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- W2475432326 abstract "Metals to form the Macraes deposit were derived from the host schists during prograde metamorphism. The metal-bearing metamorphogenic fluid was generated during dehydration of metasediments in the prograde transition from upper greenschist facies to amphibolite facies, at the same time as the Hyde-Macraes Shear Zone was forming retrogressively at shallower levels. Similar processes are occurring in some modern collisional orogens, including the Southern Alps mountains to the north of the Macraes deposit." @default.
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- W2475432326 date "2016-01-01" @default.
- W2475432326 modified "2023-09-27" @default.
- W2475432326 title "Genesis of Macraes as a Metamorphogenic Gold Deposit" @default.
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- W2475432326 doi "https://doi.org/10.1007/978-3-319-35158-2_9" @default.
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