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Suez University
Faculty of Petroleum & Mining Engineering
Minerals and Rocks
Student
Belal Farouk El-saied Ibrahim
Class / III
Section / Engineering Geology and Geophysics
The Reference / Basic Pet. Geology
( P.K.Link)
Presented to Prof. Dr. / Shouhdi E. Shalaby
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Main TopicsMain Topics
Minerals.Minerals. Rocks.Rocks.
IgneousIgneous
SedimentarySedimentary
MetamorphicMetamorphic Rock cycle.Rock cycle.
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What are minerals?What are minerals?
All rocks are composed All rocks are composed of mineralsof minerals
Minerals are naturally Minerals are naturally occurring, inorganic, occurring, inorganic, crystalline solid with a crystalline solid with a definite chemical definite chemical composition found on composition found on Earth.Earth.
There are about 3500 There are about 3500 known mineralsknown minerals
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About 20 minerals make up more than About 20 minerals make up more than 95% of all of the 95% of all of the rocksrocks in the Earth in the Earth’’s s
crustcrust
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Composition of the Earth’s Composition of the Earth’s CrustCrust
Eight Elements that make up over 98% Eight Elements that make up over 98% of Earth’s Crustof Earth’s Crust-Oxygen (O)-Oxygen (O)-Silicon (SI)-Silicon (SI)-Aluminum (Al)-Aluminum (Al)-Iron (Fe)-Iron (Fe)-Calcium (Ca)-Calcium (Ca)-Sodium (Na)-Sodium (Na)-Potassium (K)-Potassium (K)-Magnesium (Mg)-Magnesium (Mg)
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MINERAL PROPERTIESPhysical properties of minerals are dictated by the nature of the underlying atomic structure, nature and arrangement of chemical bonds, and energy levels of valence electrons. ColorColor LusterLuster HardnessHardness StreakStreak DensityDensity Crystal ShapeCrystal Shape Cleavage and FractureCleavage and Fracture Special PropertiesSpecial Properties
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ColorColor Usually the first and most easily Usually the first and most easily
observedobserved
-Some minerals are always the same -Some minerals are always the same colorcolor
-Some minerals can have many -Some minerals can have many colorscolors
QUARTZROSE QUARTZ SMOKY QUARTZ
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LusterLuster
General General appearance of a appearance of a mineral surface mineral surface in reflected lightin reflected light
Glassy-Obsidian
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Hardness: MOH’S Hardness Scale (NOT absolute):
Talc 1Gypsum 2Calcite 3Fluorite 4Apatite 5Orthoclase 6Quartz 7Topaz 8Corundum 9Diamond 10
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External Crystal Form:a solid plane in which the atoms are arranged in orderly, repeating patterns
A. cubic B. tetragonal C. hexagonal D. orthorhombic E. triclinic F. monoclini (some minerals do not show well-developed crystals).
Fluorite
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CUBICHALITE
TETRAGONALWULFENITE
HEXAGONALBERYL
ORTHORHOMBICTANZANITE
MONOCLINICGYPSUM
TRICLINICMONTEBRASITE
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Crystal Form
Quartz
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Fig. 02.15bFig. 02.15bCrystal Form
Feldspar
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CLEAVAGE: splitting along preferred directions due to weak bonds within the atomic structure. Cleavage is described as perfect, good, poor.
This is a property of crystals – be careful that you are looking at crystals and not crystal aggregates.
Cleavages can be confused with crystal faces – can often see cleavage planes perpendicular to crystal faces.
Some crystals do not show cleavage due to similar bond strengths throughout the crystal structure. However, a crystal can have 1, 2, 3… directions of cleavage. It is important to note: (i) the number of cleavage directions, and (ii) their angular relationship:
1 direction; 2 directions at 90˚; 2 directions, inclined; 3 directions, cubic; 3 directions, rhombohedral; 4 directions, octahedral; 6 directions dodecahedral.
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Planer Cleavage in MicaPlaner Cleavage in Mica
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Weak Bonding Yields Planer Weak Bonding Yields Planer CleavageCleavage
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Amphibole Cleavage ~120/60°Amphibole Cleavage ~120/60°
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Rhombohedral Cleavage in Rhombohedral Cleavage in CalciteCalcite
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Fracture: the way a substance breaks where not controlled by cleavage. Described as: conchoidal, irregular, splintery, blocky, hackly.
