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dc.contributor.authorYao, Weihua
dc.contributor.supervisorProf Xian-Hua Li
dc.contributor.supervisorProf. Zheng-Xiang Li
dc.contributor.supervisorProf Bryan Krapez
dc.date.accessioned2017-01-30T10:18:20Z
dc.date.available2017-01-30T10:18:20Z
dc.date.created2014-08-06T03:15:42Z
dc.date.issued2014
dc.identifier.urihttp://hdl.handle.net/20.500.11937/2183
dc.description.abstract

This thesis reports results of a combined sedimentological, stratigraphic, detrital provenance, geochronological, isotopic and geochemical study of the early Palaeozoic South China Block (SCB). It reveals the driving mechanism for the Wuyi–Yunkai orogeny, and the sedimentary and provenance evolution of the lower Palaeozoic Nanhua foreland basin. The thesis further explores possible tectonic interactions between the SCB and northern India during the assembly of Gondwanaland in late Neoproterozoic to early Palaeozoic time.

dc.languageen
dc.publisherCurtin University
dc.titleEvolution of the Lower Palaeozoic Nanhua Foreland Basin and nature of the Wuyi-Yunkai Orogeny, South China
dc.typeThesis
dcterms.educationLevelPhD
curtin.accessStatusOpen access
curtin.facultyFaculty of Science and Engineering, Department of Applied Geology


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