1976
DOI: 10.2113/gsecongeo.71.1.139
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Gold, base metals, and diamonds in Botswana

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Cited by 20 publications
(2 citation statements)
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“…The Selebi‐Phikwe Ni‐Cu sulfide deposit is an Archean stratabound massive sulfide deposit associated with amphibolite host rocks, with pyrrhotite (Fe 1−x S), chalcopyrite (CuFeS 2 ), and pentlandite [(Fe, Ni) 9 S 8 ] being the most important ore minerals (Baldock et al., 1976 ; Wakefield, 1976 ). The mining of sulfide Ni‐Cu‐Co ores started in 1973.…”
Section: Methodsmentioning
confidence: 99%
“…The Selebi‐Phikwe Ni‐Cu sulfide deposit is an Archean stratabound massive sulfide deposit associated with amphibolite host rocks, with pyrrhotite (Fe 1−x S), chalcopyrite (CuFeS 2 ), and pentlandite [(Fe, Ni) 9 S 8 ] being the most important ore minerals (Baldock et al., 1976 ; Wakefield, 1976 ). The mining of sulfide Ni‐Cu‐Co ores started in 1973.…”
Section: Methodsmentioning
confidence: 99%
“…porém questionou alguns desses dados, af¡rmando que scheelita e uraninita eram provenientes de gran¡tos cortados pelo Rio lndus. SegundoBardet (1974), na África Ocidental a ilmenita magnesiana e o piropo (grãos inferiores a 1 mm) em clima tropical não são encontrados a mais que 1 km do kimberl¡to fonte, enquanto em clima de monção ambos não podem ser recuperados além de 13 km de sua fonte Baldock et al (1976),. no entanto, mencionam um halo de dispersão com cerca de 300 km para os minerais indicadores proven¡entes do campo kimberlítico de Orapa, no Botswana.…”
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