220

07-0

.01

DD

H_L

AT_

0214

114

320

173

2007

-0.0

1D

DH

_LA

T_02

143

145

2017

420

070.

02D

DH

_LA

T_02

145

147

2017

520

07-0

.01

DD

H_L

AT_

0214

714

920

176

2007

-0.0

1D

DH

_LA

T_02

149

151

2017

720

07-0

.01

DD

H_L

AT_

0220

178

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0215

115

320

179

2007

-0.0

1D

DH

_LA

T_02

153

155

2018

020

07-0

.01

DD

H_L

AT_

0215

515

720

181

2007

-0.0

1-0

.01

DD

H_L

AT_

0215

715

920

182

2007

-0.0

1D

DH

_LA

T_02

159

161

2018

320

07-0

.01

DD

H_L

AT_

0216

116

3.3

2018

420

07-0

.01

DD

H_L

AT_

0216

3.3

164

2018

520

07-0

.01

DD

H_L

AT_

0216

4.3

165.

320

186

2007

-0.0

1

Pag

e 3

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_03

03

2018

720

070.

74D

DH

_LA

T_03

35

2018

820

070.

03D

DH

_LA

T_03

2018

9S

TD-C

DN

-GS

-2B

2007

2.01

DD

H_L

AT_

035

720

190

2007

-0.0

10.

01D

DH

_LA

T_03

79

2019

120

070.

01D

DH

_LA

T_03

911

2019

220

07-0

.01

DD

H_L

AT_

0311

1320

193

2007

-0.0

1D

DH

_LA

T_03

2019

4D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0313

1520

195

2007

0.05

DD

H_L

AT_

0315

1720

196

2007

-0.0

1D

DH

_LA

T_03

1719

2019

720

07-0

.01

DD

H_L

AT_

0319

2120

198

2007

-0.0

1D

DH

_LA

T_03

2123

2019

920

07-0

.01

DD

H_L

AT_

0323

2520

200

2007

-0.0

1D

DH

_LA

T_03

2527

2020

120

07-0

.01

-0.0

1D

DH

_LA

T_03

2729

2020

220

07-0

.01

DD

H_L

AT_

0329

3120

203

2007

-0.0

1D

DH

_LA

T_03

3133

2020

420

07-0

.01

DD

H_L

AT_

0333

3520

205

2007

0.03

DD

H_L

AT_

0335

3720

206

2007

-0.0

1D

DH

_LA

T_03

3739

2020

720

070.

01D

DH

_LA

T_03

3941

2020

820

07-0

.01

DD

H_L

AT_

0341

4320

209

2007

-0.0

1D

DH

_LA

T_03

2021

0B

LAN

CO

2007

0.01

DD

H_L

AT_

0343

4520

211

2007

-0.0

1D

DH

_LA

T_03

4547

2021

220

07-0

.01

-0.0

1D

DH

_LA

T_03

4749

2021

320

07-0

.01

DD

H_L

AT_

0349

5120

214

2007

-0.0

1D

DH

_LA

T_03

5153

2021

520

07-0

.01

DD

H_L

AT_

0353

5520

216

2007

-0.0

1D

DH

_LA

T_03

5557

2021

720

07-0

.01

DD

H_L

AT_

0357

5920

218

2007

-0.0

1D

DH

_LA

T_03

5961

2021

920

07-0

.01

DD

H_L

AT_

0361

6320

220

2007

-0.0

1D

DH

_LA

T_03

6365

2022

120

07-0

.01

-0.0

1

DD

H_L

AT_

0320

222

STD

-CD

N-G

S-

1P5B

2007

1.46

DD

H_L

AT_

0365

6720

223

2007

0.01

DD

H_L

AT_

0367

6920

224

2007

-0.0

1

Pag

e 1

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_03

6971

2022

520

070.

03D

DH

_LA

T_03

7173

2022

620

07-0

.01

DD

H_L

AT_

0373

7520

227

2007

-0.0

1D

DH

_LA

T_03

7577

2022

820

07-0

.01

DD

H_L

AT_

0377

7920

229

2007

-0.0

1D

DH

_LA

T_03

7981

2023

020

07-0

.01

DD

H_L

AT_

0320

231

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_03

8183

2023

220

07-0

.01

DD

H_L

AT_

0383

8520

233

2007

0.03

0.02

DD

H_L

AT_

0385

8720

234

2007

-0.0

1D

DH

_LA

T_03

8789

2023

520

07-0

.01

DD

H_L

AT_

0389

9120

236

2007

-0.0

1D

DH

_LA

T_03

9193

2023

720

070.

02D

DH

_LA

T_03

9395

2023

820

070.

53D

DH

_LA

T_03

9596

2023

920

070.

11D

DH

_LA

T_03

9696

.820

240

2007

-0.0

1D

DH

_LA

T_03

96.8

97.3

2024

120

07-0

.01

-0.0

1D

DH

_LA

T_03

97.3

9820

242

2007

-0.0

1D

DH

_LA

T_03

9899

2024

320

07-0

.01

DD

H_L

AT_

0399

100

2024

420

07-0

.01

DD

H_L

AT_

0310

010

120

245

2007

-0.0

1D

DH

_LA

T_03

101

102

2024

620

07-0

.01

DD

H_L

AT_

0320

247

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0310

210

320

248

2007

-0.0

1D

DH

_LA

T_03

103

104

2024

920

07-0

.01

DD

H_L

AT_

0310

410

520

250

2007

-0.0

1-0

.01

DD

H_L

AT_

0310

510

620

251

2007

-0.0

1D

DH

_LA

T_03

106

107

2025

220

07-0

.01

DD

H_L

AT_

0310

710

820

253

2007

-0.0

1D

DH

_LA

T_03

108

109

2025

420

07-0

.01

DD

H_L

AT_

0310

911

020

255

2007

-0.0

1D

DH

_LA

T_03

110

111

2025

620

070.

02

DD

H_L

AT_

0320

257

STD

-CD

N-G

S-P

5B20

070.

41D

DH

_LA

T_03

111

112

2025

820

07-0

.01

DD

H_L

AT_

0311

211

320

259

2007

13.0

212

.63

DD

H_L

AT_

0311

311

420

260

2007

-0.0

10.

01D

DH

_LA

T_03

114

115

2026

120

07-0

.01

DD

H_L

AT_

0311

511

620

262

2007

-0.0

1

Pag

e 2

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_03

116

117

2026

320

07-0

.01

DD

H_L

AT_

0320

264

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_03

117

118

2026

520

07-0

.01

DD

H_L

AT_

0311

811

920

266

2007

0.04

0.06

DD

H_L

AT_

0311

912

020

267

2007

0.02

DD

H_L

AT_

0312

012

120

268

2007

-0.0

1D

DH

_LA

T_03

121

122

2026

920

07-0

.01

DD

H_L

AT_

0312

212

320

270

2007

0.01

DD

H_L

AT_

0312

312

520

271

2007

0.12

0.04

DD

H_L

AT_

0312

512

720

272

2007

0.19

DD

H_L

AT_

0312

712

8.3

2027

320

070.

04

Pag

e 3

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_04

02

2027

420

070.

01D

DH

_LA

T_04

24

2027

520

070.

05D

DH

_LA

T_04

46

2027

620

070.

010.

01D

DH

_LA

T_04

68

2027

720

070.

04D

DH

_LA

T_04

810

2027

820

07-0

.01

DD

H_L

AT_

0420

279

DU

PLI

CA

DO

2007

0.02

DD

H_L

AT_

0410

1220

280

2007

-0.0

1D

DH

_LA

T_04

1214

2028

120

07-0

.01

DD

H_L

AT_

0414

1620

282

2007

-0.0

1D

DH

_LA

T_04

1618

2028

320

070.

02D

DH

_LA

T_04

1820

2028

420

07-0

.01

DD

H_L

AT_

0420

2220

285

2007

-0.0

1D

DH

_LA

T_04

2224

2028

620

07-0

.01

DD

H_L

AT_

0424

2620

287

2007

-0.0

1D

DH

_LA

T_04

2628

2028

820

07-0

.01

-0.0

1D

DH

_LA

T_04

2830

2028

920

070.

01D

DH

_LA

T_04

2029

0B

LAN

CO

2007

-0.0

1D

DH

_LA

T_04

3032

2029

120

070.

03D

DH

_LA

T_04

3234

2029

220

07-0

.01

-0.0

1D

DH

_LA

T_04

3436

2029

320

070.

01D

DH

_LA

T_04

3638

2029

420

07-0

.01

DD

H_L

AT_

0420

295

STD

-CD

N-G

S-2

B20

072.

