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Mean composition of Biwabik, weighted for area and thickness of individual units, shows more Fe and CaO, less SiO 2 , than older estimates. Uniformity in composition of composite samples used for calculation is considered to indicate uniformity of chemical and physical environment in source and depositional areas.
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B. Buhn and I. G. Stanistreet Insight into the enigma of Neoproterozoic manganese and iron formations from the perspective of supercontinental break-up and glaciation Geological Society, London, Special Publications, January 1, 1997; 119(1): 81 - 90. [Abstract] [PDF] |
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