Abstract
ABSTRACT A description is given of a detrital grain from the Elsburg A1 Reef, Orange Free State goldfield, which is composed of several other abraded constituents, mostly heavy minerals. There is no question that this grain is a fragment of an older conglomerate, thus indicating extensive reworking and resedimentation processes during the deposition of the Upper Division of the Witwatersrand System.
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Schedule a callMore From: Journal of sedimentary research. Section A, Sedimentary petrology and processes : an international journal of SEPM (Society for Sedimentary Geology)
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