Abstract
Transitions from pyrrhotite–magnetite- to pyrite–magnetite- and pyrite–hematite-bearing assemblages in metasedimentary rocks in the Kambalda-St. Ives goldfield have been shown to be spatially associated with economic gold grades. Fluid mixing, fluid–rock interaction and phase separation have been proposed previously as causes for this association. Textural, mineralogical and isotopic evidence is reviewed, and thermodynamic calculations are used to investigate the mineralogical consequences of progressive fluid–rock interaction in interflow metasediments. Fluid–rock interactions in response to fluid infiltration and/or bulk composition variation are plausible mechanisms for production of the observed features.
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Acknowledgements
This work was supported by a Curtin University Research and Teaching Fellowship and by CSIRO (Commonwealth Scientific and Industrial Research Organisation) Exploration and Mining. Neil Phillips and Roger Powell are thanked for helpful discussions. Frank Bierlein and an anonymous reviewer are thanked for perceptive reviews that improved the paper, and Patrick Williams is thanked for editorial support.
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Evans, K.A. A test of the viability of fluid–wall rock interaction mechanisms for changes in opaque phase assemblage in metasedimentary rocks in the Kambalda-St. Ives goldfield, Western Australia. Miner Deposita 45, 207–213 (2010). https://doi.org/10.1007/s00126-009-0260-4
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DOI: https://doi.org/10.1007/s00126-009-0260-4