The Cenozoic Evolution of Crustal Shortening and Left‐Lateral Shear in the Central East Kunlun Shan: Implications for the Uplift History of the Tibetan Plateau-Reference-Cited by-同舟云学术

The Cenozoic Evolution of Crustal Shortening and Left‐Lateral Shear in the Central East Kunlun Shan: Implications for the Uplift History of the Tibetan Plateau

Published:2020-08-25 Issue:9 Volume:39 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Staisch Lydia M.¹²^ORCID,Niemi Nathan A.¹^ORCID,Clark Marin K.¹,Chang Hong³^ORCID

Affiliation:

1. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA

2. Now at Geology Minerals Energy and Geophysics Science Center U.S. Geological Survey Portland OR USA

3. Institute of Earth Environment CAS Xi'an China

Funder

European GNSS Agency

Northwest Fisheries Science Center

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006065

Reference150 articles.

1. Late Cenozoic right-lateral strike-slip faulting in southern Tibet

2. Quaternary extension in southern Tibet: Field observations and tectonic implications

3. Evidence for Mesozoic shear along the western Kunlun and Altyn-Tagh fault, northern Tibet (China)

4. The high K2O volcanism of northwestern Tibet: Geochemistry and tectonic implications

5. Kinematic model of active deformation in central Asia

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