Frictional Properties of the Longmenshan Fault Belt Gouges From WFSD‐3 and Implications for Earthquake Rupture Propagation-Reference-Cited by-同舟云学术

Frictional Properties of the Longmenshan Fault Belt Gouges From WFSD‐3 and Implications for Earthquake Rupture Propagation

Published:2022-05 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:

Kuo Li‐Wei¹²^ORCID,Hung Chien‐Cheng³^ORCID,Li Haibing⁴^ORCID,Aretusini Stefano⁵^ORCID,Chen Jianye⁶^ORCID,Di Toro Giulio⁵⁷^ORCID,Spagnuolo Elena⁵^ORCID,Di Felice Fabio⁵^ORCID,Wang Huan⁴,Si Jialiang⁴^ORCID,Sheu Hwo‐Shuenn⁸^ORCID

Affiliation:

1. Department of Earth Sciences National Central University Taoyuan Taiwan

2. Earthquake‐Disaster & Risk Evaluation and Management Center National Central University Taoyuan Taiwan

3. Earth Simulation Laboratory Department of Earth Sciences Utrecht University Utrecht The Netherlands

4. Key Laboratory of Deep‐Earth Dynamics of Ministry of Natural Resources Institute of Geology Chinese Academy of Geological Sciences Beijing China

5. Instituto Nazionale di Geofisica e Vulcanologia Rome Italy

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

7. Department of Geosciences University of Padua Padua Italy

8. National Synchrotron Radiation Research Centrer Hsinchu Taiwan

Funder

Ministry of Science and Technology, Taiwan

H2020 European Research Council

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/10.1029/2022JB024081

Reference90 articles.

1. Effects of sample preparation on the microstructural signatures of faulting in clay-bearing fault gouge

2. Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone

3. Production of nanoparticles during experimental deformation of smectite and implications for seismic slip

4. Subseismic to Seismic Slip in Smectite Clay Nanofoliation

5. Slow rupture of frictional interfaces

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