Postseismic Process Inversion Using Full Time Series of Surface Deformation: Full Time‐Series Inversion (FTI) Theory and Its Application to the 2017 Sarpol‐e Zahab Earthquake-Reference-Cited by-同舟云学术

Postseismic Process Inversion Using Full Time Series of Surface Deformation: Full Time‐Series Inversion (FTI) Theory and Its Application to the 2017 Sarpol‐e Zahab Earthquake

Published:2022-09 Issue:9 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Yue Han¹²³^ORCID,Wang Kang⁴^ORCID,Xue Lian¹³,Shen Zhengkang¹⁵,Sun Jianbao⁶^ORCID

Affiliation:

1. School of Earth and Space Sciences Peking University Beijing China

2. Center for Habitable Intelligent Geosciences Institute of Artificial Intelligence Peking University Beijing China

3. Hongshan Geophysical National Observation and Research Station Peking University Beijing China

4. Department of Earth and Planetary Science University of California, Berkeley Berkeley CA USA

5. Department of Earth, Planetary, and Space Sciences University of California, Los Angeles Los Angeles CA USA

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

Funder

National Natural Science Foundation 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/10.1029/2021JB023317

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3. A unified continuum representation of post-seismic relaxation mechanisms: semi-analytic models of afterslip, poroelastic rebound and viscoelastic flow

4. Displacement and Stress Associated with Distributed Anelastic Deformation in a Half‐Space

5. A high-resolution, time-variable afterslip model for the 2010 Maule Mw = 8.8, Chile megathrust earthquake

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