{"created":"2023-07-25T08:11:10.205144+00:00","id":11304,"links":{},"metadata":{"_buckets":{"deposit":"3746e684-7067-4c96-b82b-159c9a530a59"},"_deposit":{"created_by":18,"id":"11304","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"11304"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00011304","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":"18","bibliographicPageStart":"1","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":"Lacustrine sediment, unconformably overlies the late Pleistocene Kariya Lava and overlain by the\nAta Pyroclastic Flow Deposit is exposed in the wall area of Ata Caldera so called, Ibusuki City. It was\nnamed the Horekizon Formation by authors. This formation characteristically contains a pyroclastic\nmaterial and divided into three horizons based on their lithofacies. The presence of lacustrine sediment in\nthe caldera wall area suggests that caldera area was mountain before collapse of Ata caldera. Thirteen\nground layers are observed in the Ata Pyroclastic Flow Deposit in Horekizon area. Based on the vertical\nchange of lithofacies of the Ata pyroclastic flow deposit, a plinian eruption, twelve small and medium\npyroclastic flow eruptions, three gigantic pyroclastic flow eruptions and two small pyroclastic flow eruptions are recognized in ascending order. A ground layer in the lower Ata Pyroclastic Flow Deposit contains\nboulder reach a maximum diameter of 1.3 meters and a ground layer in the middle Ata Pyroclastic Flow\nDeposit contains lithic clasts of granite, mudstone and silicified rocks. The lithic clasts in the ground layers\nare presumed to have been derived from the late Pleistocene andesite. The occurrence of the Horekizon\nFormation and the Ata Pyroclastic Flow Deposit support the idea that source of the Ata Pyroclastic Flow\nDeposit is situated at southward near Horekizon area.","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":"山下, 大輔","creatorNameLang":"ja"},{"creatorName":"YAMASHITA, Daisuke","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"大木, 公彦","creatorNameLang":"ja"},{"creatorName":"OKI, Kimihiko","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_p1-18.pdf","filesize":[{"value":"1.7 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AA11246904_v45_p1-18.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/11304/files/AA11246904_v45_p1-18.pdf"},"version_id":"60478ecb-7edf-43e6-a3cb-dcd2bb809cf2"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Ata Pyroclastic Flow Deposit","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Horekizon Formation","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Ata caldera","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"ground layer","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":"指宿市池田堀切園に分布する堀切園層と阿多火砕流堆積物の腑存状況","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"指宿市池田堀切園に分布する堀切園層と阿多火砕流堆積物の腑存状況","subitem_title_language":"ja"},{"subitem_title":"Peculiar mode of occurrence of the Horekizon Formation and the Ata Pyroclastic Flow Deposit distributed in Ikeda-Horekizon, Ibusuki City, 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":"11304","relation_version_is_last":true,"title":["指宿市池田堀切園に分布する堀切園層と阿多火砕流堆積物の腑存状況"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-02-08T04:50:00.182432+00:00"}