Late Paleoproterozoic ultrahigh-temperature mafic granulite from the eastern Alxa Block, North China Craton

Precambrian Research(2023)

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摘要
•UHT mafic granulite is identified in the eastern Alxa Block (AB)•Peak metamorphism at 948 – 1048 ℃/11 – 14 kbar following a clockwise P-T path.•A long-lived (1.97 – 1.86 Ga) hot orogen in the eastern AB resulted from subduction.•UHT metamorphism supports the extension of the Khondalite Belt to the eastern AB.
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north china craton,mafic granulite,late paleoproterozoic,eastern alxa block,ultrahigh-temperature
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