Xin Li
Chinese Academy of Sciences
MagnetotelluricsGeologyGeochemistryCrustDeformation (mechanics)
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Publications 3
#1Jie Tan (China University of Geosciences)H-Index: 1
#2Laiming Zhang (China University of Geosciences)H-Index: 5
Last. Xin Li (CAS: Chinese Academy of Sciences)
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Abstract East China experienced crustal extensions during the Early Cretaceous and the latest Cretaceous-Cenozoic. For a long time,previous studies have recognized a short-lived compressional event between these two extensional regimes during the early Late Cretaceous but not much attention has been paid to it, although it may shed new light on the tectonic evolution of East Asia and the mechanism of the North China Craton Destruction. The Jiaolai Basin, located at the margin of East China, cons...
#1Shuai Xue (CAS: Chinese Academy of Sciences)
#2Denghai Bai (CAS: Chinese Academy of Sciences)
Last. Yongli Yan (CAS: Chinese Academy of Sciences)
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Abstract The northeastern margin of Tibet is the youngest risen part and key area for understanding the growth mechanism of the Tibetan Plateau. New broadband magnetotelluric (MT) data are conducted at the conjunction of the Longmenshan and West Qinling orogenic belts in NE Tibet. The preferred resistivity model obtained using 3-D inversion method shows a dramatic resistivity contrast from the Sichuan Basin (SB) to the West Qinling Orogenic Belt (WQOB). Beneath the SB and Longmenshan Orogenic Be...
#1Xin Li (CAS: Chinese Academy of Sciences)
#2Denghai Bai (CAS: Chinese Academy of Sciences)
Last. Ilya Lozovsky (RAS: Russian Academy of Sciences)
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Abstract It is widely accepted that large-scale strike-slip faults play an important role in accommodating the India‐Eurasia convergence, but the relationships between surface displacements and deep deformation along the faults remain largely uncertain. To address this issue, 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. Although different in details, these two p...