Specific Gravity: unitless property, defined by
Ice: 0.9Quartz: 2.65Most silicates: 2.5-3.0Galena 7.5Gold 19.3
mass_ of _ substan ce
mass_ of _ equal_ vol._ of _H 2O
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Conchoidal Fracture in GlassConchoidal Fracture in Glass
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Special and Other PropertiesSpecial and Other Properties
StriationsStriations - Commonly found on plagioclase - Commonly found on plagioclase feldspar. Straight, parallel lines on one or more feldspar. Straight, parallel lines on one or more of the cleavage planes caused by mineral of the cleavage planes caused by mineral twinning.twinning.
MagnetismMagnetism - Property of a substance such that - Property of a substance such that it will spontaneous orient itself within a magnetic it will spontaneous orient itself within a magnetic field. Magnetite (Fefield. Magnetite (Fe33OO44) has this property and it ) has this property and it can be used to distinguish it from other non-can be used to distinguish it from other non-magnetite iron oxides, such as hematite (Femagnetite iron oxides, such as hematite (Fe22OO33).).
Double RefractionDouble Refraction - Seen in calcite crystals. - Seen in calcite crystals. Light is split or refracted into two components Light is split or refracted into two components giving rise to two distinct images.giving rise to two distinct images.
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PlagioclasPlagioclase e
striationsstriations
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Calcite Double Calcite Double RefractionRefraction
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Special PropertiesSpecial Properties
Magnetism (Magnetite)Magnetism (Magnetite) Glowing under ultraviolet light Glowing under ultraviolet light
(Fluorite)(Fluorite) Salty taste (Halite)Salty taste (Halite) Smell (Sulfur)Smell (Sulfur) Reaction to HCl (Calcite)Reaction to HCl (Calcite)
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FluorescenceFluorescenceMagnetismMagnetismMagnetiteMagnetite
Double RefractionCalcite
Smell Sulfur
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RocksRocks
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RocksRocks
Made of two or more different Made of two or more different minerals that have been: minerals that have been: cemented togethercemented togethersqueezed and heated together squeezed and heated together melted and cooled together. melted and cooled together.
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Types of RocksTypes of Rocks
IgneousIgneous SedimentarySedimentary MetamorphicMetamorphic
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Igneous RocksIgneous Rocks
Magma- molten material undergroundMagma- molten material underground Lava- magma that reaches the surfaceLava- magma that reaches the surface
Igneous rocks are formed from magma Igneous rocks are formed from magma that has cooled and hardened either that has cooled and hardened either beneath the surface or from a volcanic beneath the surface or from a volcanic eruptioneruption
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2 Ways to Form Igneous 2 Ways to Form Igneous RockRock
Intrusive Intrusive Igneous RocksIgneous Rocks- - form when form when magma hardens magma hardens beneath Earth’s beneath Earth’s surfacesurface
Magma intrudes Magma intrudes into existing rocksinto existing rocks
Extrusive Extrusive Igneous Rocks- Igneous Rocks- form when lava form when lava hardens on the hardens on the surface of the surface of the EarthEarth
Extruded onto the Extruded onto the surfacesurface
granite
rhyolite
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Classification of Igneous Classification of Igneous RocksRocks
CompositionComposition-refers to the minerals -refers to the minerals that make up the rockthat make up the rock
TextureTexture-shape, size, arrangement -shape, size, arrangement and distribution of minerals that and distribution of minerals that make up the rockmake up the rock
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CompositionBowen’s Reaction
• N. L. Bowen studied mineral crystallization and found out that minerals form at specific times during that solidification process and they generally form in the same order.
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TexturesTextures
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TexturesTextures GlassyGlassy
Fine-grainedFine-grained
Coarse-grainedCoarse-grained
PorphyriticPorphyritic
Obsidian Granite
Granite
Basalt
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Sedimentary Sedimentary RocksRocks
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Sedimentary RocksSedimentary Rocks
Sediments = pieces of solid Sediments = pieces of solid material deposited on the material deposited on the Earth’s surface.Earth’s surface.
