The Mangaroon Orogeny: Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton

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The Mangaroon Orogeny: Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton

The Capricorn Orogen records nearly one billion years of intraplate orogenesis within the West Australian Craton, although the processes responsible for this protracted, punctuated reworking remain unclear. Of the major tectonic events that affected the region, the 1680–1620 Ma Mangaroon Orogeny is...

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Bibliographic Details
Main Authors:	Piechocka, Agnieszka, Zi, Jianwei, Gregory, Courtney, Sheppard, Steve, Korhonen, F.J., Fitzsimons, Ian, Johnson, Tim, Rasmussen, Birger
Format:	Journal Article
Language:	English
Published:	ELSEVIER 2019
Subjects:	Science & Technology Physical Sciences Geosciences, Multidisciplinary Geology Intraplate orogeny U-Pb geochronology Monazite Xenotime LPHT metamorphism Proterozoic U-PB CAPRICORN OROGEN ARUNTA-INLIER GEODYNAMIC EVOLUTION INTRAPLATE REWORKING FACIES METAMORPHISM MONAZITE GEOCHRONOLOGY TEMPERATURE SATURATION
Online Access:	http://purl.org/au-research/grants/arc/LP130100922 http://hdl.handle.net/20.500.11937/84215

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