132.

08D

DH

_LA

T_04

3840

2029

620

07-0

.01

DD

H_L

AT_

0440

4220

297

2007

0.03

DD

H_L

AT_

0442

4420

298

2007

-0.0

1D

DH

_LA

T_04

4446

2029

920

070.

02D

DH

_LA

T_04

4648

2030

020

070.

03D

DH

_LA

T_04

4850

2030

120

070.

04D

DH

_LA

T_04

5052

2030

220

07-0

.01

DD

H_L

AT_

0452

5420

303

2007

0.02

DD

H_L

AT_

0454

5620

304

2007

0.02

DD

H_L

AT_

0456

5820

305

2007

0.02

DD

H_L

AT_

0420

306

DU

PLI

CA

DO

2007

0.01

DD

H_L

AT_

0458

6020

307

2007

0.02

0.02

DD

H_L

AT_

0460

6220

308

2007

0.04

DD

H_L

AT_

0462

6420

309

2007

0.03

DD

H_L

AT_

0464

6620

310

2007

-0.0

1D

DH

_LA

T_04

6668

2031

120

07-0

.01

DD

H_L

AT_

0468

7020

312

2007

0.03

Pag

e 1

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_04

7072

2031

320

070.

01D

DH

_LA

T_04

2031

4B

LAN

CO

2007

-0.0

1D

DH

_LA

T_04

7274

2031

520

070.

02D

DH

_LA

T_04

7476

2031

620

070.

02D

DH

_LA

T_04

7678

2031

720

070.

04D

DH

_LA

T_04

7880

2031

820

070.

04D

DH

_LA

T_04

8082

2031

920

070.

040.

03D

DH

_LA

T_04

8284

2032

020

070.

02D

DH

_LA

T_04

8486

2032

120

070.

02D

DH

_LA

T_04

8688

2032

220

070.

02D

DH

_LA

T_04

8890

2032

320

070.

03

DD

H_L

AT_

0420

324

STD

-CD

N-G

S-

1P5B

2007

1.35

1.53

DD

H_L

AT_

0490

9220

325

2007

0.03

DD

H_L

AT_

0492

9420

326

2007

0.03

DD

H_L

AT_

0494

9620

327

2007

0.07

DD

H_L

AT_

0496

9820

328

2007

-0.0

1D

DH

_LA

T_04

9810

020

329

2007

0.01

DD

H_L

AT_

0410

010

220

330

2007

-0.0

1D

DH

_LA

T_04

102

104

2033

120

070.

020.

02D

DH

_LA

T_04

104

106

2033

220

07-0

.01

-0.0

1D

DH

_LA

T_04

106

108

2033

320

07-0

.01

DD

H_L

AT_

0410

811

020

334

2007

-0.0

1D

DH

_LA

T_04

110

112

2033

520

070.

02D

DH

_LA

T_04

112

114

2033

620

07-0

.01

DD

H_L

AT_

0411

411

620

337

2007

-0.0

1D

DH

_LA

T_04

2033

8B

LAN

CO

2007

-0.0

1D

DH

_LA

T_04

116

118

2033

920

07-0

.01

DD

H_L

AT_

0411

812

020

340

2007

-0.0

1-0

.01

DD

H_L

AT_

0412

012

220

341

2007

-0.0

1D

DH

_LA

T_04

122

124

2034

220

07-0

.01

DD

H_L

AT_

0412

412

520

343

2007

-0.0

1D

DH

_LA

T_04

125

126

2034

420

070.

04D

DH

_LA

T_04

126

127

2034

520

07-0

.01

DD

H_L

AT_

0412

712

820

346

2007

0.02

DD

H_L

AT_

0412

812

920

347

2007

0.01

DD

H_L

AT_

0420

348

STD

-CD

N-G

S-

1P5B

2007

1.66

DD

H_L

AT_

0412

913

020

349

2007

-0.0

1

Pag

e 2

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_04

130

131

2035

020

070.

15D

DH

_LA

T_04

131

132

2035

120

070.

070.

07D

DH

_LA

T_04

132

133

2035

220

070.

07D

DH

_LA

T_04

133

134

2035

320

070.

04D

DH

_LA

T_04

134

135

2035

420

070.

01D

DH

_LA

T_04

135

136

2035

520

07-0

.01

DD

H_L

AT_

0413

613

720

356

2007

-0.0

1D

DH

_LA

T_04

2035

7D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0413

713

820

358

2007

-0.0

1D

DH

_LA

T_04

138

139

2035

920

07-0

.01

DD

H_L

AT_

0413

914

020

360

2007

-0.0

1D

DH

_LA

T_04

140

141

2036

120

07-0

.01

-0.0

1D

DH

_LA

T_04

141

142

2036

220

07-0

.01

DD

H_L

AT_

0414

214

320

363

2007

-0.0

1D

DH

_LA

T_04

143

144

2036

420

07-0

.01

DD

H_L

AT_

0414

414

520

365

2007

0.02

DD

H_L

AT_

0414

514

620

366

2007

-0.0

1D

DH

_LA

T_04

146

147

2036

720

07-0

.01

DD

H_L

AT_

0414

714

820

368

2007

0.01

DD

H_L

AT_

0414

815

020

369

2007

0.01

DD

H_L

AT_

0415

015

2.7

2037

020

070.

040.

03D

DH

_LA

T_04

2037

1D

UP

LIC

AD

O20

070.

01

Pag

e 3

of 3

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_05

202.

9520

520

372

2007

0.02

DD

H_L

AT_

0520

520

6.4

2037

320

07-0

.01

DD

H_L

AT_

0520

6.4

207

2037

420

07-0

.01

DD

H_L

AT_

0520

375

BLA

NC

O20

07-0

.01

-0.0

1D

DH

_LA

T_05

207

208

2037

620

07-0

.01

DD

H_L

AT_

0520

820

920

377

2007

0.03

DD

H_L

AT_

0520

921

020

378

2007

-0.0

1D

DH

_LA

T_05

210

211

2037

920

07-0

.01

DD

H_L

AT_

0521

121

220

380

2007

-0.0

1D

DH

_LA

T_05

212

213

2038

120

070.

01D

DH

_LA

T_05

213

214

2038

220

07-0

.01

DD

H_L

AT_

0521

421

420

383

2007

0.02

DD

H_L

AT_

0520

384

STD

-CD

N-G

S-2

B20

071.

691.

86D

DH

_LA

T_05

215

216

2038

520

070.

01D

DH

_LA

T_05

216

217

2038

620

07-0

.01

DD

H_L

AT_

0521

721

820

387

2007

-0.0

1D

DH

_LA

T_05

218

219

2038

820

07-0

.01

DD

H_L

AT_

0521

922

020

389

2007

0.02

DD

H_L

AT_

0522

022

120

390

2007

0.02

DD

H_L

AT_

0522

122

220

391

2007

0.04

DD

H_L

AT_

0522

222

320

392

2007

-0.0

1D

DH

_LA

T_05

223

224

2039

320

070.

01D

DH

_LA

T_05

224

225

2039

420

07-0

.01

DD

H_L

AT_

0522

522

620

395

2007

-0.0

1-0

.01

DD

H_L

AT_

0522

622

720

396

2007

-0.0

1D

DH

_LA

T_05

227

227.

8520

397

2007

-0.0

1D

DH

_LA

T_05

03

2045

120

07D

DH

_LA

T_05

35

2045

220

07D

DH

_LA

T_05

2045

3B

LAN

CO

2007

DD

H_L

AT_

055

720

454

2007

DD

H_L

AT_

057

920

455

2007

DD

H_L

AT_

059

1120

456

2007

DD

H_L

AT_

0511

1320

457

2007

DD

H_L

AT_

0520

458

STD

-CD

N-G

S-P

5B20

07D

DH

_LA

T_05

200

201

2045

920

07D

DH

_LA

T_05

201

202

2046

020

07

Pag

e 1

of 1

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_06

87.7

589

2039

820

070.

01D

DH

_LA

T_06

8990

2039

920

070.

01D

DH

_LA

T_06

2040

0D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0690

9120

401

2007

0.02

DD

H_L

AT_

0691

9220

402

2007

-0.0

1-0

.01

DD

H_L

AT_

0692

9320

403

2007

-0.0

1D

DH

_LA

T_06

9394

2040

420

07-0

.01

DD

H_L

AT_

0694

9520

405

2007

-0.0

1D

DH

_LA

T_06

9596

2040

620

07-0

.01

DD

H_L

AT_

0696

9820

407

2007

-0.0

1D

DH

_LA

T_06

9798

2040

820

07-0

.01

DD

H_L

AT_

0698

9920

409

2007

-0.0

1D

DH

_LA

T_06

9910

020

410

2007

-0.0

1D

DH

_LA

T_06

100

101

2041

120

071.

