PROTEROZOIC GOLD
Transcription
PROTEROZOIC GOLD
PROTEROZOIC GOLD Vic Wall Vic Wall and Associates Steve Massey Western Geoscience Greg Hall Golden Phoenix Interna;onal REFERENCE Wall, V. J. 2005. TAG Thermal Aureole (Pluton related) Gold Systems. AIG journal February Granites-‐Tanami: features • Major Proterozoic gold province – NT-‐WA border area, Central Australia • 300km. (E-‐W) x 200km. (N-‐S) – 15-‐20Moz. Au resources + produc;on – current produc;on ~400-‐500Koz. Au pa. – several mul;million ounce deposit clusters • The Granites, Dead Bullock Soak, Callie, Tanami • styles good grade Granites-‐Tanami: deposits (Callie: +5mozs) Granites-‐Tanami: features • Recent discoveries (Old Pirate, Buccaneer) • Ground access difficul;es – major ground posi;ons – na;ve ;tle – remote • Poorly exposed & mapped, but good regional geophysical datasets Granites-‐Tanami: methodology • Data integra;on – aeromagne;c – regional gravity – regional geology – mineral occurrences – current tenure • Regional geological interpreta;on • Targe;ng – empirical explora;on model – TAG model Granites-‐Tanami: regional geology • Similar to Pine Creek and analogies with Hall’s Creek, but – regional WNW strike of Palaeo-‐Proterozoic – flat, deeply weathered, windblown cover widespread Pine Creek: geology Pine Creek: plutons, structures & magne;cs Granites-‐Tanami: regional geology • Deposi;onal ages • Archaean/Early Prot. gneissic basement • circa. 1900Ma. metasediment-‐dominated succession • Deforma;on • ~1860Ma, slate-‐belt style, NNE-‐SSW shortening – shallow dipping regional enveloping surface • accompanied by lower greenschist metamorphism • minor subsequent deforma;on, except around plutons Granites-‐Tanami: regional lithostra;graphy Granites-‐Tanami: RTP Y#Y# Y# Y# #Y# #Yà ÃYÃY# à à Y#à à à #Y# Y à Ãà à à Ãà Y#Y#Y#Y# Tanami Dice Tanami Central Money Bul ld og Y#Y# Y# à Y# Ji ms Cen tral Y# Y# Y# Y# Ji ms West Y# Y# Y# Cal lie ÃÃà Ri dge Trium ph Hi ll Col li wobb le Sh oe Y# Y#Ãà Ãà Quorn à Y# Y# 50 km Granites-‐Tanami: regional geology • Plutonism – 1810-‐1820Ma – reduced, frac;onated I-‐type suite – emplaced 6-‐10kms. depth • Related broad thermal aureoles – metamorphic & gravity evidence: • extensive pluton roof zones • Intrusion accompanied by, around/above pluton margins – higher strain zones & faul;ng • steep stretching linea;on (high temperature) • brigle faults (lower temperature/mmic. grade) – upwarping/doming of stra;graphy Tanami area: Y# outcrop geology/ # Y#à Tangent Tanami Melon ÃTanami ÃYY# à # # Y Y RTP Ã##YÃà Tanami Dice à #Yà Yà Tanami Trasherà #Y# Y# Tanami Central Y à à Redback Rise Spider Zone Ãà Money Ãà ÃÃÃY# Ãà Bulldog Y# Jims Central Y# Ãà Camel Bore Y# Jims West Y# Y# Oberon Y# Y# 20 km Tanami area: Y# N-‐sun # Y#Yà angle Tanami Melon ÃTanami Tangent à Y à # Y# #à #à Y Y Tanami Dice RTP Tanami TrasherÃÃYYÃ##YÃ#Y#ÃY# Tanami Central Ãà Money à Redback Rise Spider Zone Ãà ÃÃÃÃY# Ãà Bulldog Y# Jims Central Y# Ãà Camel Bore Y# Jims West Y# Y# Oberon Y# Y# 20 km Tanami area: layer Y# gravity/ Y# Y#à Tangent Tanami Melon ÃTanami à Y# à # # Y Y RTP #Yà à Tanami Dice Y#à Ãà Y#Y# Y# Tanami Central Tanami TrasherÃà Y# à à Redback Rise Spider Zone Ãà Money Ãà ÃÃÃY# Ãà Bulldog Y# Jims Central Y# Ãà Camel Bore Y# Jims West Y# Y# Oberon Y# Y# 20 km Granites-‐Tanami: bouger gravity/RTP Y#Y# Y# Y# #Y# #Yà ÃYÃY# à à Y#à à à #Y# Y à Ãà à à Ãà Y#Y#Y#Y# Tanami Dice Tanami Central Money Bul ld og Y#Y# Y# à Y# Ji ms Cen tral Y# Y# Y# Y# Ji ms West Y# Y# Y# Cal lie ÃÃà Ri dge Trium ph Hi ll Col li wobb le Sh oe Y# Y#Ãà Ãà Quorn à Y# Y# 50 km Granites-‐Tanami: geology model Granites-‐Tanami: key deposits & geology • ‘The Granites’ cluster – hosted by iron forma;on/pelite package – in high temperature, high strain zone • proximal and subparallel to and wrapping around