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PEMBROOK RESOURCES
Orogenic Gold Deposits
• Definitions• Geological Environment• Age• Host Rocks• Related Deposits• Mineralization, Veins & Alteration• Structural Settings• Mode of Formation• Favorable Exploration Characteristics• World & Latin America Examples
PEMBROOK RESOURCES
Orogenic Gold Deposits
OROGENIC GOLD
INTRUSION-RELATED
EPITHERMALSPLACERS
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Orogenic Gold Deposits
• Orogenic Gold deposits are gold deposits formed in regionally metamorphosed terranes during compressional to transpressional defomation processes at convergent plate margins in accretionary and collisional orogens (Groves et al., 1998)
• World Average: 100,000’s to 100Mt @ 2 to 15 g/t Au
• Grade – Variable 1.1 (Las Cristinas) to 21.3 g/t Au (Red Lake)
• 25% of world’s gold is sourced from orogenic gold deposits
Definition
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Orogenic Gold Deposits
• Mineralization associated with accretionary to collisional tectonics at convergent plate boundaries
Geological Environment
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Orogenic Gold Deposits
Dominantly Archean to Phanerozoic
• Late Archean (2.7 to 2.55 Ga)• Early Proterozoic (2.1 to 1.8 Ga)• Late Proterozoic (700 to 600 Ma)• Late Paleozoic (455 to 340 Ma) • Mesozoic-Cenozoic (285 to 70 Ma)
Coincide with periods of crustal growthand global thermal events
Age
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Orogenic Gold Deposits
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Orogenic Gold Deposits
Kalgoorlie, Australia (40M oz)Timmins, Canada (70M oz)
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Orogenic Gold Deposits
Obuasi, Ghana (30M oz)
Telfer, Australia (21M oz)Homestake, US (27M oz)
Tanami, Australia (10M oz)
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Orogenic Gold Deposits
Murunta, Uzbekistan (170M oz)Linglong, China (16M oz)
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Orogenic Gold Deposits
• Epigenetic
• Host lithology is deformed and metamorphosed – gold deposition late during the deformation-metamorphic history
• Can be any host rock
Common Hosts
• Mafic to intermediate metavolcanic sequences(or greenstones)
• Slate and low-grade metamorphic sediments (especially greywacke)
• Poorly-developed mineral zonations both laterally and vertically
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Orogenic Gold Deposits
Systen & Vein Geometry
• Dominantly a complex (discordant) array of anastomizing moderately to steeply dipping, laminated fault-fill quartz-carbonate veins in brittle-ductile shear zones and faults, with or without fringing shallow-dipping extensional veins and breccias
• Individual veins are 10 cm to 10 meters in width and typically have 100’s meters of strike extent
• Larger systems have multiple vein zones and may be depth persistent (Calle +2 km depth)
• Stockworks and hydrothermal breccias may represent the main mineralization styles when developed in competent units
PEMBROOK RESOURCES
Orogenic Gold Deposits
Vein Textures
• Textures represent the local deformation process and vary according to the nature of the host structure (extensional vs. compressional).
• Extensional veins typically display quartz and carbonate fibres at a high angle to the vein walls and with multiple stages of mineral growth
• Compressional laminated veins are composed of massive, fine-grained quartz. When present in laminated veins, fibres are subparallel to the vein walls
• Vein as open space infill and altered wall rock as replacements
PEMBROOK RESOURCES
Orogenic Gold Deposits
Alteration
• Proximal to distal assemblages
• Scale and intensity of alteration function of system depth and wall rock composition
• Best developed in ultramafic and greenstone hosts
• In sediment-hosted systems, alteration is narrow and discrete enveloping the mineralization
• Present in veins but more likely as wall rock alteration (especially po-py)
• Comprise less than 5 (in veins) to 10% (in wall rock) of the volume of the orebody
• No significant vertical mineral zoning or change in gold grade
Precious MetalsPrecious Metals
• Gold occurs as free gold and with sulphide in veins (generally in small fractures in quartz), vein margins and in wall rock associated with iron sulphides and on the margins of rock-fragments
• Au can also contain 15 to 20% weight silver; minor silver sulposalts and tetrahedrites
• Ore-grade mineralization also occurs as disseminated sulphides in altered (carbonatized) rocks along vein selvages
• Structurally-controlled zones of dilation in “pressure shadow” settings adjacent ridge bodies (passive intrusions, more competent and rigid lithologies)
• Structurally-controlled in faults and fold closures, withprecious minerals at redox (carbonates, manganiferous units) boundaries (Sierra Pelada Au-Pd-Pt)
• Fault zone splays in carbonate-saprolite and anintrusive-buttress (?) Sadiola (+11 Moz Au)
Serra Pelada
Sadiola
Pembrook Mining Corp.
Santa HelenaPembrook Mining Corp.
Rheological ContrastsPembrook Mining Corp.
