Spatial Changes in Late Quaternary Slip Rates Along the Gyaring Co Fault: Implications for Strain Partitioning and Deformation Modes in Central Tibet-Reference-Cited by-同舟云学术

Spatial Changes in Late Quaternary Slip Rates Along the Gyaring Co Fault: Implications for Strain Partitioning and Deformation Modes in Central Tibet

Published:2021-05 Issue:5 Volume:40 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Wang Duo¹²^ORCID,Chang Hong¹^ORCID,Yin Gongming²,Han Fei²³,Mao Zebin⁴,Du Jinhua⁵,Zheng Wenjun⁶⁷^ORCID,Wang Xulong¹⁶⁷^ORCID

Affiliation:

1. State Key Laboratory of Loess and Quaternary Geology Center for Excellence in Quaternary Science and Global Change Institute of Earth Environment Chinese Academy of Sciences Xi'an China

2. State Key Laboratory of Earthquake Dynamics Institute of Geology China Earthquake Administration Beijing China

3. Yunnan Key Laboratory of Earth System Science Yunnan University Kunming China

4. Yunnan Earthquake Agency Kunming China

5. School of Earth Science and Resources Chang'an University Xi'an China

6. Guangdong Provincial Key Laboratory of Geodynamics and Geohazards School of Earth Sciences and Engineering Sun Yat‐Sen University Guangzhou China

7. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Zhuhai China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006110

Reference87 articles.

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

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

3. The Plio-Quaternary uplift of the Apennine chain: new data from the analysis of topography and river valleys in Central Italy

4. Kinematic model of active deformation in central Asia

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