granitoid pluton margin (~E-‐W trending) – short strike length (<300m), long down plunge extent of ore zones/lenses • 7-‐15g/t Au, average 11g/t Au underground grades • bulk mineable widths – bedding subparallel carbonate-‐quartz & calc-‐silicate veining • related gold, arsenopyrite, pyrrho;te enrichment – similar lithologies & parageneses to Musselwhite, Lupin, etc Cerberus Mi The Granites area: geology/ Avon RTP Gahn Shoe Triumph Hill Colliwobble Y# Y# Quorn à ÃÃà à Y# 20 km Cerberus Mi The Granites area: N-‐sun angle Avon RTP Gahn Shoe Triumph Hill Colliwobble Y# Y# Quorn à ÃÃà à Y# 20 km Cerberus M The Granites area: layer gravity/ Avon RTP Gahn Triumph Hill Colliwobble Shoe Y# Y# Quorn à ÃÃà à Y# 20 km Callie area: N-‐sun angle RTP Avon Ridge Gahn Y#à à Ãà Callie Y# à Triumph Hill Fumarole Colliwobble Sleepy Hollow Y# Y# 20 km Y# Dead Bullock Soak geology Callie geology Callie: Cross sec;on Callie lithologies Granites-‐Tanami: key deposits & geology • Callie (>7Moz.Au) – hosted by reduced (carbonaceous) metasediments – in faulted an;formal hinge zone (~E-‐W trending) – bedding subparallel-‐ & steep quartz-‐rich veinlet system • 7-‐10g/t, bulk mineable widths – moderate temperature • bio;te stable, weak altera;on in metasediment hornfels – in pluton roof zone above & structures subparallel to pluton margin – Musselwhite-‐like structural semng Callie area: bouger gravity/ RTP Avon Ridge Gahn Y#à à Ãà Callie Y# à Triumph Hill Fumarole Colliwobble Sleepy Hollow Y# Y# 20 km Y# Callie area: layer gravity/ RTP Avon Ridge Gahn Y#à à Ãà Callie Y# à Triumph Hill Fumarole Colliwobble Sleepy Hollow Y# Y# 20 km Callie area: outcrop geology/ RTP Avon Ridge Gahn Y#à à Ãà Callie Y# à Triumph Hill Fumarole Colliwobble Sleepy Hollow Y# Y# 20 km Y# Pluton-‐related (Thermal Aureole) Gold 6 2 1 Ì 3 5 2 4 5km GRANITOID INTRUSIONS THERMAL AUREOLE COUNTRY ROCKS KEY STRUCTURAL ZONES 1 2 3 4 5 6 GOLD DEPOSIT SETTINGS Fort Knox Sukhoi Log, Kumtor Pogo, Vasilkovskoye Granites-Tanami Muruntau Obuasi, Telfer TAG: Western Australia • Telfer, >30 Moz. Au (-‐Cu) deposit • bedding parallel veins; discordant stockworks, breccias • high grade quartz-‐carbonate-‐pyrite-‐chalcopyrite veins – hosted by ?mid Proterozoic siliciclas;c succession with some carbonates & evaporites – fold-‐thrust compressional deforma;on & greenschist metamorphism; • reac;va;on of basement structures – felsic pluton/batholith emplacement • post main regional deforma;ons • ~620Ma., similar isotopic age to Au mineraliza;on • frac;onated I-‐type suites Telfer Au-‐Cu deposit Telfer: district geology TAG: Western Australia • Telfer deposit localised in – pluton roof zone (above pluton edge?) • regional gravity signature • note map pagern, nearby skarns & other pluton proximal deposits – outer aureole semng – mul;ply plunging, asymmetric, an;clinorial ‘domal’ structures • reac;vated fold-‐(blind) thrust system – dila;on along bedding controlled by stra;graphy, small thrusts – dila;on in discordant zones, related to small scale fault-‐fold systems – favourably thin-‐bedded stra;graphy, in over more than 1km. thickness • higher temperature altera;on & higher Cu with increasing depth • highly saline fluids Telfer ‘dome’ Telfer cross secCon Telfer: ore zones Telfer: structural geology Telfer: structural interpretaCon Telfer gravity magne;c image W.A. N.T. Pluton-‐related (Thermal Aureole) Gold 6 2 1 Ì 3 5 2 4 5km GRANITOID INTRUSIONS THERMAL AUREOLE COUNTRY ROCKS KEY STRUCTURAL ZONES 1 2 3 4 5 6 GOLD DEPOSIT SETTINGS Fort Knox Sukhoi Log, Kumtor Pogo, Vasilkovskoye Granites-Tanami Muruntau Obuasi, Telfer Telfer bouger gravity Where next? W.A. N.T. PROTEROZOIC GOLD Vic Wall Vic Wall and Associates Steve Massey Western Geoscience Greg Hall Golden Phoenix Interna;onal
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