Investigation on Two M w 3.6 and M w 4.1 Earthquakes Triggered by Poroelastic Effects of Hydraulic Fracturing Operations Near Crooked Lake, Alberta-Reference-Cited by-同舟云学术

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Investigation on Two M w 3.6 and M w 4.1 Earthquakes Triggered by Poroelastic Effects of Hydraulic Fracturing Operations Near Crooked Lake, Alberta

Published:2021-05 Issue:5 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Hui Gang¹^ORCID,Chen Shengnan¹^ORCID,Chen Zhangxin¹^ORCID,He Yongming²,Wang Shuhua³^ORCID,Gu Fei⁴^ORCID

Affiliation:

1. Department of Chemical and Petroleum Engineering University of Calgary Calgary AB Canada

2. College of Energy Chengdu University of Technology Chengdu China

3. Computer Modeling Group Ltd. Calgary AB Canada

4. PetroChina Research Institute of Petroleum Exploration and Development Beijing China

Funder

Canada First Research Excellence Fund

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/10.1029/2020JB020308

Reference48 articles.

1. Hydraulic Fracturing and Seismicity in the Western Canada Sedimentary Basin

2. Fault activation by hydraulic fracturing in western Canada

3. General Theory of Three‐Dimensional Consolidation

4. Fault zone architecture and permeability structure

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3. Normal fault reactivation induced by hydraulic fracturing: Poroelastic effects;Interpretation;2024-05-23

4. Brittle sedimentary strata focus a multimodal depth distribution of seismicity during hydraulic fracturing in the Sichuan Basin, Southwest China;Tectonophysics;2024-05

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