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• W2045525089 abstract "Abstract Three types of greyschist (fissile, dark grey, and light grey thickly segregated types) and subordinate greenschist make up most of the Otago Schist hosting the Moke Creek sulphide deposit. Greyschist in the study area is mostly of Torlesse Terrane affinity, with the exception of a sliver of Caples Terrane affinity schist preserved in the footwall of the Moonlight Fault. The three greyschist types are geochemically indistinguishable; however, the former two types contain higher contents of graphite, which may explain their darker field appearance. The greenschists are shown to represent metamorphosed MORB and within‐plate basalts. Schist immediately hosting the Moke Creek sulphide deposit consists of both muscovite‐rich and subordinate epidote‐rich varieties. The former variety contains up to 6.4 wt% K2O, whereas the epidote‐rich variety is depleted in K2O but contains >5 wt% CaO. It is suggested that sericitisation during hydrothermal alteration associated with sulphide deposition produced the m..." @default.
• W2045525089 created "2016-06-24" @default.
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• W2045525089 date "2002-06-01" @default.
• W2045525089 modified "2023-09-26" @default.
• W2045525089 title "Lithology, geochemistry, and structure of Moke Creek sulphide deposit host rocks, Otago Schist, New Zealand" @default.
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• W2045525089 doi "https://doi.org/10.1080/00288306.2002.9514968" @default.
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