{"created":"2023-07-27T06:26:53.120013+00:00","id":10793,"links":{},"metadata":{"_buckets":{"deposit":"c7c8e67c-6ee7-4fe1-bef4-34ef826db833"},"_deposit":{"created_by":3,"id":"10793","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"10793"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00010793","sets":["934:935:937"]},"author_link":["1509","51","66758"],"item_4_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1995-02-05","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"49","bibliographicPageStart":"41","bibliographicVolumeNumber":"90","bibliographic_titles":[{"bibliographic_title":"岩石鉱物鉱床学会誌 = The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists"}]}]},"item_4_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Peridotite xenoliths and essential ejecta from the Ninomegata crater of the Megata volcano, Northeast Japan arc, were described in detail. The peridotites have a wide spread of Cr # (=Cr/(Cr+Al) atomic ratio) of chromian spinel, from 0.10 to 0.45, almost comparable with but slightly lower than that of the Ichinomegata peridotites. They often have a secondary hydrous mineral, pargasite, replacing primary minerals. One of lherzolites has several small veinlets of hornblendite. The amount of pargasite is far smaller than that from the Ichinomegata peridotites. The Ninomegata peridotite xenoliths, therefore, preserve characteristics of primary mantle restite; they are in the olivine-spinel mantle array and the Fe3+/(Cr+Al+Fe3+) atomic ratio of chromian spinel is not high (<0.05). Petrographical and/or chemical variety of peridotite xenoliths decreases from Ichinomegata to Sannomegata through Ninomegata within the Megata volcano. The essential ejecta from the Ninomegata crater has almost the same characteristics as those from Ichinomegata in terms of petrography and bulk chemistry.","subitem_description_type":"Abstract"}]},"item_4_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Japan Association of Mineralogical Sciences = 日本鉱物科学会"}]},"item_4_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.2465/ganko.90.41","subitem_relation_type_select":"DOI"}}]},"item_4_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://jams.la.coocan.jp/","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.jstage.jst.go.jp/article/ganko/90/2/90_2_41/_pdf","subitem_relation_type_select":"URI"}}]},"item_4_rights_23":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"Copyright © Japan Association of Mineralogical Sciences 日本鉱物科学会"}]},"item_4_source_id_11":{"attribute_name":"NCID","attribute_value_mlt":[{"subitem_source_identifier":"AN10047992","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0914-9783","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":"阿部, なつ江"}],"nameIdentifiers":[{"nameIdentifier":"1509","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"80302933","nameIdentifierScheme":"e-Rad","nameIdentifierURI":"https://kaken.nii.ac.jp/ja/search/?qm=80302933"},{"nameIdentifier":"80302933","nameIdentifierScheme":"金沢大学研究者情報","nameIdentifierURI":"http://ridb.kanazawa-u.ac.jp/public/detail.php?kaken=80302933"},{"nameIdentifier":"80302933","nameIdentifierScheme":"研究者番号","nameIdentifierURI":"https://nrid.nii.ac.jp/nrid/1000080302933"}]},{"creatorNames":[{"creatorName":"荒井, 章司"}],"nameIdentifiers":[{"nameIdentifier":"51","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"20107684","nameIdentifierScheme":"e-Rad","nameIdentifierURI":"https://kaken.nii.ac.jp/ja/search/?qm=20107684"},{"nameIdentifier":"20107684","nameIdentifierScheme":"金沢大学研究者情報","nameIdentifierURI":"http://ridb.kanazawa-u.ac.jp/public/detail.php?kaken=20107684"},{"nameIdentifier":"20107684","nameIdentifierScheme":"研究者番号","nameIdentifierURI":"https://nrid.nii.ac.jp/nrid/1000020107684"}]},{"creatorNames":[{"creatorName":"二ノ宮, 淳"}],"nameIdentifiers":[{"nameIdentifier":"66758","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"9999-12-31"}],"displaytype":"detail","filename":"SC-PR-ARAI-S-41.pdf","filesize":[{"value":"2.4 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"SC-PR-ARAI-S-41.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/10793/files/SC-PR-ARAI-S-41.pdf"},"version_id":"acc24a3e-a60c-4727-969c-e646eee5186a"}]},"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":"東北日本弧, 二ノ目潟かんらん岩捕獲岩および本質噴出物について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"東北日本弧, 二ノ目潟かんらん岩捕獲岩および本質噴出物について"},{"subitem_title":"Peridotite xenoliths and essential ejecta from the Ninomegata crater, the Northeastern Japan arc","subitem_title_language":"en"}]},"item_type_id":"4","owner":"3","path":["937"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-11-09"},"publish_date":"2017-11-09","publish_status":"0","recid":"10793","relation_version_is_last":true,"title":["東北日本弧, 二ノ目潟かんらん岩捕獲岩および本質噴出物について"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2024-06-20T05:54:54.079625+00:00"}