The assembly of Rodinia: The correlation of early Neoproterozoic (ca. 900 Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB)
Garnet schists from the South Beishan Orogen experienced high-grade metamorphism at ca. 900 Ma. ~900 Ma metamorphism is coeval with extensive continental arc formation in the SBOB and CTA. The SBOB and CTA occupied in the periphery of the Rodinia during the final assembly stage.