GOLD IN NEWFOUNDLAND...Appalachian and pre-Appalachian tectonic evolution of the Newfoundland...
Transcript of GOLD IN NEWFOUNDLAND...Appalachian and pre-Appalachian tectonic evolution of the Newfoundland...
The Island of Newfoundland represents an emerging, underexplored gold district, where focused exploration for precious metals was essentially non-existent prior to the early 1980's. Gold has been mined from epithermal (gold-copper) and orogenic (gold-only) deposits, and as a by-product in several volcanogenic massive sulphide (VMS) operations. Production from orogenic and VMS deposits is continuing, and a number of new advanced projects are targeting similar deposit styles. Ongoing exploration is also directed at both high- and low-sulphidation epithermal deposits. Recent option- and joint-venture-agreements, coupled with new claim-staking, indicate renewed interest in these underexplored terranes.
January 2020
Oro
geni
c
Line
arD
DH
: (H
Pon
d) 3
.40
m @
11.
70 g
/t A
u;(D
ome)
8.6
m @
18.
46 g
/T A
u;(R
oad)
2.7
m @
15.
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T Au
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he K
nob)
14.
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@ 8
.98
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tan
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.3 m
@ 1
0.2
g/t A
u
Moo
sehe
adD
DH
: 11.
9m @
44.
9 g/
t Au;
24.
90m
@ 3
3.56
g/t
Au;
5.10
m @
124
.20g
/t A
u
VM
SVu
lcan
Min
eral
s In
c.
Colc
hest
erD
DH
: 5.8
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2.8
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u;4.
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5.6
0 g/
t Au,
2.3
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n
Terr
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iner
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art
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@ 0
.13
g/t A
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herm
al /
Porp
hyry
DD
H: 8
9.2
m @
0.4
1 g/
t Au
and
15.4
g/t
Ag
Big
Easy
Cart
ier I
ron
Corp
orat
ion
Oth
erD
. Hic
ksLi
ttle
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DH
: (W
olf P
ond
Zone
) 2.5
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(22
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t Zon
e) 2
.5 m
@ 4
.9 g
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DH
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b
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dro
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urce
s Lt
d.St
agho
rnD
DH
: 26.
3 m
@ 1
.37
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Soko
man
Min
eral
s Co
rp.
New
Fou
nd G
old
Corp
.
DD
H: 5
.50
m @
5.4
9 g/
t Au
and
133.
51 g
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g H
erita
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sour
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.5%
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110
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and
1.7
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usio
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sted
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nd L
. Qui
nlan
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r Lan
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(Mos
quito
Hill
) 11,
180,
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@ 0
.546
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38
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@ 0
.457
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Silv
ertip
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lora
tion
Cons
ulta
nts
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Brad
y
(Rei
d Po
rphy
ry Z
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5,9
90,0
00 t
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* @
0.5
88 g
/t A
u
Firs
t Min
ing
Gol
d Co
rp.
H
ope
Broo
k5,
500,
000
t ind
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@ 4
.77
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6,00
0 t I
nfer
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@ 4
.11
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nfer
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.68%
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8% P
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6 g/
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7 g/
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13.1
% b
arite
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h Ta
lly P
ond
Nor
Zinc
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t Lea
min
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14,1
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00 t
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17.
12 g
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d 1.
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/t A
u Ca
lline
x M
ines
Inc.
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herm
al
Mar
atho
n G
old
Corp
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geni
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Mar
itim
e Re
sour
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Corp
.
(All
depo
sits
) 45,
146,
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t mea
sure
d an
d in
dica
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@ 1
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26
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t Au
(Orio
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indi
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mer
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atad
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inin
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at A
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den
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lyn
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.79
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t Au
(Cen
tral
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e) 7
,686
,600
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dica
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2.7
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7.6
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2,03
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0 t i
nfer
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@ 2
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aux
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indo
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lass
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45,7
00 t
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.82
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315,
000
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952
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ope
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k (P
P)11
,200
,000
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4 g/
t Au
Buch
ans
(PP)
16,1
96,8
76 t
@ 1
4.5%
Zn,
7.6
% P
b,1.
3% C
u, 1
26 g
/t A
g an
d 1.
