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dc.contributor.authorWang, Chong
dc.contributor.supervisorZheng-Xiang Lien_US
dc.contributor.supervisorSergei Pisarevskiyen_US
dc.date.accessioned2020-07-09T10:13:06Z
dc.date.available2020-07-09T10:13:06Z
dc.date.issued2019en_US
dc.identifier.urihttp://hdl.handle.net/20.500.11937/79966
dc.description.abstract

The North China Craton has abundant Precambrian geological records, but its positions in the two supercontinents are still controversial. Detailed geochronological, geochemical, rock magnetic and paleomagnetic analyses have been carried out. The ~1.24–1.21 Ga magmatism in this craton indicates a LIP caused by a mantle plume. Comparable coeval paleopoles, APWPs and geological histories for the North China and proto-Australian cratons suggest their possible connection during ~1.78–1.32 Ga, but separation after that time.

en_US
dc.publisherCurtin Universityen_US
dc.titlePaleogeographic reconstruction of the North China Craton in the supercontinent Nuna/Columbia: paleomagnetic and geological constraintsen_US
dc.typeThesisen_US
dcterms.educationLevelPhDen_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US
curtin.contributor.orcidWang, Chong [0000-0002-7948-6554]en_US


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