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    Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA

    Meadows H 2017.pdf (74.44Mb)
    Appendix B (Excel).xlsx (103.4Kb)
    Appendix C (Excel).xlsx (66.59Kb)
    Appendix D (Excel).xlsx (431.4Kb)
    Appendix E (Excel).xlsx (537.9Kb)
    Appendix F (Excel).xlsx (27.94Kb)
    Access Status
    Open access
    Authors
    Meadows, Holly Rachael
    Date
    2017
    Supervisor
    Prof. Steven Reddy
    Type
    Thesis
    Award
    PhD
    
    Metadata
    Show full item record
    Faculty
    Science and Engineering
    School
    Department of Applied Geology
    URI
    http://hdl.handle.net/20.500.11937/69391
    Collection
    • Curtin Theses
    Abstract

    The Capricorn Orogen, Western Australia, has a complex history spanning over a billion years. Regional deformation, metamorphism and magmatism has induced migration of ore fluids into local ore deposits. Mineral geochemistry records the chemical environment of ore precipitation and is employed to determine the source of fluids and age of mineral growth. Integration of mineral geochemistry into complex geological systems is used to identify overprinting fluid and deformation events, and evaluate the formation of ore.

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