{"created":"2023-07-25T10:59:40.306875+00:00","id":1391,"links":{},"metadata":{"_buckets":{"deposit":"fd27b7a7-eb4a-41b7-b429-db6d0945f7b7"},"_deposit":{"created_by":4,"id":"1391","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"1391"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00001391","sets":["1:356:379"]},"author_link":["46163","58080","58081"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1982-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"215","bibliographicPageStart":"207","bibliographicVolumeNumber":"25","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Fujimura, Akio","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Kato, Manabu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Kumazawa, Mineo","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"The preferred orientation of phyllosilicates in two Yamato chondrites (C2) has been examined by means of X-ray pole figure goniometry. Both C2 chondrites show almost the same textural features under the optical microscope as those of Murchison (C2) studied previously. In Yamato-74642,however, X-ray diffraction intensity of phyllosilicates is extremely weak and no information on the oriented texture could be obtained. Hydrous minerals in Yamato-74642 have probably been altered by some thermal event. Yamato-74662 possesses a weak but clear preferred orientation of phyllosilicates, indicating evidence of anisotropic deformation. The magnitude of plastic deformation is estimated to be in the order of 10%.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Department of Earth Sciences, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Department of Earth Sciences, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Department of Earth Sciences, Nagoya University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1982-12-01"}],"displaytype":"detail","filename":"KJ00000012025.pdf","filesize":[{"value":"948.9 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000012025","url":"https://nipr.repo.nii.ac.jp/record/1391/files/KJ00000012025.pdf"},"version_id":"1cd56bd0-6cc7-4836-a20b-a4d1f9393bb9"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Preferred orientation of phyllosilicates in Yamato-74642 and -74662, in relation to deformation of C2 chondrites","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Preferred orientation of phyllosilicates in Yamato-74642 and -74662, in relation to deformation of C2 chondrites","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["379"],"pubdate":{"attribute_name":"公開日","attribute_value":"1982-12-01"},"publish_date":"1982-12-01","publish_status":"0","recid":"1391","relation_version_is_last":true,"title":["Preferred orientation of phyllosilicates in Yamato-74642 and -74662, in relation to deformation of C2 chondrites"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:51:04.380685+00:00"}