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Sedimentary RockSedimentary Rock Rocks that are composed of the Rocks that are composed of the
weathered remains of preexisting weathered remains of preexisting rock, or plant and animal remains.rock, or plant and animal remains.
Sedimentary rocks commonly Sedimentary rocks commonly originate from sediments laid originate from sediments laid down in horizontal strata by water down in horizontal strata by water or wind.or wind.
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Horizontal Beds of SedimentaryHorizontal Beds of Sedimentary RockRock
BedsBedding planes
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Sedimentary RocksSedimentary Rocks How is a sedimentary rock formed?How is a sedimentary rock formed?
Sediments get compacted and cemented Sediments get compacted and cemented together.together.
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Sedimentary RocksSedimentary Rocks Clastic – made from fragments of Clastic – made from fragments of
other rocks, that have been other rocks, that have been transported, deposited, then transported, deposited, then compacted and cemented together.compacted and cemented together.
Shale, sand, conglomerate, siltstone, Shale, sand, conglomerate, siltstone, brecciabreccia
Classified by the size of the fragments in Classified by the size of the fragments in the rocksthe rocks
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Cemented RocksCemented Rocks Clastic sedimentary rockClastic sedimentary rock – rocks – rocks
composed of weathered composed of weathered sediments:sediments: Pebbles or gravel – usually quartzPebbles or gravel – usually quartz Sand – usually quartzSand – usually quartz Clay and silt – weathered feldspars Clay and silt – weathered feldspars
and mica :and mica : held together by a natural cementheld together by a natural cement
or by compaction of clay and silt.or by compaction of clay and silt.
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Sedimentary rocks drop according Sedimentary rocks drop according to size; larger particles fall first to size; larger particles fall first followed by smaller particlesfollowed by smaller particles
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Clastics RocksClastics Rocks ConglomerateConglomerate
SandstoneSandstone
MudstoneMudstone
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ConglomerateConglomerate – – cemented sand, silt, and cemented sand, silt, and
pebble sediments. If pebble sediments. If large fragments are large fragments are
angular this rock is called angular this rock is called a breccia.a breccia.
SandstoneSandstone – – cemented cemented
quartz sand quartz sand grains. Feels grains. Feels
gritty. Unfilled gritty. Unfilled spaces between spaces between
grains make grains make most most
sandstones sandstones porous and porous and
permeable to permeable to water.water.
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ShaleShale – clay and silt sized particles – clay and silt sized particles lithified by dehydration and lithified by dehydration and
compaction. Note the cleavage at compaction. Note the cleavage at bedding planes. Thumps when you bedding planes. Thumps when you tap it with a nail and, moistened, it tap it with a nail and, moistened, it
smells like damp earth.smells like damp earth.
Bedding planes
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Sandstone in the Pinnacle Desert, Sandstone in the Pinnacle Desert, AustraliaAustralia
Photo used with permission from Mike Jarvis, Naperville Central HS, Naperville,
IL
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Chemical Sedimentary Chemical Sedimentary RocksRocks
Rocks formed either as Rocks formed either as precipitates or as evaporites of precipitates or as evaporites of dissolved chemical sediments.dissolved chemical sediments.
Rock salt, rock gypsum, some Rock salt, rock gypsum, some limestoneslimestones
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Rock saltRock salt, the , the mineral halite mineral halite
(NaCl), left as an (NaCl), left as an evaporite as a evaporite as a
shallow sea shallow sea evaporated.evaporated.
AlabasterAlabaster, the mineral , the mineral gypsum (CaSOgypsum (CaSO44), also ), also
an evaporite.an evaporite.
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Compact (or precipitate) limestoneCompact (or precipitate) limestone, the , the mineral calcite (CaCOmineral calcite (CaCO33), precipitated from ), precipitated from
sea water as evaporation increased sea water as evaporation increased concentration. Many cavern systems are concentration. Many cavern systems are
formed in this type of limestone.formed in this type of limestone.
