An ancient unconformity event is identified within the granulite-facies province of North China, which is marked by the boundary between the overlying khondalit
Detailed REE geochemical studies of the Xingzi Group metasedimentary rocks at Lushan and rock-forming minerals such as garnet have been conducted and the result
Nd-Sr isotopic compositions of 12 Mesozoic granitoids from Jiangxi Province have been reported. They show loe-ε_(ND)(-13.8—- 8.3), high-l_(sr)(0.71069—0.739