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dc.contributor.authorPiechocka, Agnieszka Marta
dc.contributor.supervisorIan Fitzsimonsen_US

SHRIMP U-Pb phosphate geochronology was used to date low- to high-grade metamorphism and leucocratic magmatism associated with Proterozoic intraplate reworking in the Gascoyne Province of Western Australia. The results show that regional metamorphism is probably related to emplacement of magmas rather than to the presence of a thermal lid as widely proposed. Late reactivation of the province, which established the present crustal architecture, was successfully dated using 40Ar/39Ar mica geochronology.

dc.publisherCurtin Universityen_US
dc.titleThe Tectonothermal Evolution of the Gascoyne Province and its Role in Proterozoic Australiaen_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US

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