{"@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/1362262943836017792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jsg.2006.03.008"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814106000575?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814106000575?httpAccept=text/plain"}}],"dc:title":[{"@value":"Computerized identification of stress tensors determined from heterogeneous fault-slip data by combining the multiple inverse method and k-means clustering"}],"description":[{"notation":[{"@value":"The multiple inverse method is a resampling technique that can separate stresses from heterogeneous fault-slip data. Numerous optimal stresses are determined for each extracted subset of data, and the clusters of these stresses are thought to represent significant solutions. Hitherto, the clusters have had to be visually recognized on stereonets. This study computerized the identification of the clusters by using the k-means clustering technique. We tested the technique using artificial datasets with known solutions. As a result, it was found that the present method detected objectively the correct solutions. In addition, the spread of each cluster was evaluated to indicate the confidence levels of the identified stresses that were represented by the cluster centers."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943836017792","@type":"Researcher","foaf:name":[{"@value":"Makoto Otsubo"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943836017794","@type":"Researcher","foaf:name":[{"@value":"Katsushi Sato"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943836017793","@type":"Researcher","foaf:name":[{"@value":"Atsushi Yamaji"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier 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<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/1360567182409656448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sinistral transpressional and extensional tectonics in Dronning Maud Land, East Antarctica, including the Sør Rondane Mountains"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453500544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal slip change based on curved 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