supported by the National Basic Research Program of China(2009CB825002);the National Natural Science Foundation of China(40773013 and 91014007)
Systematical studies of post-collisional igneous rocks in the Dabie orogen suggest that the thickened mafic lower crust of the orogen was partially melted to form low-Mg#adakitic rocks at 143–131 Ma.Delamination and ...
国家自然科学基金项目(40773013);教育部博士点新教师基金项目(20070491518);GPMR开放基金项目(GPMR0742);美国National Science Foundation(EAR-0838227);阿肯色州Arkansas Space Grant Consortium(SW19002)联合资助
supported by the National Natural Science Foundation of China (40773013)
C-type adakites have been commonly considered as a result of partial melting of the mafic lower continental crust (LCC) at high pressure, as supported by high P-T experiments on hydrous basalts. However, because the m...
the Chinese Academy of Sciences (Grant No. kzcx2-yw-131);the National Natural Science Foundation of China (Grant Nos. 40572035, 40634023 and40773013).
Although tectonic models were presented for exhumation of ultrahigh-pressure (UHP) metamorphic rocks during the continental collision, there is increasing evidence for the decoupling between crustal slices at various ...