4 g/
t Au
Cons
olid
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es L
imite
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mbl
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P)(M
ain)
399
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t @
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% C
u, 5
.1 g
/t A
u;(M
ing)
1,9
91,5
92 t
@ 3
.7%
Cu,
22
g/t
Ag
and
2.4
g/t A
u
Firs
t Mar
itim
e M
inin
g Co
rpor
atio
n (7
)Ti
lt Co
ve (P
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oduc
ed 4
2,42
5 oz
gol
d as
byp
rodu
ct
Atla
ntic
Coa
st C
oppe
r (8)
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le B
ay (P
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ed 6
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oz
gold
as
bypr
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t
Oro
geni
c
VM
S
Asa
rco
Inc.
(5)
Ram
bler
Met
als
and
Min
ing
plc
Ram
bler
(P)
D
uck
Pond
(PP)
4,10
0,00
0 t @
3.3
% C
u, 5
.7%
Zn,
59
g/t A
gan
d 0.
9 g/
t Au
Teck
Res
ourc
es L
imite
d
476,
300t
@1.
39 A
u
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herm
al
CURR
ENT
AN
D P
AST
PRO
DU
CERS
Ow
ner/
Opt
ione
e/Co
ntac
tPr
oper
ty(Z
one)
/ Re
sour
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Dri
ll In
ters
ecti
on
Ow
ner/
Opt
ione
e/Co
ntac
tPr
oper
tyRe
sour
ce
JBP
Line
arU
nity
Res
ourc
es In
c.D
DH
: (Po
cket
Pon
d) 1
1.90
m @
11.
11 g
/t A
u
Ant
ler G
old
Inc.
Wild
ing
Lake
DD
H: (
Elm
Zon
e) 5
.35m
@ 1
0.0
g/t A
u
KEY:
PP=
Past
Pro
duce
r P=
Prod
ucer
*43
-101
or J
ORC
com
plia
nt R
esou
rce
Estim
ate
Curr
ent h
olde
r (1)
Ram
bler
Met
als
and
Min
ing
Cana
da (2
) Mar
itim
e Re
sour
ces
Corp
. (3)
Ana
cond
a M
inin
g In
c.(4
) Firs
t Min
ing
Gol
d Co
rp. (
5) B
ucha
ns R
esou
rces
Ltd
. (6)
Ram
bler
Met
als
and
Min
ing
Cana
da(7
) Met
als
Cree
k Re
sour
ces
Corp
. (8)
Vul
can
Min
eral
s In
c.
Thre
shol
dD
DH
inte
rsec
tion
g/t
Au
x m
> 1
0
DD
H: 6
.4 m
@ 2
.26
g/t A
uCl
arks
Bro
okM
etal
s Cr
eek
Reso
urce
s Co
rp.
23,4
48,0
00 m
easu
red
and
indi
cate
d*@
1.6
4% C
u, 0
.32g
/t A
u an
d 2.
52g/
t Ag
Poin
t Rou
sse
/St
og'e
r Tig
ht (P
)20
4,00
0 t i
ndic
ated
* @
3.5
9 g/
t Au;
25
2,00
0 t I
nfer
red*
@ 3
.27
g/t A
u
B
B
BB
B
B
B
B
B
B
BB
B
B
B
B
BBBB
0 50 100
Kilometres
BB
BB Current gold producers
Gold showing Past gold producers
Siluro-Devonian
epithermal gold systems
are hosted by early
Paleozoic subaerial
volcanic rocks and
terrestrial and marine
sedimentary rocks.
Gold is hosted by Late
Proterozoic and Paleozoic
intrusions in disparate settings.
Some of the most important
deposits occur where intrusions
are spatially associated with
major crustal structures.
Orogenic gold of Paleozoic
age is associated with
mesothermal-style
quartz-sulphide veins and
quartz-carbonate shear
zones in a variety of
deformed metamorphic
terranes.
Orogenic gold systems
occur in mid-Paleozoic
slate belts developed in
Ordovician and Silurian
sediments.
Cambro-Ordovician
gold-bearing
hydrothermal systems
are typically associated
with the formation of
volcanogenic massive
sulphide deposits.
Large-scale gold-bearing
systems of late Proterozoic
age include well-preserved,
low- and high-sulphidation
epithermal examples, and
intrusion-related
mineralization.
