UHT metamorphism. Can integrated thermobarometry and geochronology quantify lower crustal processes?

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UHT metamorphism. Can integrated thermobarometry and geochronology quantify lower crustal processes?

The Eastern Ghats Province cooled at 0.34 ± 0.09 °C/Ma from ~6.8–8.3 kbar, 1000°C between c. 1000–880 Ma, and was reheated to >900 °C at c. 550–500 Ma. This reflects a period of burial in the deep crust of an orogen with high radiogenic heat production and slow rates of erosion. Additionally, loc...

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Bibliographic Details
Main Author:	Mitchell, Ruairidh J.
Format:	Thesis
Published:	Curtin University 2019
Online Access:	http://hdl.handle.net/20.500.11937/80609

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