27D

DH

_LA

T_06

101

102

2041

220

070.

030.

02D

DH

_LA

T_06

102

103

2041

320

070.

01D

DH

_LA

T_06

103

104

2041

420

07-0

.01

DD

H_L

AT_

0610

410

520

415

2007

-0.0

1D

DH

_LA

T_06

105

106

2041

620

07-0

.01

DD

H_L

AT_

0610

610

720

417

2007

-0.0

1D

DH

_LA

T_06

107

108

2041

820

07-0

.01

DD

H_L

AT_

0610

810

920

419

2007

-0.0

1D

DH

_LA

T_06

109

110

2042

020

070.

24D

DH

_LA

T_06

110

111

2042

120

07-0

.01

DD

H_L

AT_

0611

111

220

422

2007

0.35

DD

H_L

AT_

0620

423

BLA

NC

O20

07-0

.01

-0.0

1D

DH

_LA

T_06

112

113

2042

420

079.

13D

DH

_LA

T_06

113

114

2042

520

0737

.86

DD

H_L

AT_

0611

411

520

426

2007

1.11

DD

H_L

AT_

0620

427

STD

-CD

N-G

S_2

B20

071.

99D

DH

_LA

T_06

115

116

2042

820

0725

.22

DD

H_L

AT_

0611

611

720

429

2007

0.11

DD

H_L

AT_

0611

711

820

430

2007

0.97

0.7

DD

H_L

AT_

0611

811

920

431

2007

-0.0

1D

DH

_LA

T_06

119

120

2043

220

07-0

.01

DD

H_L

AT_

0612

012

120

433

2007

-0.0

1D

DH

_LA

T_06

121

122

2043

420

07-0

.01

DD

H_L

AT_

0612

212

320

435

2007

-0.0

1-0

.01

DD

H_L

AT_

0612

312

420

436

2007

-0.0

1D

DH

_LA

T_06

124

125

2043

720

070.

04

Pag

e 1

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_06

125

126

2043

820

070.

28D

DH

_LA

T_06

126

127

2043

920

07-0

.01

DD

H_L

AT_

0612

712

820

440

2007

-0.0

1D

DH

_LA

T_06

128

129

2044

120

07-0

.01

DD

H_L

AT_

0612

913

020

442

2007

-0.0

1D

DH

_LA

T_06

130

131

2044

320

07-0

.01

DD

H_L

AT_

0613

113

220

444

2007

-0.0

1-0

.01

DD

H_L

AT_

0613

213

320

445

2007

-0.0

1D

DH

_LA

T_06

133

134

2044

620

07-0

.01

DD

H_L

AT_

0613

413

520

447

2007

0.35

DD

H_L

AT_

0613

513

7.8

2044

820

070.

02D

DH

_LA

T_06

137.

813

9.8

2044

920

07-0

.01

DD

H_L

AT_

0613

9.8

140.

7620

450

2007

-0.0

1

Pag

e 2

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_07

212.

8321

3.6

2046

320

07-0

.01

DD

H_L

AT_

0721

3.6

214.

120

464

2007

-0.0

1-0

.01

DD

H_L

AT_

0721

4.1

215

2046

520

07-0

.01

DD

H_L

AT_

0721

521

5.57

2046

620

07-0

.01

DD

H_L

AT_

0721

5.57

216.

5220

467

2007

-0.0

1D

DH

_LA

T_07

216.

5221

720

468

2007

-0.0

1D

DH

_LA

T_07

217

218

2046

920

07-0

.01

DD

H_L

AT_

0721

821

920

470

2007

-0.0

1D

DH

_LA

T_07

219

220

2047

120

07-0

.01

DD

H_L

AT_

0722

022

120

472

2007

-0.0

1D

DH

_LA

T_07

221

222

2047

320

07-0

.01

DD

H_L

AT_

0720

474

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_07

222

223

2047

520

07-0

.01

DD

H_L

AT_

0722

322

420

476

2007

-0.0

1D

DH

_LA

T_07

224

225

2047

720

07-0

.01

DD

H_L

AT_

0722

522

620

478

2007

-0.0

1-0

.01

DD

H_L

AT_

0722

622

720

479

2007

-0.0

1D

DH

_LA

T_07

227

228

2048

020

07-0

.01

DD

H_L

AT_

0722

822

920

481

2007

-0.0

1D

DH

_LA

T_07

2048

2B

LAN

CO

2007

-0.0

1D

DH

_LA

T_07

229

230

2048

320

07-0

.01

DD

H_L

AT_

0723

023

120

484

2007

-0.0

1D

DH

_LA

T_07

231

232

2048

520

07-0

.01

DD

H_L

AT_

0723

223

320

486

2007

-0.0

1D

DH

_LA

T_07

233

234

2048

720

07-0

.01

DD

H_L

AT_

0723

423

520

488

2007

-0.0

1D

DH

_LA

T_07

235

236

2048

920

07-0

.01

DD

H_L

AT_

0742

.15

42.8

820

490

2007

0.01

DD

H_L

AT_

0720

491

STD

- C

DN

-GS

-1P

5B20

071.

671.

7D

DH

_LA

T_07

43.9

444

.920

492

2007

-0.0

1D

DH

_LA

T_07

4747

.820

493

2007

-0.0

1-0

.01

DD

H_L

AT_

0749

49.6

820

494

2007

-0.0

1D

DH

_LA

T_07

49.6

850

.620

495

2007

-0.0

1D

DH

_LA

T_07

236

237

2049

620

07-0

.01

DD

H_L

AT_

0723

723

820

497

2007

-0.0

1D

DH

_LA

T_07

238

239

2049

820

07-0

.01

DD

H_L

AT_

0723

924

020

499

2007

-0.0

1D

DH

_LA

T_07

240

241

2050

020

07-0

.01

DD

H_L

AT_

0724

124

220

501

2007

-0.0

1-0

.01

Pag

e 1

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_07

242

243

2050

220

07-0

.01

DD

H_L

AT_

0724

324

420

503

2007

-0.0

1D

DH

_LA

T_07

244

245

2050

420

07-0

.01

DD

H_L

AT_

0724

524

620

505

2007

-0.0

1D

DH

_LA

T_07

246

247

2050

620

07-0

.01

DD

H_L

AT_

0720

507

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0724

724

820

508

2007

-0.0

1D

DH

_LA

T_07

248

249

2050

920

07-0

.01

DD

H_L

AT_

0724

925

020

510

2007

-0.0

1D

DH

_LA

T_07

250

251

2051

120

07-0

.01

DD

H_L

AT_

0725

125

220

512

2007

-0.0

1D

DH

_LA

T_07

252

253

2051

320

07-0

.01

DD

H_L

AT_

0725

325

420

514

2007

-0.0

1D

DH

_LA

T_07

254

255

2051

520

07-0

.01

DD

H_L

AT_

0725

525

620

516

2007

-0.0

1D

DH

_LA

T_07

2051

7D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0725

625

720

518

2007

-0.0

1D

DH

_LA

T_07

257

258

2051

920

070.

01D

DH

_LA

T_07

258

259

2052

020

07-0

.01

-0.0

1D

DH

_LA

T_07

259

260

2052

120

07-0

.01

DD

H_L

AT_

0726

026

120

522

2007

-0.0

1

DD

H_L

AT_

0720

523

STD

-CD

N-G

S-1

P5B

2007

1.62

DD

H_L

AT_

0726

126

220

524

2007

-0.0

1D

DH

_LA

T_07

262

263

2052

520

070.

02D

DH

_LA

T_07

263

263.

920

526

2007

-0.0

1

Pag

e 2

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_08

02

2052

720

07-0

.01

DD

H_L

AT_

082

420

528

2007

-0.0

1D

DH

_LA

T_08

46

2052

920

07-0

.01

DD

H_L

AT_

086

820

530

2007

-0.0

1D

DH

_LA

T_08

810

2053

120

07-0

.01

DD

H_L

AT_

0810

1220

532

2007

-0.0

1-0

.01

DD

H_L

AT_

0812

1420

533

2007

-0.0

1D

DH

_LA

T_08

1416

2053

420

070.

