{"@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/1363388844251279744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016jb013242"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JB013242"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013242"}}],"dc:title":[{"@value":"Spatiotemporal variations of characteristic repeating earthquake sequences along the Middle America Trench in Mexico"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Searching for repeating earthquakes allows the examination of spatiotemporal variation of slip budget in the subduction of the Cocos plate in the Guerrero‐Oaxaca region of Mexico. As different transient phenomena continuously load and unload stresses around asperities in an area where megathrust earthquakes nucleate, repeating earthquakes act as track markers for slip on the plate interface. We systematically examined 14 years of waveform records from 2001 through 2014 to identify repeating earthquakes along the subducting segment of the Cocos plate. An analysis of waveform similarity resulted in a significant number (224) of earthquake sequences with highly correlated waveforms (correlation coefficient cc ≥ 0.95 and spectral coherency coh ≥ 0.95). The reported set of correlated waveforms shows a well‐defined clustering in space and substantial temporal variability. We find a significant increase of repeating earthquake activity after the 20 March 2012 Ometepec (<jats:italic>M<jats:sub>w</jats:sub></jats:italic>7.4) and 18 April 2014 Tecpan (<jats:italic>M<jats:sub>w</jats:sub></jats:italic>7.2) earthquakes as a result of the postseismic relaxation. In contrast, the rupture zone of the 1985 (<jats:italic>M<jats:sub>w</jats:sub></jats:italic>8.1) Michoacán earthquake is completely devoid of repeating sequences, suggesting a strongly coupled segment. Examining the temporal behavior of repeating earthquake activity provides a new tool to better understand how creeping of the subduction thrust controls stress release and postseismic relaxation.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844251279744","@type":"Researcher","foaf:name":[{"@value":"Luis A. Dominguez"}],"jpcoar:affiliationName":[{"@value":"National School for Advanced Studies National Autonomous University of Mexico Morelia Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844251279745","@type":"Researcher","foaf:name":[{"@value":"Taka'aki Taira"}],"jpcoar:affiliationName":[{"@value":"Berkeley Seismological Laboratory University of California Berkeley California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844251279616","@type":"Researcher","foaf:name":[{"@value":"Miguel A. Santoyo"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics National Autonomous University of Mexico Unidad Morelia Mexico"}]}],"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":"2016-12","prism:volume":"121","prism:number":"12","prism:startingPage":"8855","prism:endingPage":"8870"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JB013242"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013242"}],"createdAt":"2016-12-09","modifiedAt":"2024-06-21","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285704783286912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Emergence and disappearance of interplate repeating earthquakes following the 2011 <i>M</i>9.0 Tohoku‐oki earthquake: Slip behavior transition between seismic and aseismic depending on the loading rate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711273633920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Repeating Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390003825203695104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeating Earthquakes Along the Colombian Subduction Zone"},{"@value":"Repeating earthquakes. Along the Colombia subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791998115840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of repeating earthquakes and their application in characterizing slow fault slip"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016jb013242"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0284-z_references_DOI_VWOPoWMCOF6fCr7ZAEpN63C0SYT"},{"@type":"CROSSREF","@value":"10.1002/2016jb013914_references_DOI_VWOPoWMCOF6fCr7ZAEpN63C0SYT"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-053018-060119_references_DOI_VWOPoWMCOF6fCr7ZAEpN63C0SYT"},{"@type":"CROSSREF","@value":"10.20965/jdr.2020.p0645_references_DOI_VWOPoWMCOF6fCr7ZAEpN63C0SYT"}]}