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Early Mesoproterozoic arc magmatism followed by early Neoproterozoic granulite facies metamorphism with a near-isobaric cooling path at Mount Brown, Princess Elizabeth Land, East Antarctica
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文摘

Arc magmatism at Mount Brown took place at ca. 1490–1400 Ma.

Granulite facies metamorphism with an near-isobaric cooling path occurred at ca. 920–900 Ma.

Mount Brown represents the earliest portion of the long-lived Rayner continental arc.

The tectonic evolution of the Rayner orogen might have lasted for ca. 600 Ma.

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