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Copper and subordinate amounts of cobalt occur as disseminations of sulfide grains in dolomite and in quartz-dolomite veins in folded, slightly metamorphosed Precambrian dolomitic rocks in the Fungurume area, Katanga, Belgian Congo. Evidence suggesting an early epigenetic origin for the mineralization is discussed. An introduction, by H. Schuiling, outlines the geologic setting of the ore deposits.
This record provided courtesy of AGI/GeoRef.
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M. Wendorff and M. Wendorff Stratigraphy of the Fungurume Group - evolving foreland basin succession in the Lufilian fold-thrust belt, Neoproterozoic-Lower Palaeozoic, Democratic Republic of Congo South African Journal of Geology, March 1, 2003; 106(1): 17 - 34. [Abstract] [Full Text] [PDF]
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