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dc.contributor.authorHartnady, Michael Ian Hay
dc.contributor.supervisorChris Kirklanden_US
dc.date.accessioned2020-02-19T04:55:06Z
dc.date.available2020-02-19T04:55:06Z
dc.date.issued2019en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/77990
dc.description.abstract

This thesis investigates the crustal evolution of the Albany-Fraser Orogen in Western Australia, using U-Pb geochronology, Lu-Hf and oxygen isotope geochemistry of zircon crystals in granitic rocks. The results show that compositional variability of rocks in the region is strongly in uenced by the heterogeneity in the pre-existing crustal substrate. This research therefore demonstrates that mapping spatial Hf isotopic variations in magmatic rocks does not always image deep crustal structure as previously thought.

en_US
dc.publisherCurtin Universityen_US
dc.titleCrustal Evolution of the Albany-Fraser Orogen, Western Australiaen_US
dc.typeThesisen_US
dcterms.educationLevelPhDen_US
curtin.departmentSchool of Earth and Planetary Scienceen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US
curtin.contributor.orcidHartnady, Michael Ian Hay [0000-0001-5297-9925]


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