Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA-Reference-Cited by-同舟云学术

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Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA

Published:2021-09-14 Issue:18 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Li Bing Q.¹²^ORCID,Khoshmanesh Mostafa³,Avouac Jean‐Philippe¹³^ORCID

Affiliation:

1. Division of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA

2. Now at Department of Civil and Environmental Engineering Western University London ON Canada

3. Division of Engineering and Applied Sciences California Institute of Technology Pasadena CA USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL095108

Reference46 articles.

1. Proceedings of the 5th Workshop on Geothermal Reservoir Engineering;Ahmed U.,1979

2. Understanding rate effects in injection-induced earthquakes

3. Geodetic measurements and numerical models of transient deformation at Raft River geothermal field, Idaho, USA

4. Fluid geochemistry at the Raft River geothermal field, Idaho, USA: New data and hydrogeological implications

5. Subsidence rates at the southern Salton Sea consistent with reservoir depletion

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