Discovery, geology and genesis of copper—cobalt mineralisation at Chambishi Southeast prospect, Zambia
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Cited by (10)
Sequence and carbon isotopic stratigraphy of the Neoproterozoic Roan Group strata of the Zambian copperbelt
2011, Precambrian ResearchCitation Excerpt :The variation in δ13C values was between sample pairs was between 1 and 1.3‰ (Bull, unpublished data), an order of magnitude less than the >10‰ isotopic excursions considered significant for correlation purposes. Chambishi Southeast is a blind occurrence of Cu-Co mineralization hosted by the Copperbelt Orebody Member on the north-eastern margin of the Chambishi Basin, 5 km southeast of the Chambishi mine (Fleischer, 1984; Fig. 2). A 5 km long, east-west trending fence of holes from the area has been examined to determine the sedimentary facies architecture of the “classical” (i.e. Copperbelt Orebody Member present) ZCB stratigraphy (Fig. 4a).
Metallogenesis of the Nkana copper-cobalt South Orebody, Zambia
2009, Journal of African Earth SciencesThe nature of early basinal fluids in the Zambian Copperbelt: A case study from the Chambishi deposit
2005, Journal of African Earth SciencesOre-related diagenesis-An encyclopedic review
1988, Developments in Sedimentology
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