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An overview is presented for the formation and evolution of Precambrian continental lithosphere in South China. This is primarily based on an integrated study of zircon U–Pb ages and Lu–Hf isotopes in crustal rocks, with additional constraints from Re–Os isotopes in mantle-derived rocks. Available Re–Os isotope data on xenolith peridotites suggest that the oldest subcontinental lithospheric mantle...
The continental crust of China is a mosaic of cratonic blocks and orogenic belts, containing small cratons and terranes with various tectonic settings. They have diverse origins and complex histories of amalgamation, and often suffered repeated reworking after multiple episodes of amalgamation. In the last three decades, extensive geological, geochemical and geophysical investigations have been carried...
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