Late Quaternary Slip Rate of the Zihong Shan Branch and Its Implications for Strain Partitioning Along the Haiyuan Fault, Northeastern Tibetan Plateau-Reference-Cited by-同舟云学术

Late Quaternary Slip Rate of the Zihong Shan Branch and Its Implications for Strain Partitioning Along the Haiyuan Fault, Northeastern Tibetan Plateau

Published:2022-04-27 Issue:5 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Yao Wenqian¹^ORCID,Liu‐Zeng Jing¹²^ORCID,Klinger Yann³^ORCID,Wang Zijun¹^ORCID,Shao Yanxiu¹,Han Longfei¹^ORCID,Wang Wei²^ORCID,Zhang Jinyu²,Liu Zhijun¹

Affiliation:

1. School of Earth System Science Institute of Surface‐Earth System Science Tianjin University Tianjin China

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

3. Université de Paris Institut de Physique du Globe de Paris UMR 7154 CNRS Paris France

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/10.1029/2021JB023162

Reference100 articles.

1. Partitioning of oblique convergence coupled to the fault locking behavior of fold-and-thrust belts: Evidence from the Qilian Shan, northeastern Tibetan Plateau

2. Explicit treatment of inheritance in dating depositional surfaces using in situ 10Be and 26Al

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4. Codependent histories of the San Andreas and San Jacinto fault zones from inversion of fault displacement rates

5. Dynamic Slip Transfer from the Denali to Totschunda Faults, Alaska: Testing Theory for Fault Branching

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