{"created":"2025-02-21T05:15:00.595972+00:00","id":2009949,"links":{},"metadata":{"_buckets":{"deposit":"ea08ecfd-706c-4f68-91bd-d0de05e13fac"},"_deposit":{"created_by":41,"id":"2009949","owners":[41],"pid":{"revision_id":0,"type":"depid","value":"2009949"},"status":"published"},"_oai":{"id":"oai:hiroshima.repo.nii.ac.jp:02009949","sets":["1730444907710"]},"author_link":[],"item_1617186331708":{"attribute_name":"Title","attribute_value_mlt":[{"subitem_title":"Contact Metamorphism in the Area around the Lower Reaches of the Oze River, Southwest Japan","subitem_title_language":"en"}]},"item_1617186419668":{"attribute_name":"Creator","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Hayashi, Takehiro","creatorNameLang":"en"}],"familyNames":[{"familyName":"Hayashi","familyNameLang":"en"}],"givenNames":[{"givenName":"Takehiro","givenNameLang":"en"}]},{"creatorNames":[{"creatorName":"Tatsukami, Minako","creatorNameLang":"en"}],"familyNames":[{"familyName":"Tatsukami","familyNameLang":"en"}],"givenNames":[{"givenName":"Minako","givenNameLang":"en"}]},{"creatorNames":[{"creatorName":"Yoshino, Gensei","creatorNameLang":"en"}],"familyNames":[{"familyName":"Yoshino","familyNameLang":"en"}],"givenNames":[{"givenName":"Gensei","givenNameLang":"en"}]}]},"item_1617186476635":{"attribute_name":"Access Rights","attribute_value_mlt":[{"subitem_access_right":"open access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_abf2"}]},"item_1617186609386":{"attribute_name":"Subject","attribute_value_mlt":[{"subitem_subject":"contact metamorphism","subitem_subject_scheme":"Other"},{"subitem_subject":"Hiroshima granite","subitem_subject_scheme":"Other"},{"subitem_subject":"cordierite","subitem_subject_scheme":"Other"},{"subitem_subject":"450","subitem_subject_scheme":"NDC"}]},"item_1617186626617":{"attribute_name":"Description","attribute_value_mlt":[{"subitem_description":"In the studied area, through the field and microscopic studies in detail, based upon variations in the mineral assemblage, progressive sequence of mudstone in the studied have been divided into 5 zones, in order of increasing metamorphism; Zone I characterized by chlorite, Zone II by yellow-colored biotite in pleochroism, the Zone III by brown-colored biotite in pleochroism, the Zone IV by cordierite and the Zone V by cordierite replaced into assemblage of chlorite and mica minerals. Distribution of the contact aureole can be regarded to reflect on both the structure of the granite body occurring in a sheet-like body below the land surface, and the movement of actual Otake Fault. The replaced cordierite appear in Zone V can be regarded to formed through hydrothermal reaction in the latest stage of the intrusion process of Hiroshima granite.","subitem_description_language":"en"}]},"item_1617186643794":{"attribute_name":"Publisher","attribute_value_mlt":[{"subitem_publisher":"広島大学学校教育学部"}]},"item_1617186702042":{"attribute_name":"Language","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_1617186920753":{"attribute_name":"Source Identifier","attribute_value_mlt":[{"subitem_source_identifier":"0387-4869","subitem_source_identifier_type":"ISSN"},{"subitem_source_identifier":"AN00213348","subitem_source_identifier_type":"NCID"}]},"item_1617187024783":{"attribute_name":"Page Start","attribute_value_mlt":[{"subitem_start_page":"69"}]},"item_1617187056579":{"attribute_name":"Bibliographic Information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1998-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"78","bibliographicPageStart":"69","bibliographicVolumeNumber":"20","bibliographic_titles":[{"bibliographic_title":"広島大学学校教育学部紀要. 第二部"},{"bibliographic_title":"Bulletin of the Faculty of School Education, Hiroshima University. Part II"}]}]},"item_1617258105262":{"attribute_name":"Resource Type","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_1617265215918":{"attribute_name":"Version Type","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_1617605131499":{"attribute_name":"File","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","date":[{"dateType":"Available","dateValue":"2023-03-18"}],"displaytype":"simple","filename":"BullFacSchEduc-HiroshimaUniv-Pt2_20_69.pdf","filesize":[{"value":"1.5 MB"}],"mimetype":"application/pdf","url":{"objectType":"fulltext","url":"https://hiroshima.repo.nii.ac.jp/record/2009949/files/BullFacSchEduc-HiroshimaUniv-Pt2_20_69.pdf"},"version_id":"3702c3fc-e2bb-4e32-8cc9-e33878fab023"}]},"item_1732771732025":{"attribute_name":"旧ID","attribute_value":"27368"},"item_title":"Contact Metamorphism in the Area around the Lower Reaches of the Oze River, Southwest Japan","item_type_id":"40003","owner":"41","path":["1730444907710"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-03-18"},"publish_date":"2023-03-18","publish_status":"0","recid":"2009949","relation_version_is_last":true,"title":["Contact Metamorphism in the Area around the Lower Reaches of the Oze River, Southwest Japan"],"weko_creator_id":"41","weko_shared_id":-1},"updated":"2025-02-22T06:39:56.095266+00:00"}