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Sedimentary RocksSedimentary Rocks Organic Rocks – formed from the Organic Rocks – formed from the
remains of plants and animals.remains of plants and animals.
Shells of marine animals pile up, Shells of marine animals pile up, compact and cement to create compact and cement to create fossiliferous limestone (coquina).fossiliferous limestone (coquina).
Sedimentary rocks are the only Sedimentary rocks are the only rocks that contain fossilsrocks that contain fossils
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CoquinaCoquina – cemented – cemented aggregate of aggregate of
geologicallygeologically modern modern shell fragments.shell fragments.
Fossiliferous Fossiliferous limestonelimestone – a – a
cemented aggregate cemented aggregate of original shell of original shell
fragments, molds, fragments, molds, and casts of ancient and casts of ancient marine organisms. marine organisms.
Note fossil mold of a Note fossil mold of a shell in this shell in this
specimen.specimen.
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PeatPeat, a mass of , a mass of matted together matted together plant material plant material
covered by Hcovered by H22O, O, which impedes which impedes
decay. Hdecay. H22 and O and O22 are are lost, concentrating lost, concentrating
carbon.carbon.
LigniteLignite, so called , so called “brown coal”, a soft “brown coal”, a soft
coal that forms coal that forms when peat is when peat is
compressed and compressed and aged, about 40% aged, about 40%
carbon.carbon.
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Bituminous coalBituminous coal – soft coal formed when – soft coal formed when lignite is compacted and altered for lignite is compacted and altered for millions of years, about 85% carbon, millions of years, about 85% carbon,
this coal is the most commonly mined this coal is the most commonly mined and used for a fuel.and used for a fuel.
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Sedimentary Rock FeaturesSedimentary Rock Features
Features in sedimentary rock that Features in sedimentary rock that reflect the sedimentary environment.reflect the sedimentary environment.
Not found in other rock types.Not found in other rock types.
Features:Features: Stratification Stratification FossilsFossils Ripple marks & crossbedsRipple marks & crossbeds Mud cracksMud cracks Nodules, concretions & geodesNodules, concretions & geodes
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Rock Stratification (layering) Bryce Rock Stratification (layering) Bryce Canyon, UTCanyon, UT
Photo used with permission from Mike Jarvis, Naperville Central HS, Naperville,
IL
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Ripple marksRipple marks caused caused by wave action on by wave action on
the sandy bottom of the sandy bottom of a shallow baya shallow bay
Almost identical Almost identical ripple marks on ripple marks on the surface of a the surface of a
sandstone sandstone millions of years millions of years
old.old.
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Mud cracksMud cracks in in drying muddrying mud
Mud cracks Mud cracks preserved on preserved on the bedding the bedding surface of a surface of a
shale.shale.
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Groundwater dissolves hollow spaces in Groundwater dissolves hollow spaces in sedimentary rock, typically limestone, sedimentary rock, typically limestone,
and mineral material is deposited inside and mineral material is deposited inside the hollow with crystal points growing the hollow with crystal points growing
toward the center.toward the center.
Geode
Thunder Egg
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Cross-bedding at Checkerboard Mesa Cross-bedding at Checkerboard Mesa Zion National Park, UT Zion National Park, UT
Photo used with permission from Mike Jarvis, Naperville Central HS, Naperville,
IL
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Dinosaur skeleton preserved in Dinosaur skeleton preserved in sedimentary rock - Chinasedimentary rock - China
Photo used with permission from Mike Jarvis, Naperville Central HS, Naperville,
IL
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THE IMPORTANCE OF SEDIMENTARY ROCKSTHE IMPORTANCE OF SEDIMENTARY ROCKS
• petroleum geology relies on the capacity of sedimentary rocks to generate deposits of petroleum oils. Coal and oil shale are found in sedimentary rocks. A large proportion of the world's uranium energy resources are hosted within sedimentary successions.
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Metamorphic Rocks
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It is metamorphosedIt is metamorphosed
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Formation of Metamorphic Formation of Metamorphic Rock Rock
Changed from Changed from one typeone type of rock into of rock into anotheranother by heat, pressure, and by heat, pressure, and chemical processes. chemical processes.
