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The evolution of a Precambrian arc-related granulite facies gold deposit: Evidence from the Glenburgh deposit, Western Australia

L. Roche,Fawna J. Korhonen,Simon P. Johnson,Michael T.D. Wingate,E. Hancock,Daniel J. Dunkley,Jian-Wei Zi,Birger Rasmussen,Janet R. Muhling, S. Occhipiniti, M. Dunbar, J. Goldsworthy

Precambrian Research（2017）

Cited 8|Views19
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Abstract
•Glenburgh gold deposit hosted in Palaeoproterozoic pelitic migmatites.•Mineralization occurred prior to peak metamorphism, between 2035 and 1991Ma.•Gold mineralization metamorphosed during 1991Ma arc magmatism of the Glenburgh Orogeny.•Peak metamorphism reached 865–885°C and 6.8–7.6kbar.
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Key words
gold deposit,glenburgh deposit,granulite,western australia,arc-related
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