Contrasting fluid systems, chemical gradients and controls on large-tonnage, high-grade Au deposits, Eastern Goldfields Province, Yilgarn Craton, Western Australia
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Walshe, JL
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CSIRO, Div Explorat & Min, Perth, WA, AustraliaCSIRO, Div Explorat & Min, Perth, WA, Australia
Walshe, JL
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Halley, SW
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CSIRO, Div Explorat & Min, Perth, WA, AustraliaCSIRO, Div Explorat & Min, Perth, WA, Australia
Halley, SW
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Hall, GA
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CSIRO, Div Explorat & Min, Perth, WA, AustraliaCSIRO, Div Explorat & Min, Perth, WA, Australia
Hall, GA
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Kitto, P
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CSIRO, Div Explorat & Min, Perth, WA, AustraliaCSIRO, Div Explorat & Min, Perth, WA, Australia
Kitto, P
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[1] CSIRO, Div Explorat & Min, Perth, WA, Australia
Large-tonnage, high-grade gold deposits in the Eastern Goldfields Province result from the interplay of two chemically contrasting fluid systems. Oxidized magmatic hydrothermal fluids (brines and vapours) were sourced from 2665-2650 Ma mafic and syenitic granite-magmas. Chemically contrasting, anhydrous and reduced fluids, composed dominantly of H-2 - H2S +/- CH4, were sourced from the deep crust/mantle. An emerging understanding of the architectural and geodynamic controls on the interaction of the two fluid systems is providing a conceptual framework to aid exploration for major gold resources.