Form Form deepdeep beneath the earth’s surface. beneath the earth’s surface.
ALLALL metamorphic rocks are formed metamorphic rocks are formed from from existingexisting igneous, sediment or igneous, sediment or metamorphic metamorphic rocksrocks..
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metamorphic rocks: controlling metamorphic rocks: controlling factorsfactors
• temperature and pressure during metamorphism
• tectonic forces
• fluids
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heat is essential
temperature during metamorphism
• heat from Earth’s deep interior
• all minerals stable over finite temperature range
• higher temperatures than range cause melting(and therefore generates igneous rocks)
think about mixing flour, yeast, water, salt….
….nothing happens until they have a heat source and then they make bread
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pressure in the Earth acts the same in all directions
pressure is proportionalto depth in the Earth
look at example with deep water
pressure increaseswith depth
volume decreaseswith depth
pressure during metamorphism
increases at ~1 kilobar per 3.3 km
high pressure minerals: more compact and dense
--grains pack together--
consequence on cube is squeezing into smaller cube
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tectonic forces - driven by plate motion!lead to forces that are not equal in all directions (differential stress)
compressive stress (hands squeeze together)causes flattening at 90° to stress
shearing (hands rubbing together) causes flattening parallel to stress
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flattened pebbles in metamorphic rock
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fluids• hot water (water vapor) most important
• heat causes unstable minerals to release water
• water reacts with surrounding rocks and transports dissolved material and ions
time• metamorphism may take millions of years
• longer times allow new minerals to grow larger--coarser grained rocks
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FormationFormation
Minerals may Minerals may change in sizechange in size or shape or shape or separate into parallel bands. or separate into parallel bands.
Metamorphic formation happens two Metamorphic formation happens two different waysdifferent ways
ContactContact metamorphism metamorphism RegionalRegional metamorphism metamorphism
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Contact MetamorphismContact Metamorphism
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Regional MetamorphismRegional Metamorphism
Regional metamorphism occurs where rocks are squeezed between two converging lithospheric
plates during mountain building.
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Classification of Metamorphic Classification of Metamorphic RocksRocks
Rocks can be Rocks can be classified into twoclassified into two different types based on their different types based on their texture:texture:
Foliated: which is when the rock grains Foliated: which is when the rock grains are arranged in parallel layers or bands.are arranged in parallel layers or bands.
Nonfoliated: which is when the rock Nonfoliated: which is when the rock grains are arranged randomly.grains are arranged randomly.
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Foliated RockFoliated Rock
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Nonfoliated RockNonfoliated Rock
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foliation
foliated (layered) metamorphic rocksresults from differential stress (not equal in all directions)
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foliated metamorphic rock: slate
Slate Slate is formed from is formed from shaleshale..
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foliated metamorphic rock: phyllite (higher T, P than slate)
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garnet
foliated metamorphic rock: schist (higher T, P than phyllite)…new minerals grow -- garnet (large, roundish grains)
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banding of quartz/feldspar and ferromagnesian minerals
foliated metamorphic rock: gneiss (higher T, P than schist)
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The typical transition in mineralology that results from progressive metamorphism of shale.
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non-foliated (non-layered) metamorphic rocksresults from pressure: equal in all directions
named on the basis of their composition
marble (CaCO3)
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The exterior of the Taj Mahal is constructed mainly of the metamorphic rock marble.
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non-foliated metamorphic rocks: quartzite
metamorphosed quartz sandstone
Quartzite Quartzite is formed from is formed from sandstonesandstone..
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Photo credit: R. Weller
non-foliated metamorphic rocks: hornfels
metamorphosed basalt
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DiamondsDiamonds Diamonds are formed from Diamonds are formed from CoalCoal
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Rock CycleRock Cycle Geologic forces cause rock to constantly Geologic forces cause rock to constantly
change from one type to anotherchange from one type to another
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The The Rock CycleRock Cycle describes the continually changing structure of describes the continually changing structure of rocks.rocks. Igneous, sedimentary, or metamorphic rock are just temporary Igneous, sedimentary, or metamorphic rock are just temporary
stages in the continuing changes that all rocks undergo.stages in the continuing changes that all rocks undergo.