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dc.contributor.authorDayong, Vivian Anak
dc.contributor.supervisorChua Han Bingen_US
dc.date.accessioned2019-04-09T01:21:58Z
dc.date.available2019-04-09T01:21:58Z
dc.date.issued2018en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/75247
dc.description.abstract

A study is proposed on the clastic sedimentary rocks of the Tukau Formation in the North-West Borneo using combined methods (i.e. geochemistry and petrography) to infer the provenance, tectonic setting and paleoweathering. Generally, Tukau sandstones are classified into quartz arenites , sublitharenites, litharenites, wacke and shale. Source rock is derived from the sedimentary to meta-sedimentary rocks dominated source with minor contribution from granitoids and ultramafic rocks. Tectonically, the Tukau Formation sedimentary rocks were deposited in a passive margin with minor extent towards active margin boundary.

en_US
dc.publisherCurtin Universityen_US
dc.titleGeochemistry and Mineralogy of Clastic Sediments of Tukau Formation: Implications on Provenance and Tectonic Settingen_US
dc.typeThesisen_US
dcterms.educationLevelMPhilen_US
curtin.departmentCurtin Malaysiaen_US
curtin.accessStatusOpen accessen_US
curtin.facultyCurtin Malaysiaen_US


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