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P-T-t evolution of Neoarchaean to Paleoproterozoic pelitic granulites from the Jidong terrane, eastern North China Craton
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文摘
Clockwise P-T path was retrieved from the Jidong pelitic granulites. SIMS U-Pb dating of metamorphic zircons suggests that the peak or near peak metamorphism took place at ca. 2.5 Ga. A subduction–collision event might occur during late Neoarchean to early Palaeoproterozoic in the eastern North China Craton.

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