{"created":"2023-05-15T13:30:05.627634+00:00","id":182,"links":{},"metadata":{"_buckets":{"deposit":"87f21988-ec01-4e91-a784-931398b4bb0d"},"_deposit":{"created_by":5,"id":"182","owners":[5],"pid":{"revision_id":0,"type":"depid","value":"182"},"status":"published"},"_oai":{"id":"oai:mfri.repo.nii.ac.jp:00000182","sets":["14:25"]},"author_link":["319","318","320","317"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2012-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"38","bibliographicPageStart":"25","bibliographicVolumeNumber":"6","bibliographic_titles":[{}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"　富士山東麓の太郎坊、幕岩付近には、宝永噴火などによるスコリアなどが厚く堆積している。このスコリアなどの中に新富士火山の溶岩が点在している。この溶岩は、幕岩地域だけに小分布する幕岩溶岩Ⅰ～Ⅲと周辺地域に広く分布する三島溶岩、日本ランド溶岩などの溶岩に対比されていた。しかし研究者によりその分布や溶岩対比が異なっていた。調査の結果、 溶岩の詳細が明らかになり、周辺地域に広く分布する溶岩との対比が不可能であることがわかった。このため、新たに、新富士火山旧期の砂沢溶岩Ⅰと中期の砂沢溶岩Ⅱ、新期の砂沢溶岩Ⅲ～Ⅵとアザミ塚・胎内溶岩と再定義することを提案する。","subitem_description_type":"Abstract"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"富士山科学研究所"}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1881-7564","subitem_source_identifier_type":"ISSN"}]},"item_10001_version_type_20":{"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":"山本, 玄珠"},{"creatorName":"ヤマモト, ゲンジュ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"317","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"北垣, 敏明"},{"creatorName":"キタガキ, トシアキ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"318","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"YAMAMOTO, Genjyu","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"319","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"KITAGAKI, Toshiaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"320","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":"2022-03-22"}],"displaytype":"detail","filename":"MFR_No06_p25_p38.pdf","filesize":[{"value":"1.4 MB"}],"format":"application/pdf","license_note":"Copyright (c) Mount Fuji Research Institute, Yamanashi Prefectural Government.\n","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"富士山研究　第6巻25～38頁","url":"https://mfri.repo.nii.ac.jp/record/182/files/MFR_No06_p25_p38.pdf"},"version_id":"b4a7c4f9-b170-4082-a9fe-af12681eda0a"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"溶岩層序","subitem_subject_scheme":"Other"},{"subitem_subject":"砂沢溶岩","subitem_subject_scheme":"Other"},{"subitem_subject":"須山胎内溶岩","subitem_subject_scheme":"Other"},{"subitem_subject":"富士火山東部","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":"富士火山の幕岩の新富士火山溶岩について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"富士火山の幕岩の新富士火山溶岩について"},{"subitem_title":"On some lava fl ows from Sin-Fuji (Younger Fuji) Volcano in Makuiwa area of Mt. Fuji","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"5","path":["25"],"pubdate":{"attribute_name":"公開日","attribute_value":"2022-03-22"},"publish_date":"2022-03-22","publish_status":"0","recid":"182","relation_version_is_last":true,"title":["富士火山の幕岩の新富士火山溶岩について"],"weko_creator_id":"5","weko_shared_id":-1},"updated":"2023-05-15T13:36:46.785807+00:00"}