{"@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/1361981469135065728.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2001jb000791"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001JB000791"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001JB000791"}},{"identifier":{"@type":"NAID","@value":"30013328100"}}],"dc:title":[{"@value":"Constitutive properties for the shear failure of intact granite in seismogenic environments"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>To investigate how the parameters prescribing the slip‐dependent constitutive law are affected by seismogenic environments, we conducted a series of triaxial fracture experiments using intact Tsukuba‐granite samples, which were deformed at wet, temperature‐pressure conditions that correspond to a crustal depth range down to 15 km at a strain rate of 10<jats:sup>−5</jats:sup>/s. It is conclusively demonstrated that the critical slip displacement <jats:italic>D</jats:italic><jats:sub>c</jats:sub> is virtually constant at the conditions of depths shallower than 10 km, and that <jats:italic>D</jats:italic><jats:sub>c</jats:sub> increases with increasing depth at depths greater than 10 km, because of the effect of temperature in the brittle‐plastic transition regime. The breakdown stress drop for intact rock is found to be roughly constant (100 MPa) in a depth range down to 15 km. The apparent fracture energy increases with increasing depth at depths greater than 10 km. These results consistently lead to the conclusion that the stability of the breakdown process is enhanced at depths greater than 10 km.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469135065728","@type":"Researcher","foaf:name":[{"@value":"Aitaro Kato"}],"jpcoar:affiliationName":[{"@value":"Earthquake Prediction Research Center, Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469135065600","@type":"Researcher","foaf:name":[{"@value":"Mitiyasu Ohnaka"}],"jpcoar:affiliationName":[{"@value":"Earthquake Prediction Research Center, Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469135065729","@type":"Researcher","foaf:name":[{"@value":"Hiromine Mochizuki"}],"jpcoar:affiliationName":[{"@value":"Earthquake Prediction Research Center, Earthquake Research Institute The University of Tokyo  Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2003-01","prism:volume":"108","prism:number":"B1","prism:startingPage":"2060"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001JB000791"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001JB000791"}],"createdAt":"2003-05-23","modifiedAt":"2023-10-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050869456410401280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Gravity changes observed between 2004 and 2009 near the Tokai slow-slip area and prospects for detecting fluid flow during future slow-slip events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380590160768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-resolution image on terminus of fault rupture: relationship with volcanic hydrothermal structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490176384","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Earthquake cycles and physical modeling of the process leading up to a large earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390283659852907776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of anti-contamination coring system for microbiological studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1390569181327751424","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dating of a fault zone distributed in the South Kyushu shear zone based on fission-track thermochronology and U-Pb dating"},{"@language":"ja","@value":"フィッション・トラック熱年代解析およびU-Pb年代測定に基づいた南九州せん断帯に分布する破砕帯の活動時期"},{"@language":"ja-Kana","@value":"フィッション ・ トラック ネツ ネンダイ カイセキ オヨビ U-Pb ネンダイ ソクテイ ニ モトズイタ ミナミキュウシュウ セン ダンタイ ニ ブンプ スル ハサイタイ ノ カツドウ ジキ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046932736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Non-volcanic seismic swarm and fluid transportation driven by subduction of the Philippine Sea slab beneath the Kii Peninsula, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2001jb000791"},{"@type":"CIA","@value":"30013328100"},{"@type":"OPENAIRE","@value":"doi_dedup___::d3fac68970f1cf763bda32d782b9bf60"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-86_references_DOI_OlIKzD4xhGnGLCe3BdcwxRaU3tF"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2020.0052_references_DOI_OlIKzD4xhGnGLCe3BdcwxRaU3tF"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.1.93_references_DOI_OlIKzD4xhGnGLCe3BdcwxRaU3tF"},{"@type":"CROSSREF","@value":"10.1093/gji/ggae435_references_DOI_OlIKzD4xhGnGLCe3BdcwxRaU3tF"}]}