{"_buckets": {"deposit": "f7dfa422-37b2-4a2b-99a8-e226989b3449"}, "_deposit": {"id": "3170", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "3170"}, "status": "published"}, "_oai": {"id": "oai:niigata-u.repo.nii.ac.jp:00003170", "sets": ["454", "489"]}, "item_5_alternative_title_1": {"attribute_name": "その他のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "Crustal Lithology and Stratigraphy of Remnant Arcs induced from Ophiolitic Rocks in the Idonnappu Zone Accretionary Complex (Hokkaido, Japan) : Comparison with Philippine Sea Remnant Arcs"}]}, "item_5_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2003-10", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "5", "bibliographicPageEnd": "780", "bibliographicPageStart": "769", "bibliographicVolumeNumber": "112", "bibliographic_titles": [{"bibliographic_title": "地学雑誌"}, {"bibliographic_title": "地学雑誌", "bibliographic_titleLang": "en"}]}]}, "item_5_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The mid-Cretaceous Oku-Niikappu Dam accretionary complex (ONDC) in the Idonnappu Zone of Hokkaido contains volcanic, plutonic, and ultrarnafic rocks with island-arc chemical features. The volcanic rocks are overlain by radiolarian chert. This stratigraphic succession represents an ancient island arc, in which activity ceased within a pelagic environment prior to accretion to the continental margin. The ophiolitic rocks of the ONDC, which may have comprised upper mantle, arc crust, and cover sediments, are thus regarded as accreted fragments of an intraoceanic remnant arc. Basaltic to andesitic volcanics, gabbroic to tonalitic plutonics, and serpentinite are constituents common to the ONDC remnant arc and equivalent settings in the modern Philippine Sea. They also have a common cover sedimentary sequence, from volcanic basement through volcaniclastic debrites to pelagic sediments. This sequence may record the history from arc activity through back-arc rifting to intraoceanic isolation. Clasts of serpentinite, plutonic, and metamorphic rocks in the volcaniclastic debrites in the ONDC and those from the Daito Ridge in the Philippine Sea imply extensional exhumation of lower crustal and upper mantle rocks during back-arc rifting.", "subitem_description_type": "Abstract"}]}, "item_5_full_name_3": {"attribute_name": "著者別名", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "41206", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Ueda, Hayato"}]}, {"nameIdentifiers": [{"nameIdentifier": "41207", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Miyashita, Sumio"}]}]}, "item_5_publisher_7": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "東京地学協会"}]}, "item_5_select_19": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_5_source_id_11": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00322536", "subitem_source_identifier_type": "NCID"}]}, "item_5_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0022135X", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "植田, 勇人"}], "nameIdentifiers": [{"nameIdentifier": "41204", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "宮下, 純夫"}], "nameIdentifiers": [{"nameIdentifier": "41205", "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": "2019-07-30"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "112_5_769-780.pdf", "filesize": [{"value": "378.7 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 378700.0, "url": {"label": "112_5_769-780.pdf", "url": "https://niigata-u.repo.nii.ac.jp/record/3170/files/112_5_769-780.pdf"}, "version_id": "ea7e7c4a-1f15-4a97-b913-bfca2fdffe50"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "remnant arc", "subitem_subject_scheme": "Other"}, {"subitem_subject": "ophiolite", "subitem_subject_scheme": "Other"}, {"subitem_subject": "back arc rifting", "subitem_subject_scheme": "Other"}, {"subitem_subject": "conglomerate", "subitem_subject_scheme": "Other"}, {"subitem_subject": "crust", "subitem_subject_scheme": "Other"}, {"subitem_subject": "残存島弧", "subitem_subject_scheme": "Other"}, {"subitem_subject": "オフィオライト", "subitem_subject_scheme": "Other"}, {"subitem_subject": "背弧拡大", "subitem_subject_scheme": "Other"}, {"subitem_subject": "礫岩", "subitem_subject_scheme": "Other"}, {"subitem_subject": "地殻", "subitem_subject_scheme": "Other"}]}, "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": "北海道イドンナップ帯付加体中のオフィオライトからみた残存島弧の地殻構成と層序 : フィリピン海残存島弧との比較", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "北海道イドンナップ帯付加体中のオフィオライトからみた残存島弧の地殻構成と層序 : フィリピン海残存島弧との比較"}, {"subitem_title": "北海道イドンナップ帯付加体中のオフィオライトからみた残存島弧の地殻構成と層序 : フィリピン海残存島弧との比較", "subitem_title_language": "en"}]}, "item_type_id": "5", "owner": "1", "path": ["454", "489"], "permalink_uri": "http://hdl.handle.net/10191/18248", "pubdate": {"attribute_name": "公開日", "attribute_value": "2012-06-05"}, "publish_date": "2012-06-05", "publish_status": "0", "recid": "3170", "relation": {}, "relation_version_is_last": true, "title": ["北海道イドンナップ帯付加体中のオフィオライトからみた残存島弧の地殻構成と層序 : フィリピン海残存島弧との比較"], "weko_shared_id": null}