{"@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/1363670318898404608.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.285.5425.236"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.285.5425.236"}}],"dc:title":[{"@value":"Role of Fluids in Faulting Inferred from Stress Field Signatures"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The stress orientation signature of weak faults containing high-pressure fluids has been observed for segments of the San Andreas fault system in southern California. The inferred lithostatic fluid pressures extend into the surrounding relatively intact rock in a zone scaling with the width of the interseismic strain accumulation. Repeated strain-related fracturing and crack sealing may have created low-permeability barriers that seal fluids into the network of currently active fractures.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318898404608","@type":"Researcher","foaf:name":[{"@value":"Jeanne L. Hardebeck"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, MC 252-21, California Institute of Technology, Pasadena, CA 91125, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318898404609","@type":"Researcher","foaf:name":[{"@value":"Egill Hauksson"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory, MC 252-21, California Institute of Technology, Pasadena, CA 91125, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"1999-07-09","prism:volume":"285","prism:number":"5425","prism:startingPage":"236","prism:endingPage":"239"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.285.5425.236"}],"createdAt":"2002-07-27","modifiedAt":"2024-01-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285704779197696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in the stress field after the 2008 <i>M</i>7.2 Iwate‐Miyagi Nairiku earthquake in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869625344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Change in stress field after the 2011 great Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476884224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress accumulation process in and around the Atotsugawa fault, central Japan, estimated from focal mechanism analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654733480064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress rotations and the long-term weakness of the Median Tectonic Line and the Rokko-Awaji Segment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815676718592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial and Temporal Stress Variations before and after the 2008 Wenchuan <i>M</i><sub>w</sub> 7.9 Earthquake and its Implications: A Study based on Borehole Stress Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390004222631011072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hyper Dense Seismic Observation for Investigation on Fault Zone Development: Application to Hypocentral Area of 2000 Western Tottori Earthquake"},{"@language":"ja","@value":"超多点稠密地震観測による断層帯発達過程の解明に向けて"},{"@value":"超多点稠密地震観測による断層帯発達過程の解明に向けて : 2000年鳥取県西部地震域への適用"},{"@language":"ja-Kana","@value":"チョウタテンチュウミツジシン カンソク ニ ヨル ダンソウタイ ハッタツ カテイ ノ カイメイ ニ ムケテ : 2000ネン トットリケン セイブ ジシンイキ エ ノ テキヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266975402496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Causes of the N–S compressional aftershocks of the E–W compressional 2008 Iwate–Miyagi Nairiku earthquake (M7.2) in the northeastern Japan arc"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.285.5425.236"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.511_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"},{"@type":"CROSSREF","@value":"10.1002/2014jb011291_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.05.013_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"},{"@type":"CROSSREF","@value":"10.1002/2014tc003600_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.08.042_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"},{"@type":"CROSSREF","@value":"10.1111/1755-6724.14965_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1073-z_references_DOI_ATE3r8tCpUe1Ozp6BxgmICBxcqw"}]}