DUNNAGEZONE
HUMBERZONE
GANDER ZONE
AVALON ZONE
AVALON ZONENeoproterozoic to Ordovician
Subaerial-marinesedimentary rocks
Mafic and felsic volcanicrocks
DUNNAGE & GANDER ZONESCambrian to Silurian
Marine clastic and volcanic rocks
Ophiolitic rocks
Metasedimentary rocks and migmatite
Neoproterozoic-Ordovician
Platformal carbonate rocks
Clastic and metasedimentaryrocks
Basal clastic, carbonate and volcanic rocks
Gneisses and granites
Mesoproterozoic and Neoproterozoic
Neoproterozoic to OrdovicianHUMBER ZONE
INTRUSIVE ROCKS
Ordovician-Devonian intrusions
Neoproterozoic intrusions
Devonian to Carboniferous sedimentary rocks
Silurian sedimentary and volcanic rocks
OVERLAP SEQUENCES
Key
Current producer
Past producer
Project with resource estimate
Occurrence with drill-hole data
CANADA
U.S.A.
U.S.A.
Geology and Tectonic Zones: Island of Newfoundland
showing producers, past-producers and principal gold occurrences
(representative projects with resource estimates and drill-hole data)
Bay d’Espoir
Gander
Grand Falls
CornerBrook
Gander
Grand Falls
CornerBrook
St. John’sPort aux Basques
HammerdownNugget Pond
Orion
Tilt Cove
Jackson’s Arm
Stog’er Tight
ColchesterViking
Little Bay
Point Leamington
Valentine Lake
GoldenPromise
Buchans
Huxter-Lane/Brady
Little River
Moosehead JBP Linear
Knob
Lemarchant
Titan
Cape Ray
Glover Island
Kitchen
Boomerang
Staghorn
Hope Brook
Stewart
Big Easy
Heritage
Pine Cove
Rambler
Clarks BrookDuck Pond
HammerdownNugget Pond
Orion
Tilt Cove
Rattling Brook/Jackson’s
Arm
Stog’er Tight
ColchesterThor/Viking
Little Bay
Point Leamington
Valentine Lake
GoldenPromise
Buchans
Huxter-Lane/Brady
Little River
Moosehead JBP Linear
Knob
Lemarchant
Titan
Cape Ray
Glover Island
Kitchen
Boomerang
Staghorn
Hope Brook
Stewart
Big Easy
Heritage
Pine Cove
Rambler
Duck Pond Clarks Brook
0 20 40 60 80
kilometres
100
Widespread magmatism and deformation characterized the
Appalachian and pre-Appalachian tectonic evolution of the
Newfoundland segment of the orogen. At several discrete
intervals, magmatism was accompanied by the formation of
large-scale gold-bearing hydrothermal alteration systems at
di�erent crustal levels. These systems host gold orebodies in
both Late Proterozoic and Paleozoic rocks, and in many
instances, are associated with major crustal structures.
Several of the styles and settings of gold mineralization are
analogous, at varying levels of detail, with world-class
deposits in ancient deformed terranes and in
Mesozoic-Cenozoic belts. These include epithermal,
orogenic, sediment-hosted and intrusion-related deposit
types. This unique geological setting creates an excellent
opportunity for new mineral discoveries in an
underexplored, readily accessible mineral district.
The Island of Newfoundland, situated off the Atlantic coast of mainland Canada, is part of the larger Appalachian-Caledonian orogenic belt. Its geology records the development and destruction of an ancient proto-Atlantic Ocean, a cycle that culminated in the mid-Paleozoic collision of pre-Appalachian crustal blocks of mid- to late Proterozoic age and contrasting tectonic origin. Vestiges of this ancient ocean are extensively preserved in the central part of the island, within the Dunnage Zone. This medial region is bounded by contrasting Proterozoic to early Paleozoic elements of the opposing continental margins: Gander and Avalon zones to the east and Humber Zone to the west.
GOLD IN NEWFOUNDLAND
Front Cover: photo courtesy of Marathon Gold Corp.
Wilding LakeWilding Lake
Hickeys PondHickeys Pond
B
B
BB
B
B
B
B
B
B
BB
B
B
B
B
BBBB
0 50 100
Kilometres
BB
BB Current gold producers
Gold showing Past gold producers
Siluro-Devonian
epithermal gold systems
are hosted by early
Paleozoic subaerial
volcanic rocks and
terrestrial and marine
sedimentary rocks.