Rheological ContrastsPembrook Mining Corp.
Stratigraphy - Rheological Contrasts (& Fault)
• Fault propagation along fold axial plane and bedding parallel planesof weakness
• Lithological heterogeneity
• Zones of dilation, extension & pressure shadows
• Maraba, Suriname (+4 Moz); Essakane (+3.1 Moz)
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Orogenic Gold Deposits
Mode of Formation
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Orogenic Gold Deposits
• Deposits are related to metamorphic fluids from accretionary processes and generated by prograde metamorphism and thermal re-equilibration of subducted volcano-sedimentary terranes
• The deep-seated, Au-transporting metamorphic fluid has been channelled to higher crustal levels through major crustal faults or deformation zones
• Along its pathway, the fluid has dissolved various components - notably gold - from the volcano-sedimentary packages, including a potential gold-rich precursor.
•The fluid then precipitated as vein material or wall-rock replacement in second and third order structures at higher crustal levels through fluid-pressure cycling processes and temperature, pH and other physico-chemical variations.
Mode of Formation
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Orogenic Gold Deposits
Favorable Regional & District Targeting Criteria
1. Complex lithostratigraphy with competency contrasts
2. Isolation of competent units within incompetent units
3. Greenschist to greenschist-amphibolite transition facies metamorphism
4. Subjacent to major, crustal-scale structure
5. Lamprophyre and porphyry dikes
6. Fe-rich host-rocks and-or early magnetite alteration
7. Anticlines and domal structures
8. Flexures (dilational jogs) in major structural trends
9. Reactivation of earlier structures especially thrusts by strike-slip movement, either late in the orogenic cycle or as a later overprinting event
PEMBROOK RESOURCES
Orogenic Gold Deposits
Favorable Regional & District Targeting Criteria
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Orogenic Gold Deposits
Favorable Orogenic Gold Terranes
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Orogenic Gold Deposits
Latin American Orogenic Provinces
• Las Cristinas-Las Brisas (20 Moz Au)
• Rosebel-Nassau Trend (20 Moz Au)
• Aurora-Omai Trend (10 Moz Au)
• Pataz District (+6 Moz Au)
• Santa Helena (+5 Moz Au)
• Crixas (+3 Moz Au)
• Morro Velho(+ 15 Moz Au)
PEMBROOK RESOURCES
Orogenic Gold Deposits
Guyana Shield
Pembrook Mining Corp.
Santa HelenaPembrook Mining Corp.
• Late Paleozoic orogenic sediment-hosted gold belt in theCentral Andes of South America
• Extends for over 3,500 km x 80 km, from Northern Peruthrough Bolivia to Central Argentina
• Several historical and recent +1 Moz discoveries within the established mineral districts
• Orogenic belt is the source for the large auriferous placer deposits – Remi, Madre de Dios & Maranon Basins
• Structurally-controlled gold deposits hosted in Ordovician to Carboniferous granites and Early Paleozoic turbiditic sequences
• Potential for large-scale (+1 Moz Au) vein and disseminated gold deposits
Orogenic Gold Deposits
Eastern Andean Cordillera
Pembrook Mining Corp.
Santa HelenaPembrook Mining Corp.
Orogenic Gold Deposits
Eastern Andean Cordillera
Pembrook Mining Corp.
Santa HelenaPembrook Mining Corp.
• Active back-arc rift-basin formed as a rift-basin between the Brazilian Shield and the Arequipa Massif during the Early Paleozoic, infilled by turbiditic sedimentation until the Late Devonian
• Orogenic gold mineralization related to Late Devonian “Eoherciniana” compression (Early Devonian in Central Argentina) and Late Carboniferous (Pataz, Huachon & Amapares intrusions)
• Unexplored potential for intrusion-related mineralization during the Permo-Triassic and Miocene (San Rafael, Antana, Alumbrera, Agua Rica)
• Four distinct magmatic events – Subduction-related Carboniferous granitoids in north-central Peru; Post-orogenic Permo-Triassic; Late Triassic plutons; Miocene stocks in south-central Peru
Orogenic Gold Deposits
Eastern Andean Cordillera
Pembrook Mining Corp.
Santa HelenaPembrook Mining Corp.
Mineral Occurrences in Carboniferous Granitoids
Orogenic Gold Deposits
Pembrook Mining Corp.
CAPAC ORCOInventory 48.5Mt @ 2.04g/t Au for 3.10M ounces
- Mineralization within sequence of Ordovician sedimentary rocks.- Sequence tightly folded with NW-trending axial planes and thrusts.- Host unit is the San Jose Group; slates, mudstones, fine quartzites.- Granitic dikes spatially coincident with mineralization.
- Occurs as series of mantos.- Four mantos over a 500m vertical range.- Can be traced for up to 1400m with average thickness of 10m.- Au with quartz + sulfides (py+pyrh+asp+gn+cp), also free Au.- Control – fold noses, shears and thrusts
SANTA HELENA
Pembrook Mining Corp.
