Evolution of the Chilka Lake granulite complex, northern Eastern Ghats Belt, India: First evidence of ~ 780 Ma decompression of the deep crust and its implication on the India-Antarctica correlation
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文摘

Chilka Lake granulites evolved through a possible clockwise PT path.

The strong ca. 780 Ma orogeny resulted decompression of the lower crust.

Domain 3 of Eastern Ghats Belt was probably attached to Prydz Bay of east Antarctica.

The present study documents the assembly and breakup of Rodinia in the India–Antarctica sector.

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