{"@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/1362262943593336320.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1017/s0016756800059987"}},{"identifier":{"@type":"URI","@value":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800059987"}}],"dc:title":[{"@value":"The Mechanics of Oblique Slip Faulting"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Summary</jats:title><jats:p>The various mechanisms which could cause oblique slip faulting are briefly reviewed. It is thought that such faulting may frequently arise from the existence of preferred planes of fracture within the rocks. The dynamics of this mechanism is studied in some detail and an expression is obtained for the first direction of slip within the plane under the influence of a general stress system of given orientation it is found that the initial slip may occur in any possible direction within the plane, the direction depending on the relative values of the three principle pressures. The theory suggests that when a pre-existing fault is subjected to a reorientated stress system (typical or rotated) the movement after fracture will usually be oblique. In conclusion, the general implications of the theory are discussed.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380009142495585925","@type":"Researcher","foaf:name":[{"@value":"M. H. P. Bott"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167568"},{"@type":"EISSN","@value":"14695081"}],"prism:publicationName":[{"@value":"Geological Magazine"}],"dc:publisher":[{"@value":"Cambridge University Press (CUP)"}],"prism:publicationDate":"1959-04","prism:volume":"96","prism:number":"2","prism:startingPage":"109","prism:endingPage":"117"},"reviewed":"false","dc:rights":["https://www.cambridge.org/core/terms"],"url":[{"@id":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800059987"}],"createdAt":"2009-05-01","modifiedAt":"2019-06-05","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/1050001338207715968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temporal changes in the internal stresses and pore pressures in a large-scale submarine mass transport deposit"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022996649445760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (M7.3)"},{"@value":"Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (<i>M</i>7.3)"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282813476898304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shear Strain Energy Change Caused by the Interplate Coupling Along the Nankai Trough: An Integration Analysis Using Stress Tensor Inversion and Slip-Deficit Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760656579712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fast multiple inversion for stress analysis from fault-slip data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760694784896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Physical Meaning of Stress Difference for Fault-Slip Analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1050870297870756096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The role of fluids in earthquake swarms in northeastern Noto Peninsula, central Japan: insights from source mechanisms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709077376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High fluid pressure and triggered earthquakes in the enhanced geothermal system in Basel, Switzerland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229802055680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of pore fluid pressures in a stimulated geothermal reservoir inferred from earthquake focal mechanisms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232324962688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A computerized method to estimate friction coefficient from orientation distribution of meso-scale faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232468992128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reactivation of map-scale faults in response to changes in crustal stress: Examples from Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523377024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of pore fluid pressure and tectonic stress on diverse seismic activities around the Mt. 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