{"_buckets": {"deposit": "cee0344e-1116-42e5-a35a-cb23f0a833f4"}, "_deposit": {"created_by": 3, "id": "8449", "owners": [3], "pid": {"revision_id": 0, "type": "depid", "value": "8449"}, "status": "published"}, "_oai": {"id": "oai:ir.kagoshima-u.ac.jp:00008449", "sets": ["4578", "116"]}, "author_link": ["75829", "75830", "9935"], "item_6_alternative_title_18": {"attribute_name": "別言語のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "Volcanic islands south of Kyushu, Japan"}]}, "item_6_alternative_title_19": {"attribute_name": "タイトルよみ", "attribute_value_mlt": [{"subitem_alternative_title": "キュウシュウ ナンポウ ノ リトウ ノ カザン"}]}, "item_6_biblio_info_5": {"attribute_name": "収録雑誌名", "attribute_value_mlt": [{"bibliographicPageEnd": "16", "bibliographicPageStart": "11", "bibliographicVolumeNumber": "34", "bibliographic_titles": [{"bibliographic_title": "Nature of Kagoshima"}]}]}, "item_6_date_6": {"attribute_name": "作成日", "attribute_value_mlt": [{"subitem_date_issued_datetime": "2008-03-31"}]}, "item_6_description_4": {"attribute_name": "要約(Abstract)", "attribute_value_mlt": [{"subitem_description": "The volcanic arc off Kyushu, which stretches some 1000 km southwestward, is associated with an active back-arc basin, the Okinawa trough. The volcanoes on these southern islands are, from north to south, Kikai caldera (Satsuma-Iojima and Showa-Iojima formed during the 1934-1935 submarine eruption), Kuchinoerabujima, Kuchinoshima, Nakanoshima, Suwanosejima, Akusekijima, Yokoatejima, Io-Torishima, and a submarine volcano NNE of Iriomotejima. The edifices and mode of eruptions of these volcanoes are quite different from each other. There are two submerged calderas; Kikai caldera and an unnamed caldera around Yokoatejima. Kikai caldera is one of the youngest calderas in Japan. Its latest caldera-forming eruption occurred approximately 7300 years ago, destructive pyroclastic flows reaching the southern parts of Kagoshima. It is widely believed that the Jomon culture in southern Kagoshima completely perished during this eruption. The associated volcanic ash spread all over Japan, and has still been preserved in the soil layers in many places. Although the erupted rocks of these volcanoes consist predominantly of pyroxene andesite, Kuchinoshima volcano erupted mainly hornblende andesite. Kikai caldera only erupted magmas of bimodal composition (basalt and rhyolite).", "subitem_description_type": "Other"}]}, "item_6_full_name_2": {"attribute_name": "著者よみ", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "75829", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "コバヤシ, テツオ"}]}]}, "item_6_full_name_3": {"attribute_name": "別言語の著者", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "75830", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "KOBAYASHI, Tetsuo"}]}]}, "item_6_publisher_23": {"attribute_name": "公開者・出版者", "attribute_value_mlt": [{"subitem_publisher": "鹿児島県自然愛護協会"}]}, "item_6_rights_12": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "鹿児島県自然愛護協会"}]}, "item_6_source_id_7": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "18827551", "subitem_source_identifier_type": "ISSN"}]}, "item_6_source_id_9": {"attribute_name": "NII書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AA12599025", "subitem_source_identifier_type": "NCID"}]}, "item_6_subject_15": {"attribute_name": "NDC", "attribute_value_mlt": [{"subitem_subject": "453", "subitem_subject_scheme": "NDC"}]}, "item_6_text_30": {"attribute_name": "NIIタイプ", "attribute_value_mlt": [{"subitem_text_value": "Journal Article"}]}, "item_6_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": "小林, 哲夫"}], "nameIdentifiers": [{"nameIdentifier": "9935", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "1000070112430", "nameIdentifierScheme": "NRID", "nameIdentifierURI": " "}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2016-10-28"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "AA12599025_v34_p11-16.pdf", "filesize": [{"value": "535.9 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 535900.0, "url": {"label": "AA12599025_v34_p11-16.pdf", "url": "https://ir.kagoshima-u.ac.jp/record/8449/files/AA12599025_v34_p11-16.pdf"}, "version_id": "032341b0-cb24-44fc-9692-53fc505c465d"}]}, "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": "九州南方の離島の火山", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "九州南方の離島の火山"}]}, "item_type_id": "6", "owner": "3", "path": ["116", "4578"], "permalink_uri": "http://hdl.handle.net/10232/18060", "pubdate": {"attribute_name": "公開日", "attribute_value": "2015-01-13"}, "publish_date": "2015-01-13", "publish_status": "0", "recid": "8449", "relation": {}, "relation_version_is_last": true, "title": ["九州南方の離島の火山"], "weko_shared_id": 3}