01D

DH

_LA

T_08

1618

2053

520

07-0

.01

DD

H_L

AT_

0818

2020

536

2007

0.01

DD

H_L

AT_

0820

537

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_08

2022

2053

820

07-0

.01

DD

H_L

AT_

0822

2420

539

2007

-0.0

1D

DH

_LA

T_08

2426

2054

020

07-0

.01

DD

H_L

AT_

0826

2820

541

2007

-0.0

1D

DH

_LA

T_08

2830

2054

220

07-0

.01

DD

H_L

AT_

0830

3220

543

2007

0.14

DD

H_L

AT_

0832

3420

544

2007

0.09

DD

H_L

AT_

0834

3620

545

2007

0.02

DD

H_L

AT_

0836

3820

546

2007

0.05

0.05

DD

H_L

AT_

0820

547

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0838

4020

548

2007

-0.0

1D

DH

_LA

T_08

4042

2054

920

070.

04D

DH

_LA

T_08

4244

2055

020

07-0

.01

DD

H_L

AT_

0844

4620

551

2007

0.02

DD

H_L

AT_

0846

4820

552

2007

-0.0

1D

DH

_LA

T_08

4850

2055

320

07-0

.01

DD

H_L

AT_

0850

5220

554

2007

-0.0

1D

DH

_LA

T_08

2055

5S

TD-C

DN

-GS

-2B

2007

2.13

2.11

DD

H_L

AT_

0852

5420

556

2007

-0.0

1-0

.01

DD

H_L

AT_

0854

5620

557

2007

-0.0

1D

DH

_LA

T_08

5658

2055

820

07-0

.01

DD

H_L

AT_

0858

6020

559

2007

-0.0

1D

DH

_LA

T_08

6062

2056

020

07-0

.01

DD

H_L

AT_

0862

6420

561

2007

-0.0

1D

DH

_LA

T_08

6466

2056

220

07-0

.01

DD

H_L

AT_

0866

6820

563

2007

-0.0

1D

DH

_LA

T_08

6870

2056

420

07-0

.01

DD

H_L

AT_

0870

7220

565

2007

-0.0

1D

DH

_LA

T_08

7274

2056

620

07-0

.01

Pag

e 1

of 5

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_08

7476

2056

720

07-0

.01

-0.0

1D

DH

_LA

T_08

7678

2056

820

07-0

.01

DD

H_L

AT_

0878

8020

569

2007

-0.0

1D

DH

_LA

T_08

8082

2057

020

07-0

.01

DD

H_L

AT_

0882

8420

571

2007

-0.0

1D

DH

_LA

T_08

2057

2D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0884

8620

573

2007

-0.0

1D

DH

_LA

T_08

8688

2057

420

07-0

.01

DD

H_L

AT_

0888

9020

575

2007

-0.0

1D

DH

_LA

T_08

9092

2057

620

07-0

.01

DD

H_L

AT_

0892

9420

577

2007

-0.0

1D

DH

_LA

T_08

9496

2057

820

07-0

.01

DD

H_L

AT_

0896

9820

579

2007

-0.0

1-0

.01

DD

H_L

AT_

0820

580

BLA

NC

O20

07-0

.01

DD

H_L

AT_

0898

100

2058

120

07-0

.01

DD

H_L

AT_

0810

010

220

582

2007

-0.0

1D

DH

_LA

T_08

102

104

2058

320

07-0

.01

DD

H_L

AT_

0810

410

620

584

2007

0.02

DD

H_L

AT_

0810

610

820

585

2007

0.02

DD

H_L

AT_

0810

811

020

586

2007

-0.0

1D

DH

_LA

T_08

110

112

2058

720

07-0

.01

DD

H_L

AT_

0811

211

420

588

2007

-0.0

1-0

.01

DD

H_L

AT_

0811

411

620

589

2007

-0.0

1D

DH

_LA

T_08

116

118

2059

020

07-0

.01

DD

H_L

AT_

0820

591

STD

-CD

N-G

S-1

P5B

2007

1.61

DD

H_L

AT_

0811

812

020

592

2007

-0.0

1D

DH

_LA

T_08

120

122

2059

320

07-0

.01

DD

H_L

AT_

0812

212

420

594

2007

-0.0

1D

DH

_LA

T_08

124

126

2059

520

070.

05D

DH

_LA

T_08

126

128

2059

620

07-0

.01

DD

H_L

AT_

0812

813

020

597

2007

-0.0

1D

DH

_LA

T_08

130

132

2059

820

07-0

.01

DD

H_L

AT_

0813

213

420

599

2007

-0.0

1D

DH

_LA

T_08

134

136

2060

020

07-0

.01

-0.0

1D

DH

_LA

T_08

136

138

2060

120

070.

02D

DH

_LA

T_08

138

140

2060

220

070.

03D

DH

_LA

T_08

140

142

2060

320

070.

02D

DH

_LA

T_08

142

144

2060

420

07-0

.01

DD

H_L

AT_

0814

414

620

605

2007

-0.0

1

Pag

e 2

of 5

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_08

2060

6D

UP

LIC

AD

O20

07-0

.01

DD

H_L

AT_

0814

614

820

607

2007

-0.0

1D

DH

_LA

T_08

148

150

2060

820

07-0

.01

DD

H_L

AT_

0815

015

220

609

2007

-0.0

1D

DH

_LA

T_08

152

154

2061

020

07-0

.01

-0.0

1D

DH

_LA

T_08

154

156

2061

120

07-0

.01

DD

H_L

AT_

0815

615

820

612

2007

-0.0

1D

DH

_LA

T_08

2061

3B

LAN

CO

2007

-0.0

1D

DH

_LA

T_08

158

160

2061

420

07-0

.01

DD

H_L

AT_

0816

016

220

615

2007

-0.0

1D

DH

_LA

T_08

162

164

2061

620

07-0

.01

DD

H_L

AT_

0816

416

620

617

2007

-0.0

1D

DH

_LA

T_08

166

168

2061

820

07-0

.01

DD

H_L

AT_

0816

817

020

619

2007

-0.0

1D

DH

_LA

T_08

170

172

2062

020

07-0

.01

DD

H_L

AT_

0817

217

420

621

2007

-0.0

1D

DH

_LA

T_08

174

176

2062

220

07-0

.01

DD

H_L

AT_

0820

623

STD

-CD

N-G

S-2

B20

072.

262.

