{"created":"2023-07-25T08:03:01.418201+00:00","id":892,"links":{},"metadata":{"_buckets":{"deposit":"a42f6fcb-bb08-4f2a-bcab-21690c867dc1"},"_deposit":{"created_by":3,"id":"892","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"892"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00000892","sets":["228:256:5412","31:32:93:94"]},"author_link":["5590","109611","109609","109608","109612","109610"],"item_7_alternative_title_18":{"attribute_name":"別言語のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Paleo-geothermal Systems in Island-arc Settings of the Western Pacific Rim"}]},"item_7_alternative_title_19":{"attribute_name":"タイトルよみ","attribute_value_mlt":[{"subitem_alternative_title":"ナンポウ トウコ ノ コチネツケイ"}]},"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicPageEnd":"86","bibliographicPageStart":"71","bibliographicVolumeNumber":"11","bibliographic_titles":[{"bibliographic_title":"南方海域調査研究報告=Occasional Papers"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1987-07-25"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"An active high temperature geothermal system consists typically of a magmatic heat\nsource, water to tramsport the heat, and fractures or permeable zones where the water\nflows. When the heat source cools down and the geothermal system becomes inactive,\nwe call this a paleo-geothermal system or fossil geothermal system.\nGold is often transported by ascending waters in the high temperature geothermal\nsystem related with volcanic activities. The upper level of the system, at a depth of\naround 400m or less, is a favorable site of gold deposition. Therefore, epithermal gold\ndeposits and their environments correspond to the paleogeothermal systems, of which\nhigh level portions are often eroded away.\nThere are many active- and paleo-geothermal systems in island-arc settings of the\nwestern Pacific rim and adjacent regions. Representative gold deposits are: Taio,\nKushikino, Hishikari and Iwato in Kyushu, Japan; Chinkuashih in Taiwan; Acupan-\nAntamok in the Philippines; Lebong Donok and Lebong Tandai in Sumatra, Indonesia;\nWau in Papua New Guinea; Mavu in the Solomon Islands; Vatukoula and Mt.Kasi in\nFiji; and Waihi in New Zealand.\nThese late Cenozoic epithermal gold regions have several characteristics. (1) Volcanic\nactivities started less than 15-16 million years ago and continued to the late Quaternary.\n(2) Igneous rocks related to the gold mineralization are predominantly dacite or hornblende andesite of the calc-alkalic series. Volcanic rocks of the alkalic series, however, host\nsome of the gold deposits. (3) The site of the gold deposits are restricted to within 8km (usually 4km) of the center of volcanic activity. (4) Two types of gold deposits are\nrecognized, the quartz-adularia veins usually with Mn-carbonates, and those in massive silicified rocks.\nBasements consist of a thick sedimentary sequence in the case of Kyushu, Japan and\nNew Zealand; and probably of oceanic crust in the case of Fiji. Porphyry copper deposits occur intimately with gold deposits in the Philippines and Papua New Guinea\nbut not in Kyushu.","subitem_description_type":"Other"}]},"item_7_full_name_2":{"attribute_name":"著者よみ","attribute_value_mlt":[{"nameIdentifiers":[{}],"names":[{"name":"イザワ, エイジ"}]},{"nameIdentifiers":[{}],"names":[{"name":"ウラシマ, ユキトシ"}]}]},"item_7_full_name_3":{"attribute_name":"別言語の著者","attribute_value_mlt":[{"nameIdentifiers":[{}],"names":[{"name":"IZAWA, Eiji"}]},{"nameIdentifiers":[{}],"names":[{"name":"URASHIMA, Yukitoshi"}]}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学"}]},"item_7_relation_32":{"attribute_name":"関連（relation）","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16098"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16099"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16100"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16101"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16102"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16103"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16104"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16106"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16107"}]},{"subitem_relation_name":[{"subitem_relation_name_text":"http://hdl.handle.net/10232/16108"}]}]},"item_7_relation_33":{"attribute_name":"関連（isVersionOf）","attribute_value_mlt":[{"subitem_relation_type":"isVersionOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16097","subitem_relation_type_select":"URI"}}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"02892707","subitem_source_identifier_type":"ISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN10030752","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"450","subitem_subject_scheme":"NDC"}]},"item_7_text_24":{"attribute_name":"公開者よみ","attribute_value_mlt":[{"subitem_text_value":"カゴシマ ダイガク"}]},"item_7_text_25":{"attribute_name":"公開者別名","attribute_value_mlt":[{"subitem_text_value":"Kagoshima University"}]},"item_7_text_44":{"attribute_name":"備考","attribute_value_mlt":[{"subitem_text_value":"Title page: http://hdl.handle.net/10232/16097, はじめに: http://hdl.handle.net/10232/16098, 開会あいさつ: http://hdl.handle.net/10232/16099, 目次: http://hdl.handle.net/10232/16100本文: http://hdl.handle.net/10232/16101, http://hdl.handle.net/10232/16102, http://hdl.handle.net/10232/16103, http://hdl.handle.net/10232/16104, http://hdl.handle.net/10232/16106閉会あいさつ: http://hdl.handle.net/10232/16107, 菱刈鉱床見学会: http://hdl.handle.net/10232/16108"}]},"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":"井沢, 英二"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"浦島, 幸世"}],"nameIdentifiers":[{},{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-27"}],"displaytype":"detail","filename":"AN10030752_v11_p71-86.pdf","filesize":[{"value":"4.2 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AN10030752_v11_p71-86.pdf","url":"https://ir.kagoshima-u.ac.jp/record/892/files/AN10030752_v11_p71-86.pdf"},"version_id":"84bf5239-b18f-4502-ab68-b5e9d784b3c4"}]},"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":"南方島弧の古地熱系","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"南方島弧の古地熱系"}]},"item_type_id":"7","owner":"3","path":["94","5412"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-06-08"},"publish_date":"2015-06-08","publish_status":"0","recid":"892","relation_version_is_last":true,"title":["南方島弧の古地熱系"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2023-09-12T06:34:56.460656+00:00"}