The Potential for Low‐Grade Metamorphism to Facilitate Fault Instability in a Geothermal Reservoir-Reference-Cited by-同舟云学术

The Potential for Low‐Grade Metamorphism to Facilitate Fault Instability in a Geothermal Reservoir

Published:2021-06-08 Issue:11 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

An Mengke¹²,Zhang Fengshou¹²^ORCID,Min Ki‐Bok³^ORCID,Elsworth Derek⁴⁵^ORCID,Marone Chris⁵⁶^ORCID,He Changrong⁷^ORCID

Affiliation:

1. Department of Geotechnical Engineering College of Civil Engineering Tongji University Shanghai China

2. Key Laboratory of Geotechnical & Underground Engineering of Ministry of Education Tongji University Shanghai China

3. Department of Energy Resources Engineering and Research Institute of Energy and Resources College of Engineering Seoul National University Seoul Republic of Korea

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

5. Department of Geosciences the Pennsylvania State University PA USA

6. Dipartimento di Scienze della Terra La Sapienza Università di Roma Italy

7. State Key Laboratory of Earthquake Dynamics Insitute of Geology, China Earthquake Adminstration Beijing China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL093552

Reference53 articles.

1. Phase relations among greenschist, epidote‐amphibolite, and amphibolite in a basaltic system;Apted M. J.;American Journal of Science,1983

2. Levelized costs of electricity and direct-use heat from Enhanced Geothermal Systems

3. Epidote in Geothermal Systems

4. Fault stability inferred from granite sliding experiments at hydrothermal conditions

5. Frictional-viscous flow of phyllosilicate-bearing fault rock: Microphysical model and implications for crustal strength profiles

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