14D

DH

_LA

T_08

176

178

2062

420

07-0

.01

DD

H_L

AT_

0817

818

020

625

2007

-0.0

1D

DH

_LA

T_08

180

182

2062

620

07-0

.01

DD

H_L

AT_

0818

218

420

627

2007

-0.0

1D

DH

_LA

T_08

184

186

2062

820

07-0

.01

DD

H_L

AT_

0818

618

820

629

2007

-0.0

1D

DH

_LA

T_08

188

190

2063

020

07-0

.01

DD

H_L

AT_

0819

019

220

631

2007

-0.0

1D

DH

_LA

T_08

192

194

2063

220

07-0

.01

DD

H_L

AT_

0819

419

620

633

2007

-0.0

1D

DH

_LA

T_08

196

198

2063

420

07-0

.01

-0.0

1D

DH

_LA

T_08

198

200

2063

520

07-0

.01

DD

H_L

AT_

0820

636

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_08

200

202

2063

720

07-0

.01

DD

H_L

AT_

0820

220

420

638

2007

-0.0

1D

DH

_LA

T_08

204

206

2063

920

07-0

.01

DD

H_L

AT_

0820

620

820

640

2007

-0.0

1D

DH

_LA

T_08

208

210

2064

120

07-0

.01

DD

H_L

AT_

0821

021

220

642

2007

-0.0

1D

DH

_LA

T_08

212

214

2064

320

07-0

.01

-0.0

1D

DH

_LA

T_08

214

216

2064

420

07-0

.01

DD

H_L

AT_

0821

621

820

645

2007

-0.0

1

Pag

e 3

of 5

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_08

218

220

2064

620

07-0

.01

DD

H_L

AT_

0822

022

220

647

2007

-0.0

1D

DH

_LA

T_08

2064

8B

LAN

CO

2007

-0.0

1D

DH

_LA

T_08

222

224

2064

920

07-0

.01

DD

H_L

AT_

0822

422

620

650

2007

-0.0

1D

DH

_LA

T_08

226

228

2065

120

07-0

.01

DD

H_L

AT_

0822

823

020

652

2007

-0.0

1D

DH

_LA

T_08

230

232

2065

320

07-0

.01

DD

H_L

AT_

0823

223

420

654

2007

-0.0

1D

DH

_LA

T_08

234

236

2065

520

07-0

.01

-0.0

1D

DH

_LA

T_08

236

238

2065

620

07-0

.01

DD

H_L

AT_

0823

824

020

657

2007

-0.0

1

DD

H_L

AT_

0820

658

STD

-CD

N-G

S-1

P5B

2007

1.64

1.63

DD

H_L

AT_

0824

024

220

659

2007

-0.0

1D

DH

_LA

T_08

242

244

2066

020

07-0

.01

DD

H_L

AT_

0824

424

620

661

2007

-0.0

1D

DH

_LA

T_08

246

248

2066

220

07-0

.01

DD

H_L

AT_

0824

825

020

663

2007

-0.0

1D

DH

_LA

T_08

250

252

2066

420

07-0

.01

-0.0

1D

DH

_LA

T_08

252

254

2066

520

07-0

.01

DD

H_L

AT_

0825

425

620

666

2007

-0.0

1D

DH

_LA

T_08

256

258

2066

720

07-0

.01

DD

H_L

AT_

0825

826

020

668

2007

-0.0

1D

DH

_LA

T_08

260

262

2066

920

07-0

.01

DD

H_L

AT_

0820

670

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_08

262

264

2067

120

07-0

.01

DD

H_L

AT_

0826

426

620

672

2007

-0.0

1D

DH

_LA

T_08

266

268

2067

320

07-0

.01

-0.0

1D

DH

_LA

T_08

268

270

2067

420

07-0

.01

DD

H_L

AT_

0827

027

220

675

2007

-0.0

1D

DH

_LA

T_08

272

274

2067

620

07-0

.01

DD

H_L

AT_

0827

427

620

677

2007

-0.0

1D

DH

_LA

T_08

276

278

2067

820

07-0

.01

DD

H_L

AT_

0827

828

020

679

2007

-0.0

1D

DH

_LA

T_08

2068

0B

LAN

CO

2007

-0.0

1D

DH

_LA

T_08

280

282

2068

120

07-0

.01

DD

H_L

AT_

0828

228

420

682

2007

-0.0

1D

DH

_LA

T_08

284

286

2068

320

07-0

.01

DD

H_L

AT_

0828

628

820

684

2007

-0.0

1

Pag

e 4

of 5

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_08

288

290

2068

520

07-0

.01

DD

H_L

AT_

0829

029

220

686

2007

-0.0

1-0

.01

DD

H_L

AT_

0829

229

420

687

2007

-0.0

1D

DH

_LA

T_08

294

296

2068

820

07-0

.01

DD

H_L

AT_

0829

629

820

689

2007

-0.0

1D

DH

_LA

T_08

2069

0S

TD-C

DN

-GS

-P5B

2007

0.47

DD

H_L

AT_

0829

830

020

691

2007

-0.0

1D

DH

_LA

T_08

300

302

2069

220

07-0

.01

DD

H_L

AT_

0830

230

420

693

2007

-0.0

1D

DH

_LA

T_08

304

306

2069

420

07-0

.01

DD

H_L

AT_

0830

630

820

695

2007

-0.0

1D

DH

_LA

T_08

308

310.

220

696

2007

-0.0

1

Pag

e 5

of 5

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_09

96.5

898

2069

720

070.

06D

DH

_LA

T_09

9899

.78

2069

820

070.

020.

02D

DH

_LA

T_09

99.7

810

120

699

2007

-0.0

1D

DH

_LA

T_09

101

102.

320

700

2007

0.01

DD

H_L

AT_

0910

2.3

103

2070

120

07-0

.01

DD

H_L

AT_

0910

310

420

702

2007

-0.0

1D

DH

_LA

T_09

104

105

2070

320

07-0

.01

DD

H_L

AT_

0910

510

620

704

2007

-0.0

1D

DH

_LA

T_09

106

107

2070

520

07-0

.01

DD

H_L

AT_

0910

710

820

706

2007

-0.0

1D

DH

_LA

T_09

108

109

2070

720

07-0

.01

DD

H_L

AT_

0920

708

DU

PLI

CA

DO

2007

-0.0

1-0

.01

DD

H_L

AT_

0910

911

020

709

2007

-0.0

1D

DH

_LA

T_09

110

111

2071

020

07-0

.01

DD

H_L

AT_

0911

111

220

711

2007

-0.0

1D

DH

_LA

T_09

112

113

2071

220

070.

02D

DH

_LA

T_09

113

114

2071

320

070.

02D

DH

_LA

T_09

114

115

2071

420

07-0

.01

DD

H_L

AT_

0911

511

620

715

2007

-0.0

1D

DH

_LA

T_09

2071

6B

LAN

CO

2007

-0.0

1D

DH

_LA

T_09

116

117

2071

720

07-0

.01

-0.0

1D

DH

_LA

T_09

117

118

2071

820

07-0

.01

DD

H_L

AT_

0911

811

920

719

2007

-0.0

1D

DH

_LA

T_09

119

120

2072

020

07-0

.01

DD

H_L

AT_

0912

012

120

721

2007

-0.0

1D

DH

_LA

T_09

121

122

2072

220

07-0

.01

DD

H_L

AT_

0912

212

320

723

2007

-0.0

1D

DH

_LA

T_09

122

123

2072

420

071.

43D

DH

_LA

T_09

123

124

2072

520

07-0

.01

DD

H_L

AT_

0912

412

520

726

2007

-0.0

1D

DH

_LA

T_09

125

126.

4720

727

2007

-0.0

1-0

.01

DD

H_L

AT_

0912

6.47

127.

4820

728

2007

0.04

DD

H_L

AT_

0912

7.48

128.

3720

729

2007

-0.0

1D

DH

_LA

T_09

128.

3712

920

730

2007

-0.0

1

Pag

e 1

of 1

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_10

2425

2073

120

07-0

.01

DD

H_L

AT_

1025

2620

732

2007

0.01

DD

H_L

AT_

1026

2820

733

2007

-0.0

1D

DH

_LA

T_10

2829

2073

420

07-0

.01

DD

H_L

AT_

1029

3020

735

2007

-0.0

1D

DH

_LA

T_10

3031

2073

620

07-0

.01

-0.0

1D

DH

_LA

T_10

3132

2073

720

07-0

.01

DD

H_L

AT_

1032

3320

738

2007

-0.0

1D

DH

_LA

T_10

3334

2073

920

07-0

.01

DD

H_L

AT_

1034

3520

740

2007

-0.0

1D

DH

_LA

T_10

3536

2074

120

07-0

.01

DD

H_L

AT_

1020

742

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_10

3637

2074

320

07-0

.01

DD

H_L

AT_

1037

3820

744

2007

-0.0

1D

DH

_LA

T_10

3839

2074

520

07-0

.01

DD

H_L

AT_

1039

4020

746

2007

-0.0

1D

DH

_LA

T_10

4041

2074

720

07-0

.01

DD

H_L

AT_

1041

4220

748

2007

-0.0

1D

DH

_LA

T_10

4243

2074

920

07-0

.01

DD

H_L

AT_

1020

750

BLA

NC

O20

07-0

.01

DD

H_L

AT_

1043

4420

751

2007

-0.0

1-0

.01

DD

H_L

AT_

1044

4520

752

2007

0.03

DD

H_L

AT_

1045

4620

753

2007

0.04

DD

H_L

AT_

1047

.448

.320

754

2007

0.03

DD

H_L

AT_

1048

.349

.17

2075

520

07-0

.01

Pag

e 1

of 1

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_11

68.4

369

.42

2075

620

07-0

.01

DD

H_L

AT_

1120

757

STD

- C

DN

-GS

-2B

2007

2.3

2.17

DD

H_L

AT_

1169

.42

70.3

320

758

2007

-0.0

1D

DH

_LA

T_11

70.3

371

.620

759

2007

-0.0

1D

DH

_LA

T_11

71.6

7320

760

2007

0.09

DD

H_L

AT_

1173

7420

761

2007

0.02

DD

H_L

AT_

1174

7520

762

2007

0.05

DD

H_L

AT_

1175

7620

763

2007

0.04

DD

H_L

AT_

1176

7720

764

2007

0.03

DD

H_L

AT_

1177

78.4

2076

520

070.

02D

DH

_LA

T_11

78.4

79.3

2076

620

070.

020.

02D

DH

_LA

T_11

79.3

8020

767

2007

0.04

DD

H_L

AT_

1180

81.2

2076

820

070.

03D

DH

_LA

T_11

81.2

81.9

2076

920

070.

