Kinematics of the Tengchong Terrane in SE Tibet from the late Eocene to early Miocene:Insights from coeval mid-crustal detachments and strike-slip shear zones
It is generally believed that the extrusion of SE Tibet was bounded by the dextral Gaoligong and the sinistral Ailaoshan-Red River strike-slip shear zones from the Oligocene to early Miocene.This study integrates field mapping,structural analysis and geochronology in western Yunnan (China),where foliated Precambrian basement rocks and late Cretaceous to early Eocene plutons are exposed to the west of the Gaoligong shear zone.
Zhiqin Xu Qin Wang Zhihui Cai Hanwen Dong Huaqi Li Xijie Chen Xiangdong Duan Hui Cao Jing Li Jean-Pierre Burg
State Key Laboratory of Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of G State Key Laboratory for Mineral Deposits Research,Department of Earth Sciences,Nanjing University N Geological Survey of Yunnan Province Kunming 650051 Geologisches Institute,ETH Zurich Zurich 8092
国内会议
北京
英文
3247-3247
2015-10-11(万方平台首次上网日期,不代表论文的发表时间)