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dc.contributor.authorMeadows, Holly Rachael
dc.contributor.supervisorProf. Steven Reddyen_US
dc.date.accessioned2018-08-03T02:26:30Z
dc.date.available2018-08-03T02:26:30Z
dc.date.issued2017
dc.identifier.urihttp://hdl.handle.net/20.500.11937/69391
dc.description.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.

en_US
dc.publisherCurtin Universityen_US
dc.titleMineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WAen_US
dc.typeThesisen_US
dcterms.educationLevelPhDen_US
curtin.departmentDepartment of Applied Geologyen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US


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