06D

DH

_LA

T_11

81.9

82.4

320

770

2007

0.05

DD

H_L

AT_

1182

.43

82.9

2077

120

07-0

.01

DD

H_L

AT_

1182

.983

.54

2077

220

07-0

.01

DD

H_L

AT_

1183

.54

8420

773

2007

-0.0

1D

DH

_LA

T_11

8485

2077

420

07-0

.01

DD

H_L

AT_

1120

775

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_11

8586

2077

620

07-0

.01

DD

H_L

AT_

1186

86.7

2077

720

07-0

.01

DD

H_L

AT_

1186

.787

.15

2077

820

07-0

.01

DD

H_L

AT_

1187

.15

87.6

520

779

2007

0.05

DD

H_L

AT_

1120

780

BLA

NC

O20

07-0

.01

DD

H_L

AT_

1187

.65

88.2

2078

120

070.

07D

DH

_LA

T_11

88.2

88.7

2078

220

070.

28D

DH

_LA

T_11

88.7

89.2

2078

320

070.

22D

DH

_LA

T_11

89.2

89.7

2078

420

079.

55D

DH

_LA

T_11

89.7

90.2

2078

520

0711

.87

DD

H_L

AT_

1190

.291

2078

620

070.

03D

DH

_LA

T_11

9191

.84

2078

720

070.

07D

DH

_LA

T_11

2078

8S

TD20

07D

DH

_LA

T_11

91.8

492

.320

789

2007

4.57

DD

H_L

AT_

1192

.392

.820

790

2007

3.08

DD

H_L

AT_

1192

.893

.820

791

2007

-0.0

1-0

.01

DD

H_L

AT_

1193

.895

2079

220

07-0

.01

DD

H_L

AT_

1195

9620

793

2007

0.01

DD

H_L

AT_

1196

9720

794

2007

-0.0

1

Pag

e 1

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_11

9798

2079

520

070.

01D

DH

_LA

T_11

9899

2079

620

07-0

.01

DD

H_L

AT_

1199

100

2079

720

070.

56D

DH

_LA

T_11

100

100.

520

798

2007

0.28

DD

H_L

AT_

1110

0.5

101

2079

920

0713

8.39

DD

H_L

AT_

1110

110

1.3

2080

020

0728

.49

DD

H_L

AT_

1110

1.3

101.

820

801

2007

24.4

8D

DH

_LA

T_11

101.

810

2.3

2080

220

076.

72D

DH

_LA

T_11

102.

310

3.5

2080

320

072.

38D

DH

_LA

T_11

103.

510

420

804

2007

15.4

1D

DH

_LA

T_11

2080

5D

UP

LIC

AD

O20

0742

.85

44.1

3D

DH

_LA

T_11

104

104.

520

806

2007

105.

51D

DH

_LA

T_11

104.

510

520

807

2007

3.93

DD

H_L

AT_

1110

510

5.5

2080

820

070.

24D

DH

_LA

T_11

105.

510

6.75

2080

920

07-0

.01

DD

H_L

AT_

1110

6.75

107.

720

810

2007

-0.0

1D

DH

_LA

T_11

107.

710

8.7

2081

120

07-0

.01

DD

H_L

AT_

1110

8.7

110.

220

812

2007

-0.0

1D

DH

_LA

T_11

2081

3B

LAN

CO

2007

-0.0

1D

DH

_LA

T_11

110.

211

0.54

2081

420

070.

01D

DH

_LA

T_11

110.

5411

1.35

2081

520

07-0

.01

DD

H_L

AT_

1111

1.35

112.

2720

816

2007

-0.0

1-0

.01

DD

H_L

AT_

1111

2.27

112.

9420

817

2007

-0.0

1D

DH

_LA

T_11

112.

9411

420

818

2007

-0.0

1

Pag

e 2

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_12

5455

2081

920

070.

06D

DH

_LA

T_12

2082

0S

TD-C

DN

-GS

-P5B

2007

0.4

DD

H_L

AT_

1255

5620

821

2007

0.08

0.11

DD

H_L

AT_

1256

5720

822

2007

0.02

DD

H_L

AT_

1257

5820

823

2007

0.01

DD

H_L

AT_

1258

5920

824

2007

0.01

DD

H_L

AT_

1259

6020

825

2007

0.02

DD

H_L

AT_

1260

6120

826

2007

DD

H_L

AT_

1261

6220

827

2007

-0.0

1D

DH

_LA

T_12

6262

.520

828

2007

-0.0

1D

DH

_LA

T_12

62.5

63.1

2082

920

070.

05D

DH

_LA

T_12

63.1

63.9

2083

020

070.

74D

DH

_LA

T_12

63.9

64.6

2083

120

070.

01D

DH

_LA

T_12

64.6

65.1

2083

220

070.

01D

DH

_LA

T_12

65.1

65.6

420

833

2007

-0.0

1D

DH

_LA

T_12

65.6

465

.820

834

2007

-0.0

1D

DH

_LA

T_12

65.8

66.3

2083

520

07-0

.01

DD

H_L

AT_

1266

.366

.820

836

2007

-0.0

1D

DH

_LA

T_12

66.8

67.3

2083

720

070.

040.

03D

DH

_LA

T_12

67.3

67.8

2083

820

070.

02D

DH

_LA

T_12

67.8

68.3

2083

920

070.

02D

DH

_LA

T_12

68.3

68.8

2084

020

070.

07D

DH

_LA

T_12

68.8

69.2

2084

120

070.

1D

DH

_LA

T_12

69.2

69.5

2084

220

07-0

.01

DD

H_L

AT_

1269

.569

.820

843

2007

-0.0

1D

DH

_LA

T_12

69.8

70.3

2084

420

07-0

.01

DD

H_L

AT_

1270

.370

.820

845

2007

-0.0

1D

DH

_LA

T_12

70.8

71.4

520

846

2007

-0.0

1-0

.01

DD

H_L

AT_

1271

.45

72.2

2084

720

07-0

.01

DD

H_L

AT_

1272

.273

.220

848

2007

-0.0

1D

DH

_LA

T_12

73.2

74.2

2084

920

07-0

.01

DD

H_L

AT_

1220

850

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_12

74.2

7520

851

2007

-0.0

1D

DH

_LA

T_12

7576

2085

220

07-0

.01

DD

H_L

AT_

1276

7720

853

2007

-0.0

1D

DH

_LA

T_12

2085

4B

LAN

CO

2007

-0.0

1D

DH

_LA

T_12

7778

2085

520

07-0

.01

DD

H_L

AT_

1278

7920

856

2007

-0.0

1-0

.01

DD

H_L

AT_

1279

79.9

520

857

2007

-0.0

1D

DH

_LA

T_12

79.9

580

.620

858

2007

-0.0

1

Pag

e 1

of 2

Hol

e N

umbe

rFr

om (m

)To

(m)

Sam

ple

No.

Sam

ple

Type

Dat

eA

u (p

pm)

Au

(ppm

) Dup

licat

eD

DH

_LA

T_12

80.6

81.6

2085

920

07-0

.01

DD

H_L

AT_

1220

860

STD

-CD

N-G

S-2

B20

07D

DH

_LA

T_12

81.6

82.4

2086

120

07-0

.01

DD

H_L

AT_

1282

.483

.420

862

2007

-0.0

1D

DH

_LA

T_12

83.4

84.7

620

863

2007

-0.0

1D

DH

_LA

T_12

84.7

685

.920

864

2007

-0.0

1D

DH

_LA

T_12

85.9

86.9

520

865

2007

DD

H_L

AT_

1286

.95

87.4

2086

620

070.

07D

DH

_LA

T_12

87.4

87.9

2086

720

070.

01D

DH

_LA

T_12

87.9

88.3

2086

820

07-0

.01

-0.0

1D

DH

_LA

T_12

88.3

88.9

320

869

2007

-0.0

1D

DH

_LA

T_12

88.9

389

.420

870

2007

-0.0

1D

DH

_LA

T_12

89.4

89.9

2087

120

07-0

.01

DD

H_L

AT_

1289

.990

.320

872

2007

-0.0

1D

DH

_LA

T_12

90.3

90.8

520

873

2007

0.07

DD

H_L

AT_

1290

.85

91.3

520

874

2007

0.19

DD

H_L

AT_

1291

.35

91.8

520

875

2007

0.05

DD

H_L

AT_

1291

.85

92.3

520

876

2007

-0.0

1D

DH

_LA

T_12

92.3

593

.35

2087

720

07-0

.01

DD

H_L

AT_

1220

878

DU

PLI

CA

DO

2007

-0.0

1D

DH

_LA

T_12

93.3

594

.35

2087

920

07-0

.01

DD

H_L

AT_

1294

.35

95.7

2088

020

070.

060.

06D

DH

_LA

T_12

95.7

9620

881

2007

0.11

DD

H_L

AT_

1296

9720

882

2007

0.04

DD

H_L

AT_

1297

9820

883

2007

0.11

DD

H_L

AT_

1298

9920

884

2007

0.02

DD

H_L

AT_

1220

885

BLA

NC

O20

07-0

.01

DD

H_L

AT_

1299

100

2088

620

070.

