Searching for Transient Slow Slips Along the San Andreas Fault Near Parkfield Using Independent Component Analysis-Reference-Cited by-同舟云学术

Searching for Transient Slow Slips Along the San Andreas Fault Near Parkfield Using Independent Component Analysis

Published:2022-06 Issue:6 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Michel Sylvain¹^ORCID,Jolivet Romain¹²^ORCID,Lengliné Olivier³,Gualandi Adriano⁴^ORCID,Larochelle Stacy⁵^ORCID,Gardonio Blandine¹⁶^ORCID

Affiliation:

1. Département de Géosciences Laboratoire de Géologie PSL Université CNRS UMR 8538 École Normale Supérieure Paris France

2. Institut Universitaire de France Paris France

3. École et Observatoire des Sciences de la Terre UMR7516 Université de Strasbourg / CNRS Strasbourg France

4. Istituto Nazionale di Geofisica e Vulcanologia Osservatrio Nazionale Terremoti Roma Italy

5. Department of Geology and Planetary Sciences California Institute of Technology Pasadena CA USA

6. Laboratoire de Géologie de Lyon CNRS‐Université Lyon 1 Lyon France

Funder

H2020 European Research Council

Centre National d’Etudes Spatiales

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/10.1029/2021JB023201

Reference90 articles.

1. From Geodetic Imaging of Seismic and Aseismic Fault Slip to Dynamic Modeling of the Seismic Cycle

2. Shallow deformation of the San Andreas fault 5 years following the 2004 Parkfield earthquake (Mw6) combining ERS2 and Envisat InSAR

3. Change of apparent segmentation of the San Andreas fault around Parkfield from space geodetic observations across multiple periods

4. Postseismic deformation due to theMw6.0 2004 Parkfield earthquake: Stress-driven creep on a fault with spatially variable rate-and-state friction parameters

5. Benoit A.(2020).Towards a continuous monitoring of small‐scale surface displacements with radar interferometry: Study of the aseismic behavior along the North Anatolian fault. Retrieved fromhttps://tel.archives-ouvertes.fr/tel-03464685v2/document

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