{"@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/1360855570538540928.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017gl075899"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL075899"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075899"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL075899"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075899"}}],"dc:title":[{"@value":"Aseismic Transform Fault Slip at the Mendocino Triple Junction From Characteristically Repeating Earthquakes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The Mendocino Triple Junction (MTJ), at the northern terminus of the San Andreas Fault system, is an actively deforming plate boundary region with poorly constrained estimates of seismic coupling on most offshore fault surfaces. Characteristically repeating earthquakes provide spatial and temporal descriptions of aseismic creep at the MTJ, including on the oceanic transform Mendocino Fault Zone (MFZ) as it subducts beneath North America. Using a dataset of earthquakes from 2008 to 2017, we find that the easternmost segment of the MFZ displays creep during this period at about 65% of the long‐term slip rate. We also find creep at slower rates on the shallower strike‐slip interface between the Pacific plate and the North American accretionary wedge, as well as on a fault that accommodates Gorda subplate internal deformation. After a nearby<jats:italic>M</jats:italic>5.7 earthquake in 2015, we observe a possible decrease in aseismic slip on the near‐shore MFZ that lasts from 2015 to at least early 2017.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380855570538540928","@type":"Researcher","foaf:name":[{"@value":"Kathryn Materna"}],"jpcoar:affiliationName":[{"@value":"Berkeley Seismology Lab Berkeley CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855570538540930","@type":"Researcher","foaf:name":[{"@value":"Taka'aki Taira"}],"jpcoar:affiliationName":[{"@value":"Berkeley Seismology Lab Berkeley CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855570538540929","@type":"Researcher","foaf:name":[{"@value":"Roland Bürgmann"}],"jpcoar:affiliationName":[{"@value":"Berkeley Seismology Lab Berkeley CA USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2018-01-24","prism:volume":"45","prism:number":"2","prism:startingPage":"699","prism:endingPage":"707"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL075899"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075899"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL075899"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075899"}],"createdAt":"2018-01-10","modifiedAt":"2024-06-30","relatedProduct":[{"@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/1360568467269617152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Repeating earthquakes and interplate coupling along the western part of the North Anatolian Fault"}]},{"@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":"10.1002/2017gl075899"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0284-z_references_DOI_A8X6yzKFCPghx7ereseW4dIr9Rz"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-053018-060119_references_DOI_A8X6yzKFCPghx7ereseW4dIr9Rz"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2019.228185_references_DOI_A8X6yzKFCPghx7ereseW4dIr9Rz"}]}