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Formation of bedded manganese deposits in the Kuruman area, South Africa, is attributed to near-surface enrichment by circulating meteoric waters of a slightly manganiferous limestone zone intercalated in late Precambrian banded ironstones of the upper Griquatown series. Braunite-or cryptomelane-rich ores predominate, but masses of crystalline hausmannite and a few jacobsite boulders are also present.
This record provided courtesy of AGI/GeoRef.
This article has been cited by other articles:
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J. Gutzmer, J. Gutzmer, and N. J. Beukes Asbestiform manjiroite and todorokite from the Kalahari manganese field, South Africa South African Journal of Geology, December 1, 2000; 103(3-4): 163 - 174. [Abstract] [Full Text] [PDF] |
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