supported by the National Natural Science Foundation of China (Grant Nos. 41630207, 41572180);the China Geological Survey Project (Grant No. 12120115027001)
In the northern West Qinling orogen(WQO), granulite-facies metamorphic rocks are recognized within the Qinling Complex. These rocks are composed of amphibole-bearing two-pyroxene granulite and garnet-sillimanite gneis...
supported by the National Natural Science Foundation of China (Grant No. 41430207)
It is generally believed that trondhjemitic rock, an important component of TTG rocks, is the anatectic product of mafic rocks. However, in many TTG gneiss terranes, for instance, the granulite facies terrane in Easte...
Supported by the Chinese Academy of Sciences (Grant No. KZCX2-YW-131);the Chinese Ministry of Science and Technology (Grant No. 2009CB825004);National Natural Science Foundation of China (Grant No. 40673009)
The Dabie-Sulu orogenic belt was formed by the Triassic continental collision between the South China Block and the North China Block. There is a large area of Mesozoic magmatic rocks along this orogenic belt, with em...
supports from the National Natural Science Foundation of China(Grant No.40472113);the National Key Basic Research and Development Program of China(Grant No.2004CB418405);the Foundation of Earthquake Sciences of China Earthquake Administration.
Migmatization in Higher Himalayan Crystallines (HHC) results from anatexis. The widely distributed migmatites in HHC are an important clue to investigate the relationship be- tween anatexis and the origins of Higher H...