【摘 要】
：
In addition to the apparent surficial deformation associated with the sinistral strike-slip Kunlun fault (KF),INDEPTH Phases Ⅲ and Ⅳ magnetotelluric results reveal that more complex deformation proces
【机 构】
：
Dublin Institute for Advanced Studies,5 Merrion Square,Dublin 2,Ireland
【出 处】
：
The International Conference on Continental Dynamics(2014年大陆
论文部分内容阅读
In addition to the apparent surficial deformation associated with the sinistral strike-slip Kunlun fault (KF),INDEPTH Phases Ⅲ and Ⅳ magnetotelluric results reveal that more complex deformation processes are occurring at midcrustal depths in northern Tibet.Two- dimensional (2D) anisotropic and 3D isotropic magnetotelluric modelling/inversions have been applied to data from the INDEPTH Ⅲ 600 and INDEPTH Ⅳ 6000 transects crossing the Kunlun Fault,one of the major northern tectonic boundaries of the atypical topography of the Tibetan plateau.
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