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Density and magnetic intensity of the crust and uppermost mantle across the northern margin of the Tibetan Plateau
Zhao, JM (Zhao, Junmeng)1,2; Shah, STH (Shah, Syed Tallataf Hussain)2,3; Zhang, H (Zhang, Heng)2; Zhang, XK (Zhang, Xiankang)4; Yao, CL (Yao, Changli)5; Li, YS (Li, Yishi)6; Liu, HB (Liu, Hongbing)1,2; Xu, Q (Xu, Qiang)1,2; Deng, G (Deng, Gong)2; Hu, ZG (Hu, Zhaoguo)7; Bhatti, ZI (Bhatti, Zahid Imran)2; Zhao, JM
Source PublicationPHYSICS OF THE EARTH AND PLANETARY INTERIORS
2017
Volume265Issue:0Pages:15-22
DOI10.1016/j.pepi.2017.02.003
AbstractRecently, we have processed the gravitational and geomagnetic data from a geophysical survey along a profile (Baicheng to Da Qaidam) which crosses the northern and eastern Tarim Basin, the Altyn Tagh Mountains, and the Qaidam Basin, respectively. Based on the P- and S-wave velocities (Zhao et al., 2006), both the density and magnetic intensity of the crust and uppermost mantle were determined by using a joint inversion of gravity versus geomagnetism. Our new results at the northern margin of the Tibetan Plateau reflect different crustal structures beneath Tarim basin and Qaidam basin, and these two basins may be produced by different terranes. In addition, strong deformation has occurred in the basement and interior of the Qaidam Basin during the tectonic evolution. (C) 2017 Elsevier B.V. All rights reserved.
Subject Area地球物理学
WOS IDWOS:000397695000002
Language英语
Indexed BySCI
KeywordALTYN-TAGH FAULT CONTINENTAL COLLISION TECTONIC IMPLICATIONS GEOLOGIC EVOLUTION CENOZOIC VOLCANISM VELOCITY STRUCTURE DEEP-STRUCTURE QAIDAM BASIN DEFORMATION SYSTEM
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics ; Geochemistry & Geophysics
Cooperation Status国际
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Cited Times:4[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/8309
Collection图书馆
Corresponding AuthorZhao, JM
Affiliation1.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China.
2.Chinese Acad Sci, Key Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China.
3.COMSATS Inst Informat Technol, Abbottabad, Pakistan.
4.China Earthquake Adm, Ctr Geophys Explorat, Zhengzhou 450002, Peoples R China.
5.China Univ Geosci, Beijing 100083, Peoples R China.
6.China Earthquake Adm, Beijing 100036, Peoples R China.
7.China Cent Bur Met & Geol, Shandong Zhengyuan Inst Geol Explorat, Jinan 250000, Peoples R China.
Recommended Citation
GB/T 7714
Zhao, JM ,Shah, STH ,Zhang, H ,et al. Density and magnetic intensity of the crust and uppermost mantle across the northern margin of the Tibetan Plateau[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS,2017,265(0):15-22.
APA Zhao, JM .,Shah, STH .,Zhang, H .,Zhang, XK .,Yao, CL .,...&Zhao, JM.(2017).Density and magnetic intensity of the crust and uppermost mantle across the northern margin of the Tibetan Plateau.PHYSICS OF THE EARTH AND PLANETARY INTERIORS,265(0),15-22.
MLA Zhao, JM ,et al."Density and magnetic intensity of the crust and uppermost mantle across the northern margin of the Tibetan Plateau".PHYSICS OF THE EARTH AND PLANETARY INTERIORS 265.0(2017):15-22.
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