Au 8.08g/tAssociated with Fe-filled fractures
Au 1.61g/tAu with quartz vein
Au 1.66g/tAu with Fe-filled breccia
Au 15.9g/tAu with Fe-filled fractures
Au 1.16g/tAu with quartz veinlets
SANTA HELENA
Pembrook Mining Corp.SANTA HELENA – OLLACHEA
EMERGING GOLD DISTRICT
OLLACHEAPotential ?
- Area of extensive informal mining since colonial times.- Mineralization related to sheeted quartz-sulfide veins and veinlets.- Mineralization associated with pyrrhotite (magnetitic).- Previous drilling by junior explorer in 1998:
129m @ 0.74g/t Au 51m @ 0.56g/t Au 74m @ 1.04g/t Au 71m @ 0.46g/t Au 44m @ 0.90g/t Au
- MIRL work. Community agreements in place. 9 holes drilled 2008. Metallurgical test program in 2009.
- Folded and sheared clastic sediments- Stratabound sheeted zone veins/veinlets of qtz-ser-py-aspy- Gold zone within siltstone immediately beneath graphitic shale- Mineralized zone with 3km of strike and thickness from 25-95m
Black shale
0
100 m
Shale, slate, siltstone
Black shale
Quartzite
Gold Zone30-90 meters thick
Best surface geochemistry 100m @ 1.3g/t Au
Best drill intercept 110m @ 1.1g/t Au
Pembrook Mining Corp.
SANTA HELENA – AYAPATAEMERGING GOLD DISTRICT
DRILL RESULTS (1997)APD-1 7m @ 2.98g/t from 42-49mAPD-2 1.6m @ 32.80g/t from 102-103.6mAPD-2A 16m @ 0.99g/t from 107-123mAPD-3 10m @ 1.35g/t from 73-83mAPD-4 33m @ 1.85g/t from 61-94mAPD-5 69m @ 1.86g/t from 71-140m
84870008488000
381500 382500380500
8487000
381000 382000 383000
9.109.101.21.2
3.43.4
5.65.6CC
FF GG
AA
Trench D40m @ 0.60 g/t
Trench B45m @ 3.60 g/t
Trench C95m @ 0.56 g/t
Trench E65m @ 1.28 g/t
Trench A127m @ 1.40 g/t
Trench G70m @ 1.26 g/t
DD
BB
Trench F127m @ 1.31 g/t
Black graphitic shale
Mineralized zone
Proposed drill holes
TrenchC
TrenchD
TrenchE
TrenchF
TrenchG
95m @ 0.56 g/t
40m @ 0.60 g/t
65m @ 1.28 g/t
100m @ 0.866 g/t
50m @ 0.168 g/t
100m @ 1.310 g/t
70m @ 1.26 g/t
Pembrook Mining Corp.
SANTA HELENA – HIGH GRADEEMERGING GOLD DISTRICT
- Narrow (2-50cm), high-grade (15-150g/t Au)- Quartz-carbonate veins- Milky quartz with iron oxide; free gold- “white clay” wall rock alteration????
Penon de Oro
- Small, Au-bearting quartz veins with associated colluvial and alluvial workings- High-grade gold (10-100g/t Au)- “Sheeted ladder” veins in fold closures
Yanacocha
EASTERN CORDILLERA OROGENIC GOLD DEPOSITSPOTENTIAL FOR
SMALL, RICH, HIGH GRADELARGE VOLUME, BULK MINEABLE LOW GRADE
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200000
200000
220000
220000
240000
240000
910
00
00
910
00
00
912
00
00
912
00
00
914
00
00
914
00
00
916
00
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916
00
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5 0 5Kilometers
San Francisco
Pembrook Mining Corp.EASTERN CORDILLERAN
PATAZ
Orogenic Gold Belt – 160km long in Eastern CordilleraNW-trending, 1-5km wide corridor associated with the Pataz Batholith (Miss)Quartz veins within, and on margin of batholith and in Ordovician phyllitesGeochemical assemblage Au-Ag-As-Fe-Pb-Zn+Cu,Sb,Bi,Te,WThree distinct phases of vein filling (1) quartz-pyrite-arsenopyrite-ankerite (2) quartz-galena-sph-ccpy-Sb sulfosalts-Electrum-Gold (3) calcite-dolomite-quartzShoots average 7-15g/t Au and Ag to 120g/tPataz Batholith 329my; Gold mineralization 312my
PRODUCED 6M Oz; Potential +10M oz
Tertiary Volcanics
Mesozoic SandstoneLimestone
Ordovician SlateQuarzite
Cambrian - Ordovician SandstoneVolcanics
Late Proterozoic PhylliteCambrian Schist
Mississippian to Triassic Sandstone (Mitu)LimestoneSiltstone / Sandstone (Ambo)