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...
financial support from the National Natural Science Foundation of China (Grant no.41530209);the Central Public-Interest Scientific Institution Basal Research Fund (Grant no.JYYWF201819);the Chinese Polar Environment Comprehensive Investi-gation&Assessment Programs (Grant no.CHINARE2015-02-05);the Geological Investigation Project of the China Geological Survey (Grant no.12120113019000)
The Grove Mountains are an inland continuation of the Prydz Belt in East Antarctica. Detailed metamorphic petrological and zircon U-Pb geochronological studies are performed on the high-pressure (HP) pelitic granu...