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Orientation data of 203–258 grains from each of four rock specimens fit the model well, suggesting a useful analytical technique with three advantages: (1) confidence in whether a metamorphic tectonite has a mineral lineation can be determined using a  χ  2 -test, (2) the orientation of the mineral lineation can be represented by the mean direction (   θ     ) with a specified confidence interval, and (3) the degree of preferred dimensional orientation of grains can be quantified by the concentration parameter (   κ     )."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011145589801601","@type":"Researcher","foaf:name":[{"@value":"Toshiaki Masuda"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011145589801602","@type":"Researcher","foaf:name":[{"@value":"Yasuo Kugimiya"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011145589801603","@type":"Researcher","foaf:name":[{"@value":"Itsuko Aoshima"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011145589801600","@type":"Researcher","foaf:name":[{"@value":"Yuko Hara"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011145589801604","@type":"Researcher","foaf:name":[{"@value":"Hideaki Ikei"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1999-04","prism:volume":"21","prism:number":"4","prism:startingPage":"467","prism:endingPage":"472"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S019181419900005X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S019181419900005X?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2025-09-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050288525443132800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A kinetic model of oriented nucleation under nonhydrostatic stress: Implications for the preferred orientation of columnar and platy minerals in metamorphic rocks"},{"@value":"A kinetic model of oriented nucleation under nonhydrostatic stress: Imprecations for the preferred orientation of columnar and platy minerals in metamorphic rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916180992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"E–W extension at 19 Ma in the Kung Co area, S. 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