Crustal architecture beneath the Tibet‐Ordos transition zone, NE Tibet, and the implications for plateau expansion-Reference-Cited by-同舟云学术

Crustal architecture beneath the Tibet‐Ordos transition zone, NE Tibet, and the implications for plateau expansion

Published:2015-12-23 Issue:24 Volume:42 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Guo Xiaoyu¹,Gao Rui¹,Wang Haiyan¹,Li Wenhui¹,Keller G. R.²,Xu Xiao¹,Li Hongqiang¹,Encarnacion John³

Affiliation:

1. State Key Laboratory of Continental Tectonics and Dynamics, Key Laboratory of Earthprobe and Geodynamics, MLR, Institute of Geology Chinese Academy of Geological Sciences Beijing China

2. School of Geology and Geophysics University of Oklahoma Norman Oklahoma USA

3. Department of Earth and Atmospheric Sciences Saint Louis University Saint Louis Missouri USA

Funder

China Geological Survey

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL066668

Reference36 articles.

1. Intracrustal detachment within zones of continental deformation

2. Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements

3. Partitioning of crustal slip between linked, active faults in the eastern Qilian Shan, and evidence for a major seismic gap, the ‘Tianzhu gap', on the western Haiyuan Fault, Gansu (China)

4. Imaging the crustal structure beneath the eastern Tibetan Plateau and implications for the uplift of the Longmen Shan range

5. Irregular western margin of the Yangtze block as a cause of variation in tectonic activity along the Longmen Shan fault zone, eastern Tibet

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