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dc.contributor.authorWu, Yafei
dc.contributor.supervisorKaty Evansen_US
dc.date.accessioned2020-03-04T07:53:00Z
dc.date.available2020-03-04T07:53:00Z
dc.date.issued2019en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/78110
dc.description.abstract

Yafei Wu’s PhD project has explored different ore-forming aspects of a world-class Chinese orogenic gold deposit. The results show that orogenic gold could be sourced from either metamorphism or magmatism. Silica has an important role in gold transport. Gold zoning in pyrite records both fluid conditions and local kinetics. Gold significantly redistributes during pyrite replacement. The knowledge gained increases our understanding of the genesis of orogenic gold widely distributed in Australia, New Zealand and worldwide.

en_US
dc.publisherCurtin Universityen_US
dc.titleGold Source and Deportment in the Daqiao Epizonal Orogenic Gold Deposit, Chinaen_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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