Gold is hosted by Late
Proterozoic and Paleozoic
intrusions in disparate settings.
Some of the most important
deposits occur where intrusions
are spatially associated with
major crustal structures.
Orogenic gold of Paleozoic
age is associated with
mesothermal-style
quartz-sulphide veins and
quartz-carbonate shear
zones in a variety of
deformed metamorphic
terranes.
Orogenic gold systems
occur in mid-Paleozoic
slate belts developed in
Ordovician and Silurian
sediments.
Cambro-Ordovician
gold-bearing
hydrothermal systems
are typically associated
with the formation of
volcanogenic massive
sulphide deposits.
Large-scale gold-bearing
systems of late Proterozoic
age include well-preserved,
low- and high-sulphidation
epithermal examples, and
intrusion-related
mineralization.
DUNNAGEZONE
HUMBERZONE
GANDER ZONE
AVALON ZONE
AVALON ZONENeoproterozoic to Ordovician
Subaerial-marinesedimentary rocks
Mafic and felsic volcanicrocks
DUNNAGE & GANDER ZONESCambrian to Silurian
Marine clastic and volcanic rocks
Ophiolitic rocks
Metasedimentary rocks and migmatite
Neoproterozoic-Ordovician
Platformal carbonate rocks
Clastic and metasedimentaryrocks
Basal clastic, carbonate and volcanic rocks
Gneisses and granites
Mesoproterozoic and Neoproterozoic
Neoproterozoic to OrdovicianHUMBER ZONE
INTRUSIVE ROCKS
Ordovician-Devonian intrusions
Neoproterozoic intrusions
Devonian to Carboniferous sedimentary rocks
Silurian sedimentary and volcanic rocks
OVERLAP SEQUENCES
Key
Current producer
Past producer
Project with resource estimate
Occurrence with drill-hole data
CANADA
U.S.A.
U.S.A.
Geology and Tectonic Zones: Island of Newfoundland
showing producers, past-producers and principal gold occurrences
(representative projects with resource estimates and drill-hole data)
Bay d’Espoir
Gander
Grand Falls
CornerBrook
Gander
Grand Falls
CornerBrook
St. John’sPort aux Basques
HammerdownNugget Pond
Orion
Tilt Cove
Jackson’s Arm
Stog’er Tight
ColchesterViking
Little Bay
Point Leamington
Valentine Lake
GoldenPromise
Buchans
Huxter-Lane/Brady
Little River
Moosehead JBP Linear
Knob
Lemarchant
Titan
Cape Ray
Glover Island
Kitchen
Boomerang
Staghorn
Hope Brook
Stewart
Big Easy
Heritage
Pine Cove
Rambler
Clarks BrookDuck Pond
HammerdownNugget Pond
Orion
Tilt Cove
Rattling Brook/Jackson’s
Arm
Stog’er Tight
ColchesterThor/Viking
Little Bay
Point Leamington
Valentine Lake
GoldenPromise
Buchans
Huxter-Lane/Brady
Little River
Moosehead JBP Linear
Knob
Lemarchant
Titan
Cape Ray
Glover Island
Kitchen
Boomerang
Staghorn
Hope Brook
Stewart
Big Easy
Heritage
Pine Cove
Rambler
Duck Pond Clarks Brook
0 20 40 60 80
kilometres
100
Widespread magmatism and deformation characterized the
Appalachian and pre-Appalachian tectonic evolution of the
Newfoundland segment of the orogen. At several discrete
intervals, magmatism was accompanied by the formation of
large-scale gold-bearing hydrothermal alteration systems at
di�erent crustal levels. These systems host gold orebodies in
both Late Proterozoic and Paleozoic rocks, and in many
instances, are associated with major crustal structures.
Several of the styles and settings of gold mineralization are
analogous, at varying levels of detail, with world-class
deposits in ancient deformed terranes and in
Mesozoic-Cenozoic belts. These include epithermal,
orogenic, sediment-hosted and intrusion-related deposit
types. This unique geological setting creates an excellent
opportunity for new mineral discoveries in an
underexplored, readily accessible mineral district.
