A New Tectonic Model for the 1927 M 8.0 Gulang Earthquake on the NE Tibetan Plateau-Reference-Cited by-同舟云学术

A New Tectonic Model for the 1927 M 8.0 Gulang Earthquake on the NE Tibetan Plateau

Published:2020-08-31 Issue:9 Volume:39 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Guo Peng¹^ORCID,Han Zhujun¹^ORCID,Gao Fan¹^ORCID,Zhu Chuanhua²,Gai Hailong³

Affiliation:

1. Key Laboratory of Active Tectonics and Volcano Institute of Geology, China Earthquake Administration Beijing China

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

3. Qinghai Earthquake Agency Xining 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/10.1029/2020TC006064

Reference62 articles.

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2. Surface tracks and slip rate of the fault along the southern margin of the Wuwei basin in the late Quaternary (in Chinese with English abstract);Ai S.;Seismology and Geology,2017

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

4. Visibility of fault strands in exploratory trenches and timing of rupture events

5. Factors affecting the recognition of faults exposed in exploratory trenches;Bonilla M.;US Geological Survey Bulletin,1991

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