03

Pag

e 2

of 2

2-1

APPENDIX 2 EXAMPLES OF DRILL LOGS

Azimuth:N:

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E:

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Au

visi

ble

Mineralización

POZO: Geólogo:

Inclinación:Prof. total:

Proyecto: PASO YOBAI Area: Inicio: Fnalización:

Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta

Sulfuros Oxidos Ganga

Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 1/12

Area:S- Suelo

BS- BasaltoAR- Arenisca

LT- Lutita

Dis - Diseminados F - Fallas

Frac - Fracturas

1 - Bajo Grado2 - Moderado Grado3 - Alto Grado

Litología Distribución Estructura Projecto: PASO YOBAI

OQ - Oquedades

Vet - VetilleosBR- Vet- Brecha- Stock

Alteración y MineralizaciónPIMA

EsmectitaNontrolitaMontmolleronita

Kaolin

0

1

2

3

4

5

6

7

8

9

10

11

12

0

1

2

3

4

5

6

7

8

9

10

11

12

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

440

1819

83

110

236

210

61

76

10

15

59

63

82

103

28

28

34

59

15

17

12

7

19

17

-5

-5

-5

-5

6

9

S: Suelofrancoarcilloso decolor marronclaro

AR: Areniscafriableblanca-rosadacon alt decaolín y algode óxidos

AR: Areniscafina rosadacon alto contde OxMn yalteracion decaolín

AR: Areniscarosada conalteracion dearcillas yOxMn

20001

20002

20003

20004

20005

20006

0.03

0.03

0.01

-0.01

0.01

0.03

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

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Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 2/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

12

13

14

15

16

17

18

19

20

21

22

23

24

12

13

14

15

16

17

18

19

20

21

22

23

24

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

103

170

134

764

1551

30

31

37

256

311

32

40

32

193

115

6

11

7

111

287

8

-5

-5

-5

-5

BS: Basaltoconalteracion decaolin

AR: Areniscarosada conalgo dealteracion dearcillas yOxMn-OxFediseminados

AR: Areniscarosada conalteracion decaolin

20007

20008

20009

20010

20011

20012:DUPLICADO

20013 -0.01

-0.01

-0.01

0.08

0.39

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 3/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

24

25

26

27

28

29

30

31

32

33

34

35

24

25

26

27

28

29

30

31

32

33

34

35

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

119

54

94

104

86

125

38

18

34

40

20

19

34

22

31

41

36

32

12

5

12

6

5

13

13

-5

7

18

5

-5

20014

20015

20016

20017

20018

20019

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 4/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

36

37

38

39

40

41

42

43

44

45

46

47

36

37

38

39

40

41

42

43

44

45

46

47

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

85

91

78

116

112

80

38

26

56

92

35

41

35

29

30

30

28

31

5

6

10

8

13

5

6

-5

-5

7

7

12

AR: Areniscarosada conoquedadesrellenas porcaolín

20020

20021

20022

20023

20024

20025:BLANCO

20026 -0.01

-0.01

-0.01

-0.01

0.02

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 5/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

48

49

50

51

52

53

54

55

56

57

58

59

48

49

50

51

52

53

54

55

56

57

58

59

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

268

99

62

84

78

89

22

19

18

26

24

31

27

29

26

30

23

32

7

13

4

11

4

12

6

6

-5

-5

-5

-5

AR: Areniscarosada conalt de caolinyOxMn+OxFeen vetillas y

20027

20028

20029

20030

20031:STDCDN-GS-2B

20032

20033

-0.01

-0.01

0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 6/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

60

61

62

63

64

65

66

67

68

69

70

71

60

61

62

63

64

65

66

67

68

69

70

71

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

453

384

168

259

127

571

53

32

29

53

64

29

76

44

52

92

26

39

6

9

6

16

7

12

6

6

9

9

6

5

diseminados

BR: Areniscabrechadacon clastosalterados acaolin conmx de harinade roca,OxFe y OxMndiseminados

AR: Areniscarosa con altde caolin yOxMn+OXFeen vetillas

AR: Areniscalixiviadacaolinizadacon OxMn

AR: Areniscarosada conalteracion decaolinparcialmentesilicificada yOxMndiseminadosy en vetillas

20034

20035

20036

20037

20038

20039

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 7/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

72

73

74

75

76

77

78

79

80

81

82

83

72

73

74

75

76

77

78

79

80

81

82

83

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

173

133

145

133

298

296

95

65

31

35

38

60

38

42

35

48

122

466

6

7

11

8

7

8

17

9

10

9

6

6

AR: Arenisca

20040

20041

20042

20043

20044

20045

0.07

0.16

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 8/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

84

85

86

87

88

89

90

91

92

93

94

95

84

85

86

87

88

89

90

91

92

93

94

95

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

940

850

1213

1457

966

656

386

584

580

407

319

172

1078

1305

1160

958

837

148

265

294

275

219

206

74

72

63

9

7

-5

7

parcialmentesilicificada ycaolinizadacon OxMn yOxFe envetillas

AR: Areniscasilicificada ycaolinizadacon OxMn yOxFediseminadasy en vetillas

BS: Basaltocon alt deesmectita-caoliny presenciade OxMn-OxFe ylimonitas

BS: Basaltocon alt deesmectita ycarbonaticacon vetillasde OxMn ycalcita

BR: Basaltoconstockwork decalcita yvenilleo desilice, alt deesmectita yvetilleo deOxFe- Mncon calcita yPydiseminada

BR: Basaltoconstockwork decalcita yvenilleo desilice con Auvisible, alt deesmectita yvetilleo deOxMn-calcita+ silice-

20046

20047

20048

20049

20050

20051:DUPLICADO

20052 0.05

5.96

0.01

0.09

-0.01

0.05

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 9/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

96

97

98

99

100

101

102

103

104

105

106

107

96

97

98

99

10

10

10

10

10

10

10

10

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

687

827

1512

1187

1270

866

368

369

432

486

435

443

1018

968

1035

1044

976

1178

243

236

215

243

253

259

7

5

40

25

13

69

sulfurosnegros y Pydiseminados

BR: Basaltoconstockwork decalcita-OxMny alt deesmectita

BS: Basaltoconstockwork decalcita-OxMny alt deesmectita

BS: Basaltocon caolin-esmectita yalgo deOxFe-OxMn

BR: Basaltoconstockwork decalcita-OxMny alt deesmectita-carbonato

BS: Basaltoconstockwork deOxMn y algode Py,alteracion deesmectita

20053

20054

20055

20056

20057

20058

-0.01

-0.01

-0.01

0.41

0.02

0.51

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

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a

Alteración

Cao

línC

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nato

Piri

ta

Silic

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alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 10/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

108

109

110

111

112

113

114

115

116

117

118

119

10

10

11

11

11

11

11

11

11

11

11

11

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

261

265

139

238

354

965

45

62

65

62

74

322

323

405

431

383

381

895

11

13

4

12

13

205

-5

-5

-5

-5

6

13BS: Basaltocon vetilleode OxMn+calcita

AR: Areniscarosada constockwork deOxFe+calcita

AR: Areniscablanquecinacon algo dearcillas

20059

20060

20061

20062

20063

20064

0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

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Esm

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Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 11/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

120

121

122

123

124

125

126

127

128

129

130

131

12

12

12

12

12

12

12

12

12

12

13

13

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

299

203

334

262

193

560

54

41

59

36

56

177

400

380

462

357

425

572

6

4

6

14

6

65

-5

-5

-5

-5

-5

6

20065:BLANCO

20066:STDCDN-GS-1P5B

20067

20068

20069

20070

20071

20072

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

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alci

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Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 12/12

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

132

133

134

135

136

137

13

13

13

13

13

13

Ana Pantano

Minas Guaira

DDH-LAT1

137.9 mts

..../..../.... ..../..../....

