Slip Rate Variation Along the Kunlun Fault (Tibet): Results From New GPS Observations and a Viscoelastic Earthquake‐Cycle Deformation Model-Reference-Cited by-同舟云学术

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Slip Rate Variation Along the Kunlun Fault (Tibet): Results From New GPS Observations and a Viscoelastic Earthquake‐Cycle Deformation Model

Published:2019-03-13 Issue:5 Volume:46 Page:2524-2533
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Diao Faqi¹^ORCID,Xiong Xiong¹,Wang Rongjiang²^ORCID,Walter Thomas R.²,Wang Yuebing³^ORCID,Wang Kai⁴

Affiliation:

1. Hubei Subsurface Multi‐Scale Imaging Key LaboratoryInstitute of Geophysics and Geomatics, China University of Geosciences Wuhan China

2. GFZ German Research Centre for Geosciences Potsdam Germany

3. China Earthquake Networks Center Beijing China

4. State Key Laboratory of Geodesy and Earth's DynamicsInstitute of Geodesy and Geophysics, Chinese Academy of Sciences Wuhan China

Funder

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL081940

Reference44 articles.

1. ITRF2008 plate motion model

2. Displacement-length scaling relationship for faults: data synthesis and discussion

3. Fault locking near Istanbul: indication of earthquake potential from InSAR and GPS observations

4. Paleoseismology and Global Positioning System: Earthquake-cycle effects and geodetic versus geologic fault slip rates in the Eastern California shear zone

5. Dissipation of fast strike-slip faulting within and beyond northeastern Tibet

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