Magmatic events recorded in granitic gneisses from the Hatu area, eastern East Kunlun Orogen: Response to the assembly of Rodinia

A suite of granitic gneisses has been identified in the Hatu area, eastern segment of the East Kunlun Orogen. Zircon U–Pb dating of granitic gneisses indicates magmatic crystallization at 895.4 ± 9.3 Ma. However, some zircons yield a metamorphic age of 433.8 ± 6.2 Ma. When taken together, these data reveal that the Early Neoproterozoic granites experienced Early Paleozoic metamorphism. The granitic gneisses are characterized by high contents of...