{"created":"2023-07-27T06:58:37.007049+00:00","id":57364,"links":{},"metadata":{"_buckets":{"deposit":"1e0e44e3-a43c-43a3-a92b-252c20486ed0"},"_deposit":{"created_by":18,"id":"57364","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"57364"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00057364","sets":["934:935:937"]},"author_link":["79877","2446"],"item_4_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2018-08-15","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"8","bibliographicPageEnd":"601","bibliographicPageStart":"593","bibliographicVolumeNumber":"124","bibliographic_titles":[{"bibliographic_title":"地質学雑誌"},{"bibliographic_title":"The Journal of the Geological Society of Japan","bibliographic_titleLang":"en"}]}]},"item_4_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Umino, Susumu"}],"nameIdentifiers":[{},{}]}]},"item_4_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"100周年以降の25年間は日本の地質学者が広く海外に活躍の場を拡げるとともに，新たな分析機器の導入や解析手法の開発により，オフィオライトを構成するマントルカンラン岩の精密な上昇プロセスやマントル中のマグマの移動・反応プロセス，マントルの流動・変形機構，マントル岩中の微小包有物の同定・分析などが勢力的に進められた．また，フィールド地質学の分野でも，詳細な地質調査に基づいて海洋地殻の形成プロセスや始生代の海洋地殻層序の復元などが行われた．本小論ではこれらの日本人によって行われた海外のオフィオライト研究のうち，世界で最も規模が大きく保存状態がよいとされるオマーン，島弧下マントルが露出するミルディータ，リサイクルしたスラブ由来の超高圧鉱物を含むルオブサ，世界で最も新しいチモールとタイタオ，世界最古の付加体からなるイスアとピルバラの各オフィオライトについて紹介した．","subitem_description_type":"Abstract"},{"subitem_description":"The last quarter-century has been a period of worldwide study of ophiolites by Japanese geologists, as described in this paper. The Oman Mountains expose the world largest and best preserved ophiolite that provides insights into crustal and mantle processes below a fast-spreading system and transformation of oceanic lithosphere to subarc crust and mantle. The Mirdita Ophiolite exposes mantle peridotites covered by mid-ocean ridge basalt (MORB) and arc tholeiitic to boninitic lavas, recording the transition from a spreading to a subduction environment. The Luobusa Ophiolite is well-known for its ultrahigh-pressure minerals such as coesite and micro-diamond inclusions in chromite, considered to represent recycling of subducted slab deep into the mantle at >380 km depth. The 5-3 Ma ophiolites in the Timor and Tanimbar Islands are the world's youngest, and are considered to have formed the forearc crust and mantle that collided with and obducted onto the northern edge of the Australian continent. Volcanic rocks have geochemical characteristics that are intermediate between arc tholeiite and MORB, although the mantle peridotites are not cognate with the overlying volcanic rocks. Another young ophiolite (6-5 Ma) of Taitao, southern Chile, was part of the eastern limb of the Chile Ridge, which was subducted and accreted in an accretionary complex along the western coast of Chile. In spite of their mid-ocean-ridge origin, the lavas and sheeted dikes of ophiolite have geochemical characteristics typical of arc magmas. Isua and Pilbara contain the world's oldest accretionary complexes consisting of superposed slices of oceanic crust that form a duplex structure, indicating the beginning of plate tectonics in the early Archean.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学理工研究域自然システム学系","subitem_description_type":"Other"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00063634","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"日本地質学会 The Geological Society of Japan"}]},"item_4_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.5575/geosoc.2018.0002","subitem_relation_type_select":"DOI"}}]},"item_4_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"http://www.geosociety.jp"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://www.geosociety.jp","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/","subitem_relation_type_select":"URI"}}]},"item_4_rights_23":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"Copyright © 日本地質学会 The Geological Society of Japan"}]},"item_4_source_id_11":{"attribute_name":"NCID","attribute_value_mlt":[{"subitem_source_identifier":"AN00141768","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0016-7630","subitem_source_identifier_type":"ISSN"},{"subitem_source_identifier":" 1349-9963","subitem_source_identifier_type":"ISSN"}]},"item_4_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"海野, 進"}],"nameIdentifiers":[{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2021-08-30"}],"displaytype":"detail","filename":"SC-PR-UMINO-S-593.pdf","filesize":[{"value":"928.1 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-UMINO-S-593.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/57364/files/SC-PR-UMINO-S-593.pdf"},"version_id":"88570c01-2519-4df4-b0b4-50e18820e994"}]},"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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"日本人による世界のオフィオライト研究","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"日本人による世界のオフィオライト研究"},{"subitem_title":"An overview of world ophiolite studies by Japanese researchers","subitem_title_language":"en"}]},"item_type_id":"4","owner":"18","path":["937"],"pubdate":{"attribute_name":"公開日","attribute_value":"2021-08-30"},"publish_date":"2021-08-30","publish_status":"0","recid":"57364","relation_version_is_last":true,"title":["日本人による世界のオフィオライト研究"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T15:00:47.083708+00:00"}