The Island of Newfoundland, situated off the Atlantic coast of mainland Canada, is part of the larger Appalachian-Caledonian orogenic belt. Its geology records the development and destruction of an ancient proto-Atlantic Ocean, a cycle that culminated in the mid-Paleozoic collision of pre-Appalachian crustal blocks of mid- to late Proterozoic age and contrasting tectonic origin. Vestiges of this ancient ocean are extensively preserved in the central part of the island, within the Dunnage Zone. This medial region is bounded by contrasting Proterozoic to early Paleozoic elements of the opposing continental margins: Gander and Avalon zones to the east and Humber Zone to the west.
GOLD IN NEWFOUNDLAND
Front Cover: photo courtesy of Marathon Gold Corp.
Wilding LakeWilding Lake
Hickeys PondHickeys Pond
The Island of Newfoundland represents an emerging, underexplored gold district, where focused exploration for precious metals was essentially non-existent prior to the early 1980's. Gold has been mined from epithermal (gold-copper) and orogenic (gold-only) deposits, and as a by-product in several volcanogenic massive sulphide (VMS) operations. Production from orogenic and VMS deposits is continuing, and a number of new advanced projects are targeting similar deposit styles. Ongoing exploration is also directed at both high- and low-sulphidation epithermal deposits. Recent option- and joint-venture-agreements, coupled with new claim-staking, indicate renewed interest in these underexplored terranes.
January 2020
Oro
geni
c
Line
arD
DH
: (H
Pon
d) 3
.40
m @
11.
70 g
/t A
u;(D
ome)
8.6
m @
18.
46 g
/T A
u;(R
oad)
2.7
m @
15.
4 g/
T Au
;(T
he K
nob)
14.
2 m
@ 8
.98
g/t A
u
R. Q
uinl
anTi
tan
DD
H: 3
.3 m
@ 1
0.2
g/t A
u
Moo
sehe
adD
DH
: 11.
9m @
44.
9 g/
t Au;
24.
90m
@ 3
3.56
g/t
Au;
5.10
m @
124
.20g
/t A
u
VM
SVu
lcan
Min
eral
s In
c.
Colc
hest
erD
DH
: 5.8
m @
3.9
1 g/
t Au,
2.8
1% C
u;4.
5m @
5.6
0 g/
t Au,
2.3
0% Z
n
Terr
aX M
iner
als
Inc.
Stew
art
DD
H: 1
11m
@ 0
.13
g/t A
u, 0
.05%
Cu
Epit
herm
al /
Porp
hyry
DD
H: 8
9.2
m @
0.4
1 g/
t Au
and
15.4
g/t
Ag
Big
Easy
Cart
ier I
ron
Corp
orat
ion
Oth
erD
. Hic
ksLi
ttle
Riv
erD
DH
: (W
olf P
ond
Zone
) 2.5
m @
5.8
g/t
Au;
(22
Wes
t Zon
e) 2
.5 m
@ 4
.9 g
/t A
u;D
DH
: 3.0
m @
4.8
g/t
Au;
0.9
m @
30.
6% S
b
Qua
dro
Reso
urce
s Lt
d.St
agho
rnD
DH
: 26.
3 m
@ 1
.37
g/t A
u
Soko
man
Min
eral
s Co
rp.
New
Fou
nd G
old
Corp
.
DD
H: 5
.50
m @
5.4
9 g/
t Au
and
133.
51 g
/t A
g H
erita
gePu
ddle
Pon
d Re
sour
ces
Inc.
Epit
herm
al
REPR
ESEN
TATI
VE
GO
LD O
CCU
RREN
CES
WIT
H D
RILL
DAT
A
VM
STu
lks
Sout
h(B
oom
eran
g) 1
,364
,600
t in
dica
ted*
@ 7
.1%
Zn,
3.0
%
Pb, 0
.5%
Cu,
110
g/t
Ag
and
1.7
g/t A
u
Intr
usio
n-ho
sted
R. a
nd L
. Qui
nlan
H
uxte
r Lan
e
(Mos
quito
Hill
) 11,
180,
000
t ind
icat
ed*
@ 0
.546
g/t
Au;
38
,760
,000
t in
ferr
ed*
@ 0
.457
g/t
Au
Silv
ertip
Exp
lora
tion
Cons
ulta
nts
Inc.
