作者:Huajian YAO
摘要:1.Introduction The subduction and collision between the Indian plate and the Eurasian plate resulted in large-scale deformation of crust and upper mantle material in the Tibetan Plateau and its periphery.Material has been transported from the central plateau to its periphery.
发文机构:Laboratory of Seismology and Physics of Earth’s Interior Anhui Mengcheng National Geophysical Observatory CAS Center for Excellence in Comparative Planetology
关键词:MANTLEEurasianPLATEAU
分类号: P542[天文地球—构造地质学]P315[天文地球—地质学]