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Yun Chen
Chinese Academy of Sciences
59Publications
18H-index
1,120Citations
Publications 59
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#1Chenglong Wu (CAS: Chinese Academy of Sciences)H-Index: 5
#2Xiaobo Tian (CAS: Chinese Academy of Sciences)H-Index: 18
Last.Jiwen Teng (CAS: Chinese Academy of Sciences)H-Index: 27
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#1Yun Chen (CAS: Chinese Academy of Sciences)H-Index: 18
#2Tian Cui (CAS: Chinese Academy of Sciences)
Last.Jiwen Teng (CAS: Chinese Academy of Sciences)H-Index: 27
view all 11 authors...
Abstract The East China Continental Margin (ECCM) is an exemplified natural laboratory not only for studying the origin and evolution of trench-arc-basin system, but also for investigating the deformation mechanism within continent and its margins. For a better understanding on the structure and evolution of the ECCM, a NW–SE trending onshore-offshore seismic profile was recently carried out there using controlled source wide-angle and passive broadband seismic experiments in combination. This 1...
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#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...
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#1Lin Chen (CAS: Chinese Academy of Sciences)H-Index: 10
#2Xiaodong Song (UIUC: University of Illinois at Urbana–Champaign)H-Index: 28
Last.Yun Chen (CAS: Chinese Academy of Sciences)H-Index: 18
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Abstract Mid-crustal melting is widely documented under orogenic plateaus. However, the mechanism for its generation and its role in the evolution of orogenic plateaus remain poorly understood. Here we investigate the physical controls and consequences of crustal melting in plateau evolution using 3-D thermo-mechanical modeling method. Our simulations demonstrate that the convergence causes orogenic crust to have more upper crustal compositions and more radiogenic elements. The persistent radioa...
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#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...
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#1Qi-Fu Chen (CAS: Chinese Academy of Sciences)
#2Yinshuang Ai (CAS: Chinese Academy of Sciences)
Last.Yun Chen (CAS: Chinese Academy of Sciences)H-Index: 18
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The Changbaishan volcano is an active and considerably hazardous volcano located on the border of China and North Korea. This paper summarizes a series of geophysical surveys as well as seismological and volcano-observational networks around the Changbaishan volcanic area. We characterize deep structures related to the Changbaishan volcanic area. The prominent low-velocity anomalies and low-resistance bodies associated with the magma system under the Changbaishan volcano were detected in the cru...
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#1Chenglong Wu (CAS: Chinese Academy of Sciences)H-Index: 5
#2Xiaobo Tian (CAS: Chinese Academy of Sciences)H-Index: 18
Last.Jiwen Teng (CAS: Chinese Academy of Sciences)H-Index: 27
view all 11 authors...
Abstract Shear-wave splitting provides insight into geodynamic processes such as lithospheric deformation and upper mantle flow. This study presents shear wave splitting parameters determined from XKS (SKS, SKKS and PKS) and Pms phases (from receiver functions) recorded by the 2D seismic array, SANDWICH, deployed in central Tibet from November 2013 to April 2016. The XKS splitting measurements show a generally strong anisotropy with an average of 1.3 s, that even includes 17 stations with delay ...
1 CitationsSource
#1W. D. Li (CAS: Chinese Academy of Sciences)H-Index: 127
#2Yun Chen (CAS: Chinese Academy of Sciences)H-Index: 18
Last.Bihong Fu (CAS: Chinese Academy of Sciences)H-Index: 4
view all 6 authors...
2 CitationsSource
#1Xi Zhang (CAS: Chinese Academy of Sciences)H-Index: 13
#2Peng Wang (CEA: China Earthquake Administration)H-Index: 6
Last.Jiwen Teng (CAS: Chinese Academy of Sciences)H-Index: 27
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#1Wei Li (CAS: Chinese Academy of Sciences)H-Index: 5
#2Yun Chen (CAS: Chinese Academy of Sciences)H-Index: 18
Last.Bihong Fu (CAS: Chinese Academy of Sciences)H-Index: 4
view all 7 authors...
Abstract The Pamir has experienced more intense deformation and shortening than Tibet, although it has a similar history of terrane accretion. Subduction as a primary way to accommodate lithospheric shortening beneath the Pamir has induced the intermediate-depth seismicity, which is rare in Tibet. Here we construct a 3D S-wave velocity model of the lithosphere beneath the Pamir by surface wave tomography using data of the TIPAGE (Tien Shan–Pamir Geodynamic program) and other seismic networks in ...
7 CitationsSource
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