215º-50º

5993027148307263.41

DDH-LAT1

Minas Guaira

353

719

159

29

30

30

215

334

299

8

17

9

-5

-5

-5

20073

20074

20075

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

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Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

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nato

Piri

ta

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ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 1/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

0

1

2

3

4

5

6

7

8

9

10

11

12

0

1

2

3

4

5

6

7

8

9

10

11

12

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

1137

473

331

139

182

96

100

89

40

19

63

56

64

98

33

30

38

44

16

12

18

12

18

13

-5

-5

-5

-5

8

6

AR:Areniscas decolor marron

LT: Lutitamicacea

AR: Areniscade colormarron claro

LT: Lutitamicacea decolor morado

20076

20077

20078

20079

20080

20081

0.16

0.08

0.02

-0.01

0.01

0.02

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

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nato

Piri

ta

Silic

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alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 2/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

12

13

14

15

16

17

18

19

20

21

22

23

24

12

13

14

15

16

17

18

19

20

21

22

23

24

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

151

1928

999

605

538

1116

1315

27

579

585

517

88

424

498

29

317

916

1026

65

351

122

7

137

232

164

35

199

277

5

53

7

6

13

11

-5

BS: Basaltode color gris



AR: Areniscade colormarron

AR:areniscas decolor marron

20082

20083

20084

20085

20086

20087

20088

20089:Duplicado

-0.01

0.09

0.03

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

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nato

Piri

ta

Silic

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alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 3/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

24

25

26

27

28

29

30

31

32

33

34

35

24

25

26

27

28

29

30

31

32

33

34

35

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

177

144

178

126

111

154

62

68

172

46

35

41

30

31

124

25

35

30

11

11

14

6

10

18

8

18

12

12

10

13

LT: Lutitas decolor gris


20090

20091

20092:Blanco

20093

20094

20095:STDCDN-GS-2B

20096

20097

20098

-0.01

-0.01

0.04

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 4/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

36

37

38

39

40

41

42

43

44

45

46

47

36

37

38

39

40

41

42

43

44

45

46

47

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

283

102

108

36

80

169

18

20

24

12

24

60

25

22

28

18

20

25

7

5

5

3

10

6

-5

-5

-5

-5

-5

7

20099

20100

20101

20102

20103

20104

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 5/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

48

49

50

51

52

53

54

55

56

57

58

59

48

49

50

51

52

53

54

55

56

57

58

59

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

346

264

463

314

251

163

53

74

24

17

16

14

35

45

27

26

25

24

7

10

9

6

5

4

-5

-5

-5

-5

5

-5

20105

20106

20107

20108

20109

20110

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 6/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

60

61

62

63

64

65

66

67

68

69

70

71

60

61

62

63

64

65

66

67

68

69

70

71

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

248

175

226

207

235

352

63

66

63

56

59

55

82

327

414

284

43

51

8

4

6

7

8

9

-5

-5

-5

-5

5

8

20111

21112

20113

20114

20115:Duplicado

20116

20117

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 7/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

72

73

74

75

76

77

78

79

80

81

82

83

72

73

74

75

76

77

78

79

80

81

82

83

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

87

95

184

780

179

211

43

43

64

40

36

62

348

313

359

334

262

35

5

4

6

17

4

5

-5

-5

-5

7

-5

-5

20118

20119

20120

20121

20122:Blanco

20123

20124

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 8/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

84

85

86

87

88

89

90

91

92

93

94

95

84

85

86

87

88

89

90

91

92

93

94

95

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

568

171

155

243

181

133

66

75

80

99

74

45

328

574

548

472

377

351

10

7

5

5

6

4

-5

-5

-5

-5

-5

-5



20125

20126

20127

20128

20129:STDCDN-GS-1P5B

20130

20131

-0.01

-0.01

-0.01

0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 9/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

96

97

98

99

100

101

102

103

104

105

106

107

96

97

98

99

10

10

10

10

10

10

10

10

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

287

149

99

180

167

610

314

142

190

56

51

35

48

68

75

52

64

68

534

524

345

484

643

440

455

458

439

7

5

5

4

5

5

6

4

5

-5

-5

-5

-5

-5

-5

-5

-5

-5

AR: Areniscade colorrosa claro

20132

20133

20134

20135

20136

20137

20138

20139-0.01

-0.01

-0.01

-0.01

-0.01

0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

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Mineralización

POZO: Geólogo:



Prof

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)

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Roc

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aTipo de Roca

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sDescripción

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alci

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Foto

s de

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s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

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mec

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Pim

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Ox

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Silí

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Mn_

ppm

POZO:

Page: 10/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

108

109

110

111

112

113

114

115

116

117

118

119

10

10

11

11

11

11

11

11

11

11

11

11

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

868

984

1084

982

917

1227

1413

841

1143

1166

589

376

353

374

372

372

405

421

363

374

498

60

1116

1083

1076

1058

1079

1020

1122

1052

1058

1279

360

247

242

243

235

237

235

253

235

244

126

13

-5

-5

-5

-5

-5

-5

7

-5

-5

19

6

AR: Arenisca


BR:Stockwork


20140

20141

20142

20143

20144

20145

20146

20147:STDCDN-GS-P5B

20148

20149

20150

20151-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

0.04

0.04

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

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Au

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Mineralización

POZO: Geólogo:



Prof

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)

Tipo

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Roc

a

MC

aTipo de Roca

Dis

tribu

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S. N

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sDescripción

Litología

Estru

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a

Esm

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Alteración

Cao

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arbo

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Piri

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Silic

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ta


Foto

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s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

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Pim

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Pim

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aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 11/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

120

121

122

123

124

125

126

127

128

129

130

131

12

12

12

12

12

12

12

12

12

12

13

13

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

792

786

761

846

1000

843

939

1858

1232

1754

1472

1205

362

380

374

358

386

390

385

471

543

414

404

403

1114

1104

1134

1115

1128

1079

1014

1033

1114

1059

1109

1048

245

250

245

248

256

234

226

247

225

237

244

235

-5

-5

-5

-5

-5

-5

-5

43

18

-5

-5

-5

BR:Stockwork


20152

20153

20154

20155

20156:Blanco

20157

20158

20159

20160

20161

20162

20163

20164-0 01

-0.01

-0.01

-0.01

-0.01

0.09

-0.01

0.04

-0.01

-0.01

-0.01

-0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

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sDescripción

Litología

Estru

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a

Esm

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a

Alteración

Cao

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arbo

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Piri

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alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

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Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 12/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

132

133

134

135

136

137

138

139

140

141

142

143

13

13

13

13

13

13

13

13

14

14

14

14

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

278

217

263

910

934

1068

1512

1242

792

73

64

71

416

405

420

462

387

362

444

519

487

965

1070

1092

1157

1083

1114

8

3

6

175

246

236

209

241

245

-5

-5

-5

-5

-5

-5

-5

-5

5

BS: Basalto

AR: Areniscade colorrosa

20165:Duplicado

20166

20167

20168

20169

20170

20171

20172

20173

20174

-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

0.04

-0.01

0.01

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

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Pim

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ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 13/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

144

145

146

147

148

149

150

151

152

153

154

155

14

14

14

14

14

14

15

15

15

15

15

15

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

191

213

454

376

145

311

49

54

157

45

37

45

352

256

498

350

212

349

4

7

33

9

8

9

-5

-5

-5

-5

-5

5

LT: Lutitas

AR:Areniscas decolor rosa

20175

20176

20177

20178:Blanco

20179

20180

20181

-0.01

-0.01

-0.01

-0.01

-0.01

0.02

Azimuth:N:

Z Collar:

E:

UTM 21S

Cal

copi

rita

Au

visi

ble

Mineralización

POZO: Geólogo:



Prof

. (m

)

Tipo

de

Roc

a

MC

aTipo de Roca

Dis

tribu

ción

S. N

egro

sDescripción

Litología

Estru

ctur

a

Esm

ectit

a

Alteración

Cao

línC

arbo

nato

Piri

ta

Silic

eC

alci

ta


Foto

s de

caja

s

Ox

Mn

Au_

ppm

As_

ppm

Cu_

ppm

P_pp

m

V_pp

m

Prof

. (m

)

Mue

stra

PIMA

Obs

erva

ción

Pim

a-Es

mec

tita

Pim

a-N

ontro

lita

Pim

a-M

ontm

Pim

a-K

aolin

Ox

Fe

Silí

cea

Mn_

ppm

POZO:

Page: 14/14

Area:S- Suelo


LT- Lutita


Frac - Fracturas



OQ - Oquedades




Kaolin

156

157

158

159

160

161

162

163

164

165

15

15

15

15

16

16

16

16

16

16

Miguel Molinas

Minas Guaira

DDH_LAT_02

165,30

11/11/07 13/11/07

23065

5992927148314263.53

DDH_LAT_02

Minas Guaira

203

137

137

96

194

212

39

43

28

32

46

44

426

281

270

293

298

320

4

3

4

6

6

8

-5

-5

-5

-5

-5

7

20182

20183

20184

20185

20186-0.01

-0.01

-0.01

-0.01

-0.01

-0.01

Paso Yo Bai 43101

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Transcript of Paso Yo Bai 43101