Gold grades and iron content of sphalerite: relationship of possible genetic significance from Hellyer volcanogenic massive-sulphide deposit of northwest Tasmania, Australia

The Institute of Materials, Minerals and Mining
A. R. Ramsden K. M. Kinealy D. H. French
Organization:
The Institute of Materials, Minerals and Mining
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3
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1967 KB
Publication Date:
Jan 1, 1991

Abstract

A negative correlation exists between sphalerite composition and gold content when gold is transported as Au(HS)2(-); however, there are spatial and temporal differences within a single deposit. A previous model for the formation of volcanogenic massive-sulphide deposits within thermally intensifying and waning hydrothermal sytems in much the same way as is observed around modern sea-floor vents is supported. The results also emphasise that recognition of the mechanisms of gold transport in ancient deposits depends critically on an understanding of their mineralogy and stratigraphy
Citation

APA: A. R. Ramsden K. M. Kinealy D. H. French  (1991)  Gold grades and iron content of sphalerite: relationship of possible genetic significance from Hellyer volcanogenic massive-sulphide deposit of northwest Tasmania, Australia

MLA: A. R. Ramsden K. M. Kinealy D. H. French Gold grades and iron content of sphalerite: relationship of possible genetic significance from Hellyer volcanogenic massive-sulphide deposit of northwest Tasmania, Australia. The Institute of Materials, Minerals and Mining, 1991.

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