financially supported by the National Natural Science Foundation of China(Grant nos.41941004,42172068,42261144673);the Fundamental Research Funds of the Chinese Academy of Geological Sciences(CAGS)(Grant no.JKYZD202321);Geological Survey Programme(Grant no.DD20221810).
The Prydz Belt in East Antarctica underwent extensive reworking during the late Neoprotertozoic–early Paleozoic Pan-African orogeny,which is characterized by granulite facies,clockwise P–T paths,and high dT/dP value...