GPS Determined Asymmetric Deformation Across Central Altyn Tagh Fault Reveals Rheological Structure of Northern Tibet-Reference-Cited by-同舟云学术

GPS Determined Asymmetric Deformation Across Central Altyn Tagh Fault Reveals Rheological Structure of Northern Tibet

Published:2022-09 Issue:9 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Ge Wei‐Peng¹²^ORCID,Shen Zheng‐Kang³⁴^ORCID,Molnar Peter⁵^ORCID,Wang Min¹^ORCID,Zhang Pei‐Zhen⁶^ORCID,Yuan Dao‐Yang⁷

Affiliation:

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

2. Now at Gansu Lanzhou National Geophysical Observation and Research Station Lanzhou Institute of Seismology China Earthquake Administration Lanzhou China

3. Department of Geophysics School of Earth and Space Science Peking University Beijing China

4. Department of Earth, Planetary, and Space Sciences University of California Los Angeles CA USA

5. Department of Geological Sciences and Cooperative Institute for Research in Environmental Sciences (CIRES) University of Colorado Boulder CO USA

6. School of Earth Sciences and Engineering Sun Yat‐Sen University Guangzhou China

7. School of Earth Sciences Lanzhou University Lanzhou China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022JB024216

Reference110 articles.

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3. Geodetic evidence for a low slip rate in the Altyn Tagh fault system

4. Spatial variations of flexure parameters over the Tibet–Quinghai plateau

5. Convection beneath young oceanic lithosphere: Implications for thermal structure and gravity

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