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

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

Internet

http://purl.org/au-research/grants/arc/LP130100922
http://hdl.handle.net/20.500.11937/84215

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