{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362825894887086464.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018jb016765"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016765"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB016765"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018JB016765"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016765"}}],"dc:title":[{"@value":"Slow Slip Event On the Southern San Andreas Fault Triggered by the 2017 <i>M</i><sub><i>w</i></sub>8.2 Chiapas (Mexico) Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Observations of shallow fault creep reveal increasingly complex time‐dependent slip histories that include quasi‐steady creep and triggered as well as spontaneous accelerated slip events. Here we report a recent slow slip event on the southern San Andreas fault triggered by the 2017 <jats:italic>M</jats:italic><jats:sub><jats:italic>w</jats:italic></jats:sub>8.2 Chiapas (Mexico) earthquake that occurred 3,000 km away. Geodetic and geologic observations indicate that surface slip on the order of 10 mm occurred on a 40‐km‐long section of the southern San Andreas fault between the Mecca Hills and Bombay Beach, starting minutes after the Chiapas earthquake and continuing for more than a year. Both the magnitude and the depth extent of creep vary along strike. We derive a high‐resolution map of surface displacements by combining Sentinel‐1 Interferometric Synthetic Aperture Radar acquisitions from different lines of sight. Interferometric Synthetic Aperture Radar‐derived displacements are in good agreement with the creepmeter data and field mapping of surface offsets. Inversions of surface displacement data using dislocation models indicate that the highest amplitudes of surface slip are associated with shallow (<1 km) transient slip. We performed 2‐D simulations of shallow creep on a strike‐slip fault obeying rate‐and‐state friction to constrain frictional properties of the top few kilometers of the upper crust that can produce the observed behavior.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825894887086593","@type":"Researcher","foaf:name":[{"@value":"Ekaterina Tymofyeyeva"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California San Diego  La Jolla CA USA"},{"@value":"Now at Jet Propulsion Laboratory California Institute of Technology  Pasadena CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086471","@type":"Researcher","foaf:name":[{"@value":"Yuri Fialko"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California San Diego  La Jolla CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086469","@type":"Researcher","foaf:name":[{"@value":"Junle Jiang"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California San Diego  La Jolla CA USA"},{"@value":"Now at Department of Earth and Atmospheric Sciences Cornell University  Ithaca NY USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086467","@type":"Researcher","foaf:name":[{"@value":"Xiaohua Xu"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California San Diego  La Jolla CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086464","@type":"Researcher","foaf:name":[{"@value":"David Sandwell"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California San Diego  La Jolla CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086470","@type":"Researcher","foaf:name":[{"@value":"Roger Bilham"}],"jpcoar:affiliationName":[{"@value":"CIRES and Geological Sciences University of Colorado  Boulder CO USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086465","@type":"Researcher","foaf:name":[{"@value":"Thomas K. Rockwell"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences San Diego State University  San Diego CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086592","@type":"Researcher","foaf:name":[{"@value":"Chelsea Blanton"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences San Diego State University  San Diego CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086466","@type":"Researcher","foaf:name":[{"@value":"Faith Burkett"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences San Diego State University  San Diego CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086468","@type":"Researcher","foaf:name":[{"@value":"Allen Gontz"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences San Diego State University  San Diego CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894887086594","@type":"Researcher","foaf:name":[{"@value":"Shahram Moafipoor"}],"jpcoar:affiliationName":[{"@value":"Geodetics Inc.  San Diego CA USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2019-09","prism:volume":"124","prism:number":"9","prism:startingPage":"9956","prism:endingPage":"9975"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#am","http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016765"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB016765"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018JB016765"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB016765"}],"createdAt":"2019-08-05","modifiedAt":"2023-09-01","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360009142419703168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Ocean's Impact on Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593724550144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Community‐Driven Code Comparisons for Three‐Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266981878912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of triggered shallow slips caused by large earthquakes using L-band SAR interferometry"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2018jb016765"},{"@type":"CROSSREF","@value":"10.1029/2020gl087273_references_DOI_4LHBqynUBVvVyuNojmh4MzMHe05"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01239-6_references_DOI_4LHBqynUBVvVyuNojmh4MzMHe05"},{"@type":"CROSSREF","@value":"10.1029/2021jb023519_references_DOI_648iinG8lbb2AgRMGtpnlEXoDU6"}]}