1993
DOI: 10.1016/0169-1368(93)90021-p
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Archaean lode gold deposits in Africa: Crustal setting, metallogenesis and cratonization

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Cited by 48 publications
(32 citation statements)
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“…Several deposits are associated with sulphidised brittle-ductile shear zones, including gold in sheeted and stockwork quartz veins, copper as malachite in buck quartz veins, and tourmaline and topaz in pegmatite and buck quartz veins (Foster and Piper, 1993;Lompo, 2001;Castaing et al, 2003). Foster and Piper (1993), Béziat et al (2008) have restricted gold mineralization in the West African Craton to the Eburnean tectono-thermal event, but this does not include gold hosted by Tarkwa Group meta-sedimentary units in Ghana Feybesse et al, 2006). Bossière et al (1996) concluded that the Tarkwa Group meta-sedimentary units in the study area have no economic value.…”
Section: Geological Settingmentioning
confidence: 97%
“…Several deposits are associated with sulphidised brittle-ductile shear zones, including gold in sheeted and stockwork quartz veins, copper as malachite in buck quartz veins, and tourmaline and topaz in pegmatite and buck quartz veins (Foster and Piper, 1993;Lompo, 2001;Castaing et al, 2003). Foster and Piper (1993), Béziat et al (2008) have restricted gold mineralization in the West African Craton to the Eburnean tectono-thermal event, but this does not include gold hosted by Tarkwa Group meta-sedimentary units in Ghana Feybesse et al, 2006). Bossière et al (1996) concluded that the Tarkwa Group meta-sedimentary units in the study area have no economic value.…”
Section: Geological Settingmentioning
confidence: 97%
“…Plan géologique et stéréogrammes des éléments structuraux de l'indice "Mariposite" 32 FIGURE 7. Photomicrographies du matériel bréchique associé à la faille "sud" à l'indice "Mariposite" 37 (Roberts 1987;Colvine et al 1988;Card et al 1989;Foster 1989;Groves et al 1989;Groves et Foster 1991;Foster et Piper 1993;Hodgson 1990Hodgson , 1993Robert 1995) ont mis en évidence un ensemble de caractéristiques communes à la plupart de ces gisements à travers le monde. Il ressort que la plupart des gisements hydrothermaux d'or archéens sont spatialement associés avec des failles d'échelle crustale et qu'ils se trouvent à l'intérieur ou en bordure des ceintures de roches vertes métamorphisées au faciès des schistes verts jusqu'au faciès des amphibolites.…”
Section: Resumeunclassified
“…Similar structurallycontrolled gold mineralisation is found within the Archaean greenstone belts of Sierra Leone; the gold mineralisation appears to have formed at somewhat higher pressure than that in other greenstone belts worldwide (Barrie and Touret, 1999). The timing of gold mineralisation is not well known, but is generally considered to be late Archaean, potentially associated with the c. 2800 Ma granitoid intrusions that occur throughout the Kénéma-Man domain (Foster and Piper, 1993).…”
Section: Placer Gold Depositsmentioning
confidence: 93%
“…The mineralisation, which may comprise quartz veins, breccia zones, stringers and disseminations, typically extends over widths of 10-20 m and may have a strike extent of more than a kilometre. Structure exerts a strong control on its distribution with north-easttrending zones of intense shearing being particularly important (Foster and Piper, 1993). Other favourable sites include zones of polyphase deformation, fold limbs and closures, and competency contrasts such as sheared lithological contacts.…”
Section: Placer Gold Depositsmentioning
confidence: 99%