{"@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/1360004233292112256.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018jb015765"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB015765"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015765"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB015765"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015765"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Absolute Stress Fields in the Source Region of the 1992 Landers Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Earthquake focal mechanisms are often inverted to obtain the deviatoric stress field. Because shear stress is equal to the frictional strength of the fault at the time of an earthquake, six components of the absolute stress tensor at the hypocenter can be obtained from a focal mechanism by combining deviatoric stress fields with the Coulomb failure criterion. For a data set of focal mechanisms determined for southern California earthquakes, including the 1992 Landers earthquake sequence, we calculated the absolute stress tensors at their hypocenters using a standard intrinsic friction coefficient under three pore pressure conditions, parameterized by the reference pore pressure at the optimally oriented faults to the stress field. Three absolute stress fields were obtained for southern California immediately before the Landers main shock by applying each data set of the stress tensors to an inversion scheme based on Bayesian statistical inference and Akaike's Bayesian Information Criterion. The coseismic stress field was calculated to obtain the absolute stress fields immediately after the main shock. The variations of the coseismic stress rotation were related to the reference pore pressure. Comparing this relation with that obtained through stress inversion, we determined the absolute stress field and the most plausible reference pore pressure to be hydrostatic. On average, the maximum shear stresses immediately before the main shock were 44 ± 15 and 79 ± 24 MPa at depths of 5 and 10 km, respectively. Earthquakes on the off‐plate boundary faults in southern California occur on faults that are loaded by Anderson‐Byerlee stress conditions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751160798592","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30451826"},{"@type":"NRID","@value":"1000030451826"},{"@type":"NRID","@value":"9000380981028"},{"@type":"NRID","@value":"9000007701558"},{"@type":"NRID","@value":"9000018811561"},{"@type":"NRID","@value":"9000283105031"},{"@type":"NRID","@value":"9000410192668"}],"foaf:name":[{"@value":"Toshiko Terakawa"}],"jpcoar:affiliationName":[{"@value":"Earthquake and Volcano Research Center, Graduate School of Environmental Studies Nagoya University  Nagoya Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233292112132","@type":"Researcher","foaf:name":[{"@value":"Egill Hauksson"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, Division of Geological and Planetary Sciences California Institute of Technology  Pasadena CA USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2018-10","prism:volume":"123","prism:number":"10","prism:startingPage":"8874","prism:endingPage":"8890"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB015765"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015765"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB015765"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015765"}],"createdAt":"2018-09-29","modifiedAt":"2023-09-03","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=absolute%20stress%20fields","dc:title":"absolute stress fields"},{"@id":"https://cir.nii.ac.jp/all?q=pore%20fluid%20pressures","dc:title":"pore fluid pressures"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782297844608","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26400451"},{"@type":"JGN","@value":"JP26400451"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26400451/"}],"notation":[{"@language":"ja","@value":"理論と観測に基づく東北日本弧・プレート境界面の絶対強度の推定"},{"@language":"en","@value":"Fault strength of the plate interface along the northeastern Japan Arc inferred from tectonic loading model and inversion alayisis"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256975055232","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18K03801"},{"@type":"JGN","@value":"JP18K03801"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18K03801/"}],"notation":[{"@language":"ja","@value":"日本列島域の三次元絶対応力場の推定"},{"@language":"en","@value":"Estimating the 3-D tectonic stress fields in and around the Japanese Islands"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282677738222848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Discrimination of fault planes from auxiliary planes based on simultaneous determination of stress tensor and a large number of fault plane solutions"}]},{"@id":"https://cir.nii.ac.jp/crid/1050285700277135232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Elastic strain energy and pore-fluid pressure control of aftershocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709077376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High fluid pressure and triggered earthquakes in the enhanced geothermal system in Basel, 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