Spatial Variations of Upper Crustal Anisotropy Along the San Jacinto Fault Zone in Southern California: Constraints From Shear Wave Splitting Analysis-Reference-Cited by-同舟云学术

Spatial Variations of Upper Crustal Anisotropy Along the San Jacinto Fault Zone in Southern California: Constraints From Shear Wave Splitting Analysis

Published:2021-04 Issue:4 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Jiang Enyuan¹,Liu Kelly H.¹^ORCID,Gao Yuan¹²^ORCID,Fu Xiaofei³,Gao Stephen S.¹^ORCID

Affiliation:

1. Geology and Geophysics Program Missouri University of Science and Technology Rolla MO USA

2. Key Laboratory of Earthquake Prediction Institute of Earthquake Forecasting China Earthquake Administration Beijing China

3. College of Earth Science and Research Institute of Unconventional Oil and Gas Northeast Petroleum University Daqing Heilongjiang China

Funder

National Science Foundation

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/10.1029/2020JB020876

Reference45 articles.

1. S-wave anisotropy in the upper mantle under a volcanic area in Japan

2. Layered crustal anisotropy around the San Andreas Fault near Parkfield, California

3. Anisotropic structure under a back arc spreading region, the Taupo Volcanic Zone, New Zealand

4. Mapping stress and structurally controlled crustal shear velocity anisotropy in California

5. Shear-wave polarizations on a curved wavefront at an isotropic free surface

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