Brad
y
(Rei
d Po
rphy
ry Z
one)
5,9
90,0
00 t
infe
rred
* @
0.5
88 g
/t A
u
Firs
t Min
ing
Gol
d Co
rp.
H
ope
Broo
k5,
500,
000
t ind
icat
ed*
@ 4
.77
g/t A
u;83
6,00
0 t I
nfer
red*
@ 4
.11
g/t A
u
(Lem
arch
ant)
2.4
20,0
00 t
indi
cate
d* @
6.1
5% Z
n,1.
60%
Pb,
0.6
8% C
u, 1
.22
g/t A
u, 6
4.0
g/t A
gan
d 23
.5%
bar
ite56
0,00
0 t i
nfer
red*
@ 4
.68%
Zn,
1.0
8% P
b,0.
45%
Cu,
1.0
6 g/
t Au,
44.
7 g/
t Ag
and
13.1
% b
arite
Sout
h Ta
lly P
ond
Nor
Zinc
Ltd
.
Poin
t Lea
min
gton
14,1
00,0
00 t
infe
rred
* @
1.8
6% Z
n, 0
.42%
Cu,
0.
02%
Pb,
17.
12 g
/t A
g an
d 1.
07 g
/t A
u Ca
lline
x M
ines
Inc.
Epit
herm
al
Mar
atho
n G
old
Corp
orat
ion
Vale
ntin
e La
ke G
reen
Bay
Mou
ntai
n La
ke M
iner
als
Inc.
G
love
r Isl
and
(Lun
ch P
ond
Sout
h Ex
tens
ion
Zone
) 1,
029,
000
t Ind
icat
ed*
@ 1
.76
g/t A
u;2,
076,
000
Infe
rred
* @
1.81
g/t
Au
Oro
geni
c
Mar
itim
e Re
sour
ces
Corp
.
(All
depo
sits
) 45,
146,
000
t mea
sure
d an
d in
dica
ted*
@ 1
.854
g/t
Au;
26
,857
,000
infe
rred
* @
1.7
74g/
t Au
(Orio
n) 1
,096
,000
t m
easu
red
and
indi
cate
d*
@ 4
.47
g/t A
u;1,
288,
000
t inf
erre
d* @
5.4
4 g/
t Au
(Ham
mer
dow
n) 7
27,5
00 t
mea
sure
d an
d in
dica
ted*
@
11.
59 g
/t A
u;1,
767,
000
t inf
erre
d* @
7.6
8 g/
t Au
Cape
Ray
M
atad
or M
inin
g Lt
d.
Gre
at A
tlant
ic R
esou
rces
Cor
p.
Gol
den
Prom
ise
(Jac
lyn
Zone
) 357
,500
t in
ferr
ed*
@ 9
.3 g
/t A
u
Ana
cond
a M
inin
g In
c.G
reat
Nor
ther
n(T
hor)
937
,000
t in
dica
ted*
@ 2
.09
g/t A
u;35
0,00
0 t I
nfer
red*
@ 1
.79
g/t A
u(R
attli
ng B
rook
) 5,4
60,0
00 t
infe
rred
* @
1.4
5 g/
t Au
(Cen
tral
Zon
e) 7
,686
,600
t in
dica
ted*
@
2.7
g/t
Au
and
7.6
g/t A
g;
2,03
0,70
0 t i
nfer
red*
@ 2
.3 g
/t A
u an
d 8.
0 g/
t Ag
(Isle
aux
Mor
t ) 7
82,6
00 t
infe
rred
* @
2.4
g/t
Au
(Big
Pon
d an
d W
indo
w G
lass
Hill
) 3,7
45,7
00 t
infe
rred
* @
1.3
g/t
Au
AD
VAN
CED
PRO
JECT
S W
ITH
RES
OU
RCE
ESTI
MAT
ES
Poin
t Rou
sse
(Arg
yle)
543
,000
t in
dica
ted*
@ 2
.19
g/t A
u;51
7,00
0 f i
nfer
red*
@ 1
.82
g/t A
u
Ana
cond
a M
inin
g In
c.
