{"@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/1362825894190055424.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1440-1738.1997.tb00175.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1997.tb00175.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1997.tb00175.x"}}],"dc:title":[{"@value":"The seismogenic zone of subduction thrust faults"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p><jats:bold>Abstract</jats:bold> Subduction thrust faults generate earthquakes over a limited depth range. They are aseismic in their seaward updip portions and landward downdip of a critical point. The seaward shallow aseismic zone, commonly beneath accreted sediments, may be a consequence of unconsolidated sediments, especially stable‐sliding smectite clays. Such clays are dehydrated and the fault may become seismogenic where the temperature reaches 100‐‐150°C, that is, at a 5‐‐15 km depth. Two factors may determine the downdip seismogenic limit. For subduction of young hot oceanic lithosphere beneath large accretionary sedimentary prisms and beneath continental crust, the transition to aseismic stable sliding is temperature controlled. The maximum temperature for seismic behavior in crustal rocks is ∼ 350°C, regardless of the presence of water. In addition, great earthquake ruptures initiated at less than this temperature may propagate with decreasing slip to where the temperature is ∼ 450°C. For subduction beneath thin island arc crust and beneath continental crust in some areas, the forearc mantle is reached by the thrust shallower than the 350°C temperature. The forearc upper mantle probably is aseismic because of stable‐sliding serpentinite hydrated by water from the underthrusting oceanic crust and sediments. For many subduction zones the downdip seismogenic width defined by these limits is much less than previously assumed. Within the narrowly defined seismic zone, most of the convergence may occur in earthquakes. Numerical thermal models have been employed to estimate temperatures on the subduction thrust planes of four continental subduction zones. For Cascadia and Southwest Japan where very young and hot plates are subducting, the downdip seismogenic limit on the subduction thrust is thermally controlled and is shallow. For Alaska and most of Chile, the forearc mantle is reached before the critical temperature, and mantle serpentinite provides the limit. In all four regions, the seismogenic zones so defined agree with estimates of the extent of great earthquake rupture, and with the downdip extent of the interseismic locked zone.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1580009750652557952","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000014139684"}],"foaf:name":[{"@value":"R. D. Hyndman"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894190055424","@type":"Researcher","foaf:name":[{"@value":"M. Yamano"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894190055426","@type":"Researcher","foaf:name":[{"@value":"D. A. Oleskevich"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10384871"},{"@type":"EISSN","@value":"14401738"}],"prism:publicationName":[{"@value":"Island Arc"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1997-09","prism:volume":"6","prism:number":"3","prism:startingPage":"244","prism:endingPage":"260"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1997.tb00175.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1997.tb00175.x"}],"createdAt":"2006-04-05","modifiedAt":"2023-10-27","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050011340342223872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake Source"}]},{"@id":"https://cir.nii.ac.jp/crid/1050013861703678720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temperature distribution for interplate seismic events in the southcentral Alaska subduction zone based on 3-D thermomechanical modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1050292726799886976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High- and low-stress subduction zones recognized in the rock record"}]},{"@id":"https://cir.nii.ac.jp/crid/1050298975368397568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3D thermal structural and dehydration modeling in the southern Chile subduction zone and its relationship to interplate earthquakes and the volcanic chain"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564287412501504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamic weakening of smectite-bearing faults at intermediate velocities : implications for subduction zone earthquakes"},{"@value":"Dynamic weakening of smectite‐bearing faults at intermediate velocities: Implications for subduction zone earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050579212423889280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Steady‐State Effective Normal Stress in Subduction Zones Based on Hydraulic Models and Implications for Shallow Slow Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050585095043544960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional thermomechanical modelling beneath Guerrero, Mexico, and its relation to the occurrence of interplate seismic phenomena"}]},{"@id":"https://cir.nii.ac.jp/crid/1050852901090021632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frictional Strengths of Subduction Thrust Rocks in the Region of Shallow Slow Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050857235853799168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Megathrust Shear Modulated by Albite Metasomatism in Subduction Mélanges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214351202688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleothermal structure of the <scp>N</scp>ankai inner accretionary wedge estimated from vitrinite reflectance of cuttings"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708756224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heat flow distribution and thermal structure of the Nankai subduction zone off the Kii Peninsula"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708772096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismogenic characteristics of the Northern Mariana shallow thrust zone from local array data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708835840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stuck in the mud? 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