{"@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/1361981471378413184.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0040-1951(82)90126-3"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195182901263?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0040195182901263?httpAccept=text/plain"}}],"dc:title":[{"@value":"Subduction zones: An introduction to comparative subductology"}],"description":[{"notation":[{"@value":"Abstract   The subduction model for trench-arc-back arc systems was deduced more or less as a logical consequence of sea-floor spreading. Many features in these systems, such as thrust-type inter-plate earthquakes and deep earthquakes along Wadati-Benioff zones, are readily explained by the subduction model. But, other features such as extensional spreading and high heat flow in back arc regions and arc volcanism are difficult to explain. An approach to solve these problems may be to recognize the existence of the two basically different modes of subduction: one Chilean-type — causing a compressional stress regime in the arc and back arc regions; the other — Mariana-type — causing a tensional stress regime. Implications of the two types of the mode of subduction for some tectonic problems, such as vertical movement and sediment accretion at trenches are discussed, with special reference to the results of recent DSDP active margin drilling. In discussing the possible causes of the two modes, it is suggested that the large-scale thermal and stress regimes in the back arc areas may not be the direct products of simple subduction, but of some additional factors involving much greater energy, such as mantle flow associated with the motion of major plates. Finally, the possible great importance of various types of collision, accretion and erosion at subduction zones is emphasized."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981471378413184","@type":"Researcher","foaf:name":[{"@value":"Seiya Uyeda"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1982-01","prism:volume":"81","prism:number":"3-4","prism:startingPage":"133","prism:endingPage":"159"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0040195182901263?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0040195182901263?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050587981434843648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Along-dip segmentation of the 2011 off the Pacific coast of Tohoku Earthquake and comparison with other megathrust earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232306089088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subduction thermal structure, metamorphism and seismicity beneath north-central Chile"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690893115392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recycled Archean sulfur in the mantle wedge of the Mariana Forearc and microbial sulfate reduction within an extremely alkaline serpentine seamount"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707433021056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemistry of metabasites from the North Shahrekord metamorphic complex, Sanandaj-Sirjan Zone: Geodynamic implications for the Pan-African basement in Iran"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182185624704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal history analysis of granitic rocks in an arc-trench system based on apatite fission-track thermochronology: A case study of the Northeast Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185955077504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"India-Antarctica-Australia-Laurentia connection in the Paleoproterozoic-Mesoproterozoic revisited: Evidence from new zircon U-Pb and monazite chemical age data from the Eastern Ghats Belt, India"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453555328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Intermediate P/T-type regional metamorphism of the Isua Supracrustal Belt, southern west Greenland: The oldest Pacific-type orogenic belt?"}]},{"@id":"https://cir.nii.ac.jp/crid/1520573330251881984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variability of megathrust earthquakes in the world revealed by the 2011 Tohoku-oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417117561472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"(U–Th)/He thermochronometric mapping across the northeast Japan Arc : towards understanding mountain building in an island-arc setting"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0040-1951(82)90126-3"},{"@type":"OPENAIRE","@value":"doi_dedup___::1c32ae37464f55b66dd04f4002661490"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.04.011_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.03.002_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.06.003_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1130/b30336.1_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1016/j.jaesx.2019.100005_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1016/j.precamres.2017.03.003_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01151-z_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1016/j.jog.2018.09.004_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.05.020_references_DOI_SUcph8vxE91NeO89cX2twAOpDnV"}]}