Poin
t Rou
sse
/Pi
ne C
ove
(PP)
863,
500
t ind
icat
ed*
@ 2
.07
g/t A
u
Rich
mon
t Min
es In
c. (1
)N
ugge
t Pon
d (P
P)48
8,00
0 t @
11.
1 g/
t Au
Rich
mon
t Min
es In
c. (2
)H
amm
erdo
wn
(PP)
315,
000
t @ 1
6.1
g/t A
u
Min
g M
iner
als
Inc.
(3)
Stog
'er T
ight
(PP)
Prod
uctio
n by
Min
g M
iner
als
of1,
952
ounc
es A
u an
d 86
1 ou
nces
Ag
BP C
anad
a In
c./
Roya
l Oak
Min
es In
c. (4
) H
ope
Broo
k (P
P)11
,200
,000
t @
4.5
4 g/
t Au
Buch
ans
(PP)
16,1
96,8
76 t
@ 1
4.5%
Zn,
7.6
% P
b,1.
3% C
u, 1
26 g
/t A
g an
d 1.
4 g/
t Au
Cons
olid
ated
Ram
bler
Min
es L
imite
d (6
)Ra
mbl
er (P
P)(M
ain)
399
,000
t @
1.3
% C
u, 5
.1 g
/t A
u;(M
ing)
1,9
91,5
92 t
@ 3
.7%
Cu,
22
g/t
Ag
and
2.4
g/t A
u
Firs
t Mar
itim
e M
inin
g Co
rpor
atio
n (7
)Ti
lt Co
ve (P
P)Pr
oduc
ed 4
2,42
5 oz
gol
d as
byp
rodu
ct
Atla
ntic
Coa
st C
oppe
r (8)
Litt
le B
ay (P
P)Pr
oduc
ed 6
,271
oz
gold
as
bypr
oduc
t
Oro
geni
c
VM
S
Asa
rco
Inc.
(5)
Ram
bler
Met
als
and
Min
ing
plc
Ram
bler
(P)
D
uck
Pond
(PP)
4,10
0,00
0 t @
3.3
% C
u, 5
.7%
Zn,
59
g/t A
gan
d 0.
9 g/
t Au
Teck
Res
ourc
es L
imite
d
476,
300t
@1.
39 A
u
Epit
herm
al
CURR
ENT
AN
D P
AST
PRO
DU
CERS
Ow
ner/
Opt
ione
e/Co
ntac
tPr
oper
ty(Z
one)
/ Re
sour
ce /
Dri
ll In
ters
ecti
on
Ow
ner/
Opt
ione
e/Co
ntac
tPr
oper
tyRe
sour
ce
JBP
Line
arU
nity
Res
ourc
es In
c.D
DH
: (Po
cket
Pon
d) 1
1.90
m @
11.
11 g
/t A
u
Ant
ler G
old
Inc.
Wild
ing
Lake
DD
H: (
Elm
Zon
e) 5
.35m
@ 1
0.0
g/t A
u
KEY:
PP=
Past
Pro
duce
r P=
Prod
ucer
*43
-101
or J
ORC
com
plia
nt R
esou
rce
Estim
ate
Curr
ent h
olde
r (1)
Ram
bler
Met
als
and
Min
ing
Cana
da (2
) Mar
itim
e Re
sour
ces
Corp
. (3)
Ana
cond
a M
inin
g In
c.(4
) Firs
t Min
ing
Gol
d Co
rp. (
5) B
ucha
ns R
esou
rces
Ltd
. (6)
Ram
bler
Met
als
and
Min
ing
Cana
da(7
) Met
als
Cree
k Re
sour
ces
Corp
. (8)
Vul
can
Min
eral
s In
c.
Thre
shol
dD
DH
inte
rsec
tion
g/t
Au
x m
> 1
0
DD
H: 6
.4 m
@ 2
.26
g/t A
uCl
arks
Bro
okM
etal
s Cr
eek
Reso
urce
s Co
rp.
23,4
48,0
00 m
easu
red
and
indi
cate
d*@
1.6
4% C
u, 0
.32g
/t A
u an
d 2.
52g/
t Ag
Poin
t Rou
sse
/St
og'e
r Tig
ht (P
)20
4,00
0 t i
ndic
ated
* @
3.5
9 g/
t Au;
25
2,00
0 t I
nfer
red*
@ 3
.27
g/t A
u