{"created":"2023-06-19T07:46:21.198914+00:00","id":159,"links":{},"metadata":{"_buckets":{"deposit":"f9cd4b89-b507-424e-9429-d9ed9fab76b2"},"_deposit":{"created_by":15,"id":"159","owners":[15],"pid":{"revision_id":0,"type":"depid","value":"159"},"status":"published"},"_oai":{"id":"oai:cis.repo.nii.ac.jp:00000159","sets":["3:18"]},"author_link":["705"],"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2015-02-28","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"8","bibliographicPageEnd":"56","bibliographicPageStart":"51","bibliographic_titles":[{"bibliographic_title":"千葉科学大学紀要"},{"bibliographic_title":"The University Bulletin of Chiba Institute of Science","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"　香川県西部，鮮新̶更新統三豊層群財田層には，もとの円磨された面ときめの粗い破断面を持ち，2つの面を画する陵がシャープな礫が多量に含まれ，本報告ではそれを破断円礫と呼ぶ．そのような破断円礫は財田層中の礫全体の31 %を占め，現河床堆積物中の割合と比べてきわめて高い．財田層中の破断円礫は，断層運動による円礫の破断とその後の流水による運搬・再堆積によるものと考えられる．陵がシャープな破断円礫が地層中に多数認められた場合には，その近傍に断層が存在し，地層の堆積と同時に活動していた可能性が高い．","subitem_description_type":"Abstract"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"千葉科学大学"}]},"item_10002_relation_12":{"attribute_name":"論文ID（NAID）","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"40020459882","subitem_relation_type_select":"NAID"}}]},"item_10002_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA1230240X","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1882-3505","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"植木, 岳雪"},{"creatorName":"ウエキ, タケユキ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"705","nameIdentifierScheme":"WEKO"},{"nameIdentifier":" 9000291613727","nameIdentifierScheme":"CiNii ID","nameIdentifierURI":"http://ci.nii.ac.jp/nrid/ 9000291613727"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2015-07-03"}],"displaytype":"detail","filename":"k08-ronbun06.pdf","filesize":[{"value":"756.6 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"k08-ronbun06.pdf","url":"https://cis.repo.nii.ac.jp/record/159/files/k08-ronbun06.pdf"},"version_id":"5467ae1a-b90a-48a9-a363-0bd0cb5e4542"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"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":"香川県西部、鮮新-更新統三豊層群中の破断円礫の成因とテクトニックな意義","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"香川県西部、鮮新-更新統三豊層群中の破断円礫の成因とテクトニックな意義"},{"subitem_title":"Broken rounds from the Plio-Pleistocene Mitoyo Group, in western Kagawa Prefecture, southwest Japan, and their tectonic implication","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"15","path":["18"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-07-03"},"publish_date":"2015-07-03","publish_status":"0","recid":"159","relation_version_is_last":true,"title":["香川県西部、鮮新-更新統三豊層群中の破断円礫の成因とテクトニックな意義"],"weko_creator_id":"15","weko_shared_id":-1},"updated":"2023-06-19T07:56:06.956734+00:00"}