{"created":"2023-07-25T08:11:10.249078+00:00","id":11305,"links":{},"metadata":{"_buckets":{"deposit":"292c9c05-7d7b-4fda-830d-d161c32ee7a7"},"_deposit":{"created_by":18,"id":"11305","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"11305"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00011305","sets":["228:229:5066","37:53"]},"author_link":[],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2012-12-30","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"29","bibliographicPageStart":"19","bibliographicVolumeNumber":"45","bibliographic_titles":[{"bibliographic_title":"鹿児島大学理学部紀要","bibliographic_titleLang":"ja"},{"bibliographic_title":"Reports of the Faculty of Science, Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2012-12-30","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"In the upper and middle reaches of Amori River, the Kakuto Pyroclastic Flow Deposit, the Aira\nBeds 1&2, the Ata Pyroclastic Flow Deposit and the Tsumaya-Ito Pyroclastic Flow Deposits are distributed\nin ascending order. The altitude of top surface of the Kakuto Pyroclastic Flow Deposit becomes higher\ntoward the west in this area. Altitude is about 60 meters above sea level around Kokubu alluvial plain and\nis about 220 meters in the eastern margin of Jusan-tsukabaru plateau though thickness of the pyroclastic\nflow deposit is almost same. This feature described above suggests that a peculiar mode of occurrence of\nthe Kakuto Pyroclastic Flow Deposit coincides with the topography of the erosion surface of the basement\nrocks. On the other hand, the Ito Pyroclastic Flow Deposit fills up in the basin-like erosion surface of the underlying beds and the top surface of the pyroclastic flow deposit is rather flat. In the western and eastern\nparts of studied area the top surface of pyroclastic f?low deposit is preserved and Jusan-tsukabaru and\nHaruyama-bai plateaus are formed. In contrast to this, the pyroclastic flow deposit was eroded by river and\ndeep valleys were cut in the center part of studied area. These valleys generally run in NE-SW and NW-SE\ndirections. From this it may be inferred that they are eroded along tectonic faults.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"13456938","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA11246904","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"454","subitem_subject_scheme":"NDC"}]},"item_7_version_type_14":{"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":"大木, 公彦","creatorNameLang":"ja"},{"creatorName":"OKI, Kimihiko","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"湯浅, 秀隆","creatorNameLang":"ja"},{"creatorName":"YUASA, Hidetaka","creatorNameLang":"en"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-31"}],"displaytype":"detail","filename":"AA11246904_v45_p19-29.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AA11246904_v45_p19-29.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/11305/files/AA11246904_v45_p19-29.pdf"},"version_id":"1d0e0ce6-3843-46cd-bd4e-2b8fcd5bbc66"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Amori River","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Kakuto Pyroclastic Flow","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Ito Pyroclastic Flow","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":"天降川中流・上流域の地形・地質に関する一考察","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"天降川中流・上流域の地形・地質に関する一考察","subitem_title_language":"ja"},{"subitem_title":"Note on topography and geology in the upper and middle reaches of Amori River, South Kyushu, Japan","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["53","5066"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2014-12-22"},"publish_date":"2014-12-22","publish_status":"0","recid":"11305","relation_version_is_last":true,"title":["天降川中流・上流域の地形・地質に関する一考察"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-02-08T04:49:59.928267+00:00"}