{"@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/1363670318871998080.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature03901"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature03901.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature03901"}},{"identifier":{"@type":"PMID","@value":"16079843"}},{"identifier":{"@type":"NAID","@value":"80017456200"}}],"dc:title":[{"@value":"Earthquake slip weakening and asperities explained by thermal pressurization"}],"description":[{"notation":[{"@value":"An earthquake occurs when a fault weakens during the early portion of its slip at a faster rate than the release of tectonic stress driving the fault motion. This slip weakening occurs over a critical distance, D(c). Understanding the controls on D(c) in nature is severely limited, however, because the physical mechanism of weakening is unconstrained. Conventional friction experiments, typically conducted at slow slip rates and small displacements, have obtained D(c) values that are orders of magnitude lower than values estimated from modelling seismological data for natural earthquakes. Here we present data on fluid transport properties of slip zone rocks and on the slip zone width in the centre of the Median Tectonic Line fault zone, Japan. We show that the discrepancy between laboratory and seismological results can be resolved if thermal pressurization of the pore fluid is the slip-weakening mechanism. Our analysis indicates that a planar fault segment with an impermeable and narrow slip zone will become very unstable during slip and is likely to be the site of a seismic asperity."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318871998080","@type":"Researcher","foaf:name":[{"@value":"Christopher A. J. Wibberley"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318871998081","@type":"Researcher","foaf:name":[{"@value":"Toshihiko Shimamoto"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1892553967704118019","@type":"Researcher","foaf:name":[{"@value":"Géoazur (GEOAZUR 6526) ; Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967704118018","@type":"Researcher","foaf:name":[{"@value":"Géoazur (GEOAZUR 6526) ; Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (... - 2019) (UNS) ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115902761473","@type":"Researcher","foaf:name":[{"@value":"Géoazur, Publications"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967704118016","@type":"Researcher","foaf:name":[{"@value":"Géoazur (GEOAZUR 6526) ; Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115902761474","@type":"Researcher","foaf:name":[{"@value":"Géoazur (GEOAZUR 6526)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115902761472","@type":"Researcher","foaf:name":[{"@value":"Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115902761600","@type":"Researcher","foaf:name":[{"@value":"Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2005-08","prism:volume":"436","prism:number":"7051","prism:startingPage":"689","prism:endingPage":"692"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/nature03901.pdf"},{"@id":"http://www.nature.com/articles/nature03901"}],"createdAt":"2005-08-03","modifiedAt":"2023-05-18","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335764454144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coseismic dehydration of serpentinite: Evidence from high-velocity friction experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1050585407782192896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frictional strength of ground dolerite gouge at a wide range of slip 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