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This strata-bound deposit is interpreted as 'a tectonically metamorphosed, remobilized ore deposit.' A sedimentary exhalative origin is postulated for the primary concentration.
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This article has been cited by other articles:
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J. K. Talluri, J. K. Talluri, H. S. Pandalai, and G. N. Jadhav Fluid Chemistry and Depositional Mechanism of the Epigenetic, Discordant Ores of the Proterozoic, Carbonate-Hosted, Zawarmala Pb-Zn Deposit, Udaipur District, India Economic Geology, November 1, 2000; 95(7): 1505 - 1525. [Abstract] [Full Text] [PDF] |
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