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Regional Flow in the Lower Crust and Upper Mantle under the Southeastern Tibetan Plateau
Regional Flow Channel Flow Crustal Deformation Deep and Large Suture
2013/3/7
Seismic tomography reveals an “R-shape” regional flow constrained between the depths of 50 to 80 km in the Southeastern Tibetan Plateau (STP) which demonstrates some of the differences revealed by the...
专著信息
书名
Cenozoic deformation of the Tarim basin and its implications for collisional mountain building in Tibetan plateau and Tian Shan
语种
英文
撰写或编译
作者
Yang Y.,Liu M.
第一作者单位
出版社
v. 21, p. 1059, doi:10...