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    Geological controls on the distribution of arsenic in the Perseverance nickel deposit, Leinster, WA

    Diragitch 2015 Full.pdf (11.66Mb)
    Access Status
    Open access
    Authors
    Diragitch, Alexandre Albiero
    Date
    2014
    Supervisor
    Dr Belinda Godel
    Dr Katy Evans
    Type
    Thesis
    Award
    MPhil
    
    Metadata
    Show full item record
    School
    Western Australian School of Mines, Department of Applied Geology
    URI
    http://hdl.handle.net/20.500.11937/275
    Collection
    • Curtin Theses
    Abstract

    The Perseverance deposit is a deformed ultramafic disseminated Ni-sulphide orebody. Arsenic is found in gersdorffite (NiAsS) and cobaltite (CoAsS). Arsenic-bearing minerals occur within massive sulphide and altered ultramafic disseminated sulphide rocks located at the base of the ultramafic complex. Cobaltite crystallisation temperature ranges from 500°C-550°C while gersdorffite ranges from 250°C-550°C. Arsenic addition occurred prior to regional metamorphism (500 - 550°C) but the arsenic source is obscured by subsequent metamorphic and metasomatic events.

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