Temperature and Fluid Pressurization Effects on Frictional Stability of Shale Faults Reactivated by Hydraulic Fracturing in the Changning Block, Southwest China-Reference-Cited by-同舟云学术

Temperature and Fluid Pressurization Effects on Frictional Stability of Shale Faults Reactivated by Hydraulic Fracturing in the Changning Block, Southwest China

Published:2020-08 Issue:8 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

An Mengke¹²,Zhang Fengshou¹²^ORCID,Chen Zhaowei³,Elsworth Derek⁴⁵^ORCID,Zhang Lianyang⁶

Affiliation:

1. Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education Tongji University Shanghai China

2. Department of Geotechnical Engineering, College of Civil Engineering Tongji University Shanghai China

3. CNPC Engineering Technology R&D Company Limited Beijing China

4. Department of Energy and Mineral Engineering, EMS Energy Institute and G3 Center The Pennsylvania State University University Park PA USA

5. Department of Geosciences The Pennsylvania State University University Park PA USA

6. Department of Civil and Architectural Engineering and Mechanics University of Arizona Tucson AZ USA

Funder

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of 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/10.1029/2020JB019584

Reference66 articles.

1. Effect of slick-water fracturing fluid on the frictional properties of shale reservoir rock gouges

2. Delayed Weakening and Reactivation of Rate‐and‐State Faults Driven by Pressure Changes Due to Fluid Injection

3. Fault activation by hydraulic fracturing in western Canada

4. Fluid-induced aseismic fault slip outpaces pore-fluid migration

5. Frictional properties of exhumed fault gouges in DFDP-1 cores, Alpine Fault, New Zealand

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