Denghai Bai
Chinese Academy of Sciences
5 Papers
Denghai Bai is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Crust & Lithosphere. The author has an hindex of 3, co-authored 5 publications.
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Papers
A plume-modified lithospheric barrier to the southeastward flow of partially molten Tibetan crust inferred from magnetotelluric data
TL;DR: In this article, the authors used long-period magnetotelluric (MT) data to obtain a continuous image of the lithospheric electrical conductivity structure across the southeastern Tibetan Plateau margin, where longwavelength crustal thickening and surface uplift have been attributed to the influx of weak crustal material from Tibet into the adjacent Yangtze Block.
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Electrical resistivity structure of the Xiaojiang strike-slip fault system (SW China) and its tectonic implications
Xin Li,Denghai Bai,Xiaobing Ma,Yun Chen,Ivan M. Varentsov,Guoqiang Xue,Shuai Xue,Ilya Lozovsky +7 more
TL;DR: In this paper, new magnetotelluric (MT) images were obtained along two profiles across the Xiaojiang strike-slip fault system (XJFS), one of the most tectonically active areas in southwest China.
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Deep electrical resistivity structure across the Gyaring Co Fault in Central Tibet revealed by magnetotelluric data and its implication
Shuai Xue,Shuai Xue,Yun Chen,Hongda Liang,Xin Li,Xiaofeng Liang,Xiaobing Ma,Zhanwu Lu,Denghai Bai,Yongli Yan +9 more
TL;DR: In this paper, an east-west trending magnetotelluric array has been operated across the Gyaring Co Fault (GCF) at the northern end of the Xainza-Dingjye Rift (XDR) in Lhasa block.
20
Contrasting crustal deformation mechanisms in the Longmenshan and West Qinling orogenic belts, NE Tibet, revealed by magnetotelluric data
TL;DR: In this paper, the authors used 3-D inversion method to obtain the preferred resistivity model obtained using broadband magnetotelluric (MT) data at the conjunction of the Longmenshan and West Qinling orogenic belts in NE Tibet.
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