{"@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/1362262944684695552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/jb089ib07p05835"}},{"identifier":{"@type":"URI","@value":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB07p05835"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB07p05835"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JB089iB07p05835"}},{"identifier":{"@type":"NAID","@value":"30034709753"}}],"dc:title":[{"@value":"Tectonic analysis of fault slip data sets"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Using data that include the direction and the sense of motion on individual fault surfaces determined by slickenside lineations, it is possible to reconstruct reduced stress tensors that correspond to the orientation of stress axes and to the ratio ϕ = (σ<jats:sub>2</jats:sub>−σ<jats:sub>3</jats:sub>)/(σ<jats:sub>1</jats:sub>−σ<jats:sub>3</jats:sub>) between principal stress values (σ<jats:sub>1</jats:sub>≥σ<jats:sub>2</jats:sub>≥σ<jats:sub>3</jats:sub>, compression being positive). No assumption is made concerning the orientation of fault planes relative to stress axes, so that reactived faults are taken into account as well as newly created ones. Qualitative and quantitative methods for analysis of fault slip data were developed during the last 10 years. The practical limitation of the methods and the necessity for critical field observations are emphasized. These methods can be applied to focal mechanisms of earthquakes. A more complex analysis of heterogeneous data sets, involving an iterative separation of different stress systems, is also discussed. This analysis enables one to distinguish successive faulting events. Careful qualitative study in the field is in all cases essential.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262944684695552","@type":"Researcher","foaf:name":[{"@value":"Jacques Angelier"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1984-07-10","prism:volume":"89","prism:number":"B7","prism:startingPage":"5835","prism:endingPage":"5848"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB07p05835"},{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB07p05835"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JB089iB07p05835"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202844755456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stress inversion meets plasticity theory: A review of the theories of fault-slip analysis from the perspective of the deviatoric stress-strain space"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810809480960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial heterogeneities in tectonic stress in Kyushu, Japan and their relation to a major shear zone Seismology"},{"@value":"Spatial heterogeneities in tectonic stress in Kyushu, Japan and their relation to a major shear zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704781985536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in paleostress and its magnitude related to seismic cycles in the Chelung‐pu Fault, Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500126336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Determining changes in the state of stress associated with an earthquake via combined focal mechanism and moment tensor analysis: Application to the 2013 Awaji Island earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500145920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantitative estimation of fluid pressure ratio of shear vein in an on-land accretionary complex, the Yokonami mélange, the Cretaceous Shimanto Belt, Kochi, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710504799360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal stress variations along a seismogenic megasplay fault in the subduction zone: <scp>A</scp>n example from the <scp>N</scp>obeoka <scp>T</scp>hrust, southwestern <scp>J</scp>apan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179754862208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in paleostress state along a subduction zone preserved in an on-land accretionary complex, the Yokonami mélange in the Cretaceous Shimanto Belt, Kochi, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183242243712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling heterogeneous deviatoric stress field around the hypocentral area of the 2005 Fukuoka earthquake (M7.0) by spatially distributed moment tensors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379389678848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-spatial-resolution slip tendency modeling based on 3D seismic data to assess induced earthquake potential and identify suitable CO2 storage sites"}]},{"@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/1360848654735986944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Method for estimating the stress field from seismic moment tensor data based on the flow rule in plasticity theory"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654738817664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Bayesian Approach to Estimating a Spatial Stress Pattern From <i>P</i> Wave First‐Motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654739409408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tertiary evolution of the Shimanto belt (Japan): A large‐scale collision in Early Miocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204439988736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"KUT: Software to Rotate Orientation Data"},{"@language":"ja","@value":"傾動補正ソフトウェアの開発"},{"@value":"システム・ソフトウェア開発 傾動補正ソフトウェアの開発"},{"@language":"ja-Kana","@value":"システム ソフトウェア カイハツ ケイドウ ホセイ ソフトウェア ノ カイハツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239580416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent advancement and applications of stress tensor inversion techniques"},{"@language":"ja","@value":"応力逆解析手法の発展と応用"},{"@language":"ja-Kana","@value":"オウリョク ギャクカイセキ シュホウ ノ ハッテン ト オウヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206509766528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic significance of magnetic susceptibility fabrics in Plio-Quaternary mudstones of southwestern foothills, Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390002184855902592","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geoscientific studies on the Quaternary faulting and geomorphic processes of the Ryukyu arc, southwestern Japan"},{"@language":"ja","@value":"琉球弧の地球科学的研究─断層と風化・侵食プロセスに関する研究の課題と展望─"},{"@value":"琉球弧の地球科学的研究 : 断層と風化・侵食プロセスに関する研究の課題と展望"},{"@language":"ja-Kana","@value":"リュウキュウ コ ノ チキュウ カガクテキ ケンキュウ : ダンソウ ト フウカ ・ シンショク プロセス ニ カンスル ケンキュウ ノ カダイ ト テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390014128337708928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Basin structure, depositional age, and paleostress of the lower Miocene Yoka Formation in the Tajima-Mihonoura area, Southwest Japan"},{"@language":"ja","@value":"兵庫県北西部，但馬御火浦の下部中新統八鹿層の盆地構造・堆積年代・古応力"}]},{"@id":"https://cir.nii.ac.jp/crid/1390021218874903808","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of kinematic history of the faults by fault geometry, composite planar fabric, and stress inversion analysis: Case study of the Yunodake Fault that was active during the 2011 Fukushima-ken Hamadori earthquake"},{"@language":"ja","@value":"断層幾何学，複合面構造，応力逆解析から推定した断層の運動像：2011年福島県浜通りの地震で活動した湯ノ岳断層の例"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680992285056","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stress Distribution in the Vicinity of Right Strike-Slip Fault, a Numerical Approach."},{"@language":"ja","@value":"右横ずれ断層周辺の応力分布，数値解析によるアプローチ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490514176","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Kinematics of the East Anatolian Fault Zone between Turkoglu (Kahramanmaras) and Celikhan (Adiyaman), eastern Turkey"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842043307392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleo-stress orientations and magnitudes from triaxial testing and stress inversion analysis in Nankai accretionary prism sediments"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/jb089ib07p05835"},{"@type":"CIA","@value":"30034709753"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0249-7_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.2473/shigentosozai.115.651_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0028_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1002/2015tc004005_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1111/iar.12193_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0342-8_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.4116/jaqua.58.377_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1186/bf03352645_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1002/2013tc003487_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1029/2011jb008687_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.6010/geoinformatics.14.85_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2024.0032_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1016/j.ijggc.2025.104355_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1186/bf03351660_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1002/2014tc003600_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1002/2016gl070129_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1002/2017jb015359_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1002/2017tc004529_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.02.023_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2022.0053_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2019.03.003_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.09.025_references_DOI_RVBXc8o8jLmrHBZTWG72gsodNQ0"}]}