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dc.contributor.authorMitchell, Ruairidh J.
dc.contributor.supervisorTimothy Johnsonen_US
dc.contributor.supervisorChristopher Clarken_US
dc.contributor.supervisorKatharine Evansen_US

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, local equilibrium can persist in metamorphic rocks at >900 °C, should solid phases be chemically and physically isolated from melt.

dc.publisherCurtin Universityen_US
dc.titleUHT metamorphism. Can integrated thermobarometry and geochronology quantify lower crustal processes?en_US
curtin.departmentSchool of Earth and Planetary Sciencesen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US
curtin.contributor.orcidMitchell, Ruairidh J. [0000-0002-4394-5384]en_US

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