{"@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/1362825893664083968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/93jb03359"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F93JB03359"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/93JB03359"}}],"dc:title":[{"@value":"Stress perturbations associated with active faults penetrated by boreholes: Possible evidence for near‐complete stress drop and a new technique for stress magnitude measurement"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Detailed studies of stress‐induced wellbore breakouts in wells drilled through active faults reveal stress field discontinuities that are apparently associated with recent fault movements. These discontinuities are expressed as localized rotations in wellbore breakout orientation in the vicinity of the fault penetrated by the borehole. This phenomenon is observed in a variety of tectonic environments and rock types. Utilizing cases where relatively complete knowledge of the horizontal principal stresses is available from in situ measurements, we use three‐dimensional dislocation modeling to demonstrate that these discontinuities can be explained as the superposition of a reference stress state and a perturbation caused by movement on preexisting faults. Case studies from normal, strike‐slip and reverse faulting stress states indicate that nearly complete stress drop is required to match the observed breakout orientation anomalies. Hydraulic fracturing data independently confirm the occurrence of near‐complete stress drop on some faults penetrated by drilling. Modeling of the observed interactions between breakouts and fractures can also be used to obtain information about the magnitude of in situ stress.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825893664083841","@type":"Researcher","foaf:name":[{"@value":"Colleen A. Barton"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893664083840","@type":"Researcher","foaf:name":[{"@value":"Mark D. Zoback"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1994-05-10","prism:volume":"99","prism:number":"B5","prism:startingPage":"9373","prism:endingPage":"9390"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F93JB03359"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/93JB03359"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338207702144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Which is heterogeneous, stress or strength? An estimation from high-density seismic observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760762900352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Small-scale stress fluctuations in borehole breakouts and their implication in identifying potential active faults around the seismogenic megasplay fault, Nankai Trough, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216175278336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Localized rotation of principal stress around faults and fractures determined from borehole breakouts in hole B of the Taiwan Chelungpu-fault Drilling Project (TCDP)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523359104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress field observation and modeling from the NanTroSEIZE scientific drillings in the Nankai Trough system, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704780323840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress state and its anomaly observations in the vicinity of a fault in <scp>N</scp>an<scp>T</scp>ro<scp>SEIZE</scp><scp>E</scp>xpedition 322"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092600238848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of the heterogeneity of stress fields using misfit angles in focal mechanisms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658221813632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recovery of Stress During the Interseismic Period Around the Seismogenic Fault of the 1995 <i>M</i><sub><i>w</i></sub> 6.9 Kobe Earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204064292736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"坑壁破壊から見た応力場変動と石油鉱業への応用"},{"@language":"en","@value":"Stress field fluctuations based on borehole failures and its implications to upstream petroleum industry"},{"@language":"ja-Kana","@value":"コウヘキ ハカイ カラ ミタ オウリョクジョウ ヘンドウ ト セキユ コウギョウ エ ノ オウヨウ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/93jb03359"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.04.009_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.1002/2015gc006072_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0730-3_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2020.228553_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.1029/2018gl079317_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0176-9_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.3720/japt.78.28_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2009.06.020_references_DOI_6xrA45FE2wbsurQnliHoXdbTDUd"}]}