{"created":"2023-07-27T07:49:07.810071+00:00","id":24009,"links":{},"metadata":{"_buckets":{"deposit":"ddbc4865-3adb-4aaa-bcb3-a983f62bd5c1"},"_deposit":{"created_by":20,"id":"24009","owners":[20],"pid":{"revision_id":0,"type":"depid","value":"24009"},"status":"published"},"_oai":{"id":"oai:doshisha.repo.nii.ac.jp:00024009","sets":["4251:8138:8139:8140:8156","8:3372:3847:3863"]},"author_link":["18947","21855","21856","21857","21858"],"item_1693811493084":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_1694490770713":{"attribute_name":"権利者情報","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"DA18202107","nameIdentifierScheme":"AID"}],"rightHolderNames":[{"rightHolderLanguage":"ja","rightHolderName":"同志社大学ハリス理化学研究所"},{"rightHolderLanguage":"en","rightHolderName":"Harris Science Research Institute of Doshisha University"}]}]},"item_1_alternative_title_2":{"attribute_name":"その他（別言語等）のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"大阪河内平野の沖積層の特徴","subitem_alternative_title_language":"ja"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-07-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"98","bibliographicPageStart":"88","bibliographicVolumeNumber":"57","bibliographic_titles":[{"bibliographic_title":"同志社大学ハリス理化学研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"The Harris science review of Doshisha University","bibliographic_titleLang":"en"}]}]},"item_1_description_12":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"島弧間盆地である大阪堆積盆の河内平野の地下の最後期更新統から完新統の\"沖積層\"についてその特徴を明らかにした．この地層は20〜30ｍの層厚を有し，4つのユニット，すなわち下位から上位へ最下部礫層，下部砂泥互層，中部海成粘土層，上部砂泥層に区分できる．中部の海成粘土層は陸域にむかってくさび状に分布する．これらの地層区分や分布はわが国の沿岸域の沖積層の典型である．最下部の礫層は河川や扇状地性で，3万年前から1万年前の氷期の低海面期に古大和川や淀川の谷を埋積している．下部の砂泥互層は1万年前から8千年前の後氷期の海進に伴って溺れ谷の河口に堆積したものである．中部の海成粘土層は8千年前から3千年前の高海面期（最高海面期は約5千3百年前）に，河内湾で海成侵食ラビーンメント面上に堆積した泥干潟や内湾泥底の厚い堆積物である．上部砂泥層は3千年前から現在までに臨海扇状地や三角州や海岸などで形成された堆積物である．この中で河内湾における特徴的な堆積相は，厚い海進期の泥干潟の堆積物である．","subitem_description_language":"ja","subitem_description_type":"Abstract"},{"subitem_description":"Geological characteristics of the latest Pleistocene to Holocene \"Chuseki-so\" beneath the Kawachi Plain in the intra-arc Osaka Basin, central Japan were clarified. The strata, which have a total thickness of 20 to 30 m, are divided into four units: lowermost gravel, lower alternation of sand and mud; middle marine clay; and upper sand and mud, in ascending order. The middle marine clay is a wedge-shaped bed that thins landward. These stratigraphic divisions and their distribution are typical of Chuseki-so in coastal areas of Japan. The lowermost gravel consists of fluvial or alluvial fan deposits, which filled in the valleys of the Paleo-Yamato River and the Yodo River during the glacial sea-level lowstand, from about 30,000 to 10,000 cal yr BP. The lower alternation of sand and mud consists of estuarine sediments in the drowned valley, which were deposited during the deglacial transgressive period of 10,000 to 8,000 cal yr BP. The middle marine clay bed, which immediately overlies a marine erosional ravinement surface, consists of thick tidal mud-flat deposits and thin bay-floor mud deposited in Kawachi Bay during the sea-level highstand from 8,000 to 3,000 cal yr BP (period of maximum flooding is about 5,300 cal yr BP). The upper sand and mud are composed of fan-delta, delta, and coastal sediments deposited during the highstand and subsequent regression from 3,000 to 0 cal yr BP. The thick transgressive mud-flat deposit is a characteristic key facies in this Kawachi Bay area.","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_1_description_25":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.14988/pa.2017.0000014612","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_15":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"同志社大学ハリス理化学研究所","subitem_publisher_language":"ja"}]},"item_1_publisher_16":{"attribute_name":"出版者（英）","attribute_value_mlt":[{"subitem_publisher":"Harris Science Research Institute of Doshisha University","subitem_publisher_language":"en"}]},"item_1_relation_24":{"attribute_name":"関連サイト","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_language":"ja","subitem_relation_name_text":"掲載刊行物所蔵情報へのリンク ／ Link to Contents"}],"subitem_relation_type":"isFormatOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doors.doshisha.ac.jp/opac/opac_link/bibid/SB12902196/?lang=0","subitem_relation_type_select":"URI"}}]},"item_1_source_id_17":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"21895937","subitem_source_identifier_type":"PISSN"}]},"item_1_source_id_19":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA12716107","subitem_source_identifier_type":"NCID"}]},"item_1_subject_27":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"456.9163","subitem_subject_scheme":"NDC"}]},"item_1_text_8":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_language":"ja","subitem_text_value":"増田, 富士雄 / 同志社大学理工学部環境システム学科教授"},{"subitem_text_language":"ja","subitem_text_value":"糸本, 夏実 / Faculty of the Science and Engineering, Doshisha University"},{"subitem_text_language":"ja","subitem_text_value":"小川, 和宏 / Faculty of the Science and Engineering, Doshisha University"},{"subitem_text_language":"ja","subitem_text_value":"櫻井, 皆生 / Faculty of the Science and Engineering, Doshisha University"},{"subitem_text_language":"ja","subitem_text_value":"趙, 哲済 / Osaka City Cultural Properties Association"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"open access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_abf2"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"増田, 富士雄","creatorNameLang":"ja"},{"creatorName":"マスダ, フジオ","creatorNameLang":"ja-Kana"},{"creatorName":"Masuda, Fujio","creatorNameLang":"en"}],"nameIdentifiers":[{},{},{},{}]},{"creatorNames":[{"creatorName":"糸本, 夏実","creatorNameLang":"ja"},{"creatorName":"イトモト, ナツミ","creatorNameLang":"ja-Kana"},{"creatorName":"Itomoto, Natsumi","creatorNameLang":"en"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"小川, 和宏","creatorNameLang":"ja"},{"creatorName":"オガワ, カズヒロ","creatorNameLang":"ja-Kana"},{"creatorName":"Ogawa, Kazuhiro","creatorNameLang":"en"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"櫻井, 皆生","creatorNameLang":"ja"},{"creatorName":"サクライ, ミナオ","creatorNameLang":"ja-Kana"},{"creatorName":"Sakurai, Minao","creatorNameLang":"en"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"趙, 哲済","creatorNameLang":"ja"},{"creatorName":"チョウ, テッサイ","creatorNameLang":"ja-Kana"},{"creatorName":"Cho, Chul-jae","creatorNameLang":"en"}],"nameIdentifiers":[{},{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-08-30"}],"displaytype":"detail","filename":"023057020004.pdf","filesize":[{"value":"2.8 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"023057020004.pdf","url":"https://doshisha.repo.nii.ac.jp/record/24009/files/023057020004.pdf"},"version_id":"703062b1-2890-483f-accb-958e6ba3bb3c"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"沖積層","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"河内平野","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"海成粘土層","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"大阪盆地","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"泥干潟堆積物","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"Chuseki-so","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Kawachi Plain","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"marine clay bed","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Osaka Basin","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"tidal flat mud","subitem_subject_language":"en","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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"大阪,河内平野の沖積層の特徴","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"大阪,河内平野の沖積層の特徴","subitem_title_language":"ja"},{"subitem_title":"オオサカ,カワチ ヘイヤ ノ チュウセキソウ ノ トクチョウ","subitem_title_language":"ja-Kana"},{"subitem_title":"Geological characteristics of the latest pleistocene to holocene \"Chuseki-so\" in the Kawachi Plain, Osaka Basin, Japan","subitem_title_language":"en"}]},"item_type_id":"1","owner":"20","path":["3863","8156"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2016-09-02"},"publish_date":"2016-09-02","publish_status":"0","recid":"24009","relation_version_is_last":true,"title":["大阪,河内平野の沖積層の特徴"],"weko_creator_id":"20","weko_shared_id":-1},"updated":"2023-11-30T01:29:11.261326+00:00"}