{"@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/1363670318208520064.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jsg.2006.03.020"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814106000654?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0191814106000654?httpAccept=text/plain"}}],"dc:title":[{"@value":"Fracture strength of tourmaline and epidote by three-point bending test: application to microboudin method for estimating absolute magnitude of palaeodifferential stress"}],"description":[{"notation":[{"@value":"Abstract   Three-point bending tests are conducted on millimetre-scale tourmaline and epidote samples at room temperature and pressure to determine fracture strengths suitable for use with the microboudin method of palaeostress analysis. The fracture strength of the samples is obtained from the Weibull scale and shape parameters using a size-effect model. Three different size-effect models are evaluated and it is found that the effective-length model is the most appropriate for describing the fracture strength of tourmaline and epidote based on geological constraints. The palaeodifferential stresses determined by this method for samples from Wadi Tayin (Sultanate of Oman), Greenbushes (Australia) and four high-pressure metamorphic belts in Japan are in the range of 10–300 MPa."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318208520066","@type":"Researcher","foaf:name":[{"@value":"Nozomi Kimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318208520068","@type":"Researcher","foaf:name":[{"@value":"Hideo Awaji"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318208520064","@type":"Researcher","foaf:name":[{"@value":"Masato Okamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318208520065","@type":"Researcher","foaf:name":[{"@value":"Yoshihisa Matsumura"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318208520067","@type":"Researcher","foaf:name":[{"@value":"Toshiaki Masuda"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2006-06","prism:volume":"28","prism:number":"6","prism:startingPage":"1093","prism:endingPage":"1102"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0191814106000654?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0191814106000654?httpAccept=text/plain"}],"createdAt":"2006-05-09","modifiedAt":"2021-07-27","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360286990822610944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Kinetics and duration of metamorphic mineral growth in a subduction complex: zircon and phengite in the Nagasaki metamorphic complex, western Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657255030272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Application of the microboudin method to palaeodifferential stress analysis of deformed impure marbles from Syros, Greece: Implications for grain-size and calcite-twin palaeopiezometers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657255095424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contrast in stress–strain history during exhumation between high- and ultrahigh-pressure metamorphic units in the Western Alps: Microboudinage analysis of piemontite in metacherts"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213934976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Afterslip associated with interplate earthquakes and the viscoelastic behavior of rocks"},{"@language":"ja","@value":"プレート境界地震に伴う余効すべりと岩石の粘弾性挙動"},{"@language":"ja-Kana","@value":"プレート キョウカイ ジシン ニ トモナウ ヨコウスベリ ト ガンセキ ノ ネンダンセイ キョドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681521399296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The relationship between the proportion of microboudinaged columnar grains and far–field differential stress: A numerical model for analyzing paleodifferential stress"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842026932864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Statistical model selection between elastic and Newtonian viscous matrix models for the microboudin palaeopiezometer"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.jsg.2006.03.020"},{"@type":"OPENAIRE","@value":"doi_dedup___::06097f53d769cb029f562d143f83fb4a"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0669-4_references_DOI_8jswYic9JmZhs9Ofs8h6EFKfTjz"},{"@type":"CROSSREF","@value":"10.1007/s00410-019-1629-8_references_DOI_8jswYic9JmZhs9Ofs8h6EFKfTjz"},{"@type":"CROSSREF","@value":"10.5575/geosoc.115.448_references_DOI_8jswYic9JmZhs9Ofs8h6EFKfTjz"},{"@type":"CROSSREF","@value":"10.2465/jmps.160711_references_DOI_8jswYic9JmZhs9Ofs8h6EFKfTjz"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2010.11.002_references_DOI_8jswYic9JmZhs9Ofs8h6EFKfTjz"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2016.06.004_references_DOI_8jswYic9JmZhs9Ofs8h6EFKfTjz"}]}