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dc.contributor.authorRodrigues Barrote, Vitor
dc.contributor.supervisorNeal McNaughtonen_US
dc.contributor.supervisorSvetlana Tessalinaen_US
dc.date.accessioned2020-10-26T08:26:37Z
dc.date.available2020-10-26T08:26:37Z
dc.date.issued2020en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/81526
dc.description.abstract

4D evolutionary models of ore deposits can be generated by combining multiple geological techniques, including geochronology and isotopic geochemistry, constraining all geological processes within a mineral system. This thesis applies this method to two replacement-type volcanic hosted massive sulphide deposits in the Yilgarn Craton, demonstrating the syn-volcanic nature of the Nimbus deposit, the relationship between the Teutonic Bore camp and the Penzance granite, and proposing tracking of seawater paleo-chemistry for exploration of sedimentary sequences.

en_US
dc.publisherCurtin Universityen_US
dc.title4D Evolution of Replacement-Type VHMS Ore Systems in the Yilgarn Craton, Western Australiaen_US
dc.typeThesisen_US
dcterms.educationLevelPhDen_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US


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