Metamorphism and P–T evolution of high pressure …
It is widely accepted that the North China Craton (NCC) was finally formed by collision of the Eastern and the Western Blocks along the Trans-North China Orogen (TNCO) at approximately 1.85 Ga.The continent–continent collision along the TNCO was partly defined by metamorphism of high pressure mafic granulites with clockwise P–T …