{"created":"2023-07-25T08:06:27.057553+00:00","id":5220,"links":{},"metadata":{"_buckets":{"deposit":"13c22e44-c040-4825-befd-a7d2ba8e2fe1"},"_deposit":{"created_by":18,"id":"5220","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"5220"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00005220","sets":["228:256:5412","31:32:93:94"]},"author_link":["110075","110076"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1987-07-25","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"70","bibliographicPageStart":"41","bibliographicVolumeNumber":"11","bibliographic_titles":[{"bibliographic_title":"南方海域調査研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Occasional Papers","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1987-07-25","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"This paper is aimed at introducing an outline of the geothermal systems of the\nTaupo Volcanic Zone in New Zealand based mainly on a recent review by Hedenquist\n(1986).\nThe development of New Zealand's geothermal energy resources began in the late\n1940s, and the world's first \"wet steam\" geothermal station was constructed in 1958 at\nWairakei. Geothermal electricity from Wairakei supplies 150 MW, some 4% of New\nZealand's total requirements at present; another 100 MW will be provided by 1989 by the new development at Ohaaki.\nTwenty major geothermal systems are located in the Taupo Volcanic Zone. The zone extends from the active andesite volcano Mt.Ruapehu to White Island, another active volcano 220km north northeast in the Bay of Plenty; this is a zone of extensive geologic structural depression. A considerable volume of rhyolitic material fills the\ndepression, erupted during the last ~1.0 Ma. Geothermal drilling and gravity surveys\nhave revealed a relatively simple set of horst and graben blocks in the basement. Most\nof the geothermal systems have boiling springs at the surface and measured heat flows of 50 to 500 MW. They all have areas of low resistivity of a few to several km^<2>, indicating that hot saline water is present at depth. Chemical and isotopic studies of deep hot water indicate that the hot fluids are dominated by meteoric waters which have been heated and have acquired most of their solutes during deep circulation.\nGold and silver is presently being deposited in most of the geothermal systems in\nthe Taupo Volcanic Zone. The study of gold deposition in such active geothermal\nsystems has allowed us to unequivocally define the chemistry of the metal transporting fluids, and to identify fluid boiling and gas loss as the principal process leading to gold\ndeposition in the analogous fossil epithermal environment.","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_relation_32":{"attribute_name":"関連（relation）","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16098","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16099","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16100","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16101","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16102","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16103","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16105","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16106","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16107","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16108","subitem_relation_type_select":"URI"}}]},"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":"PISSN"}]},"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_44":{"attribute_name":"備考","attribute_value_mlt":[{"subitem_text_language":"ja","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/10232/16105, 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":"田口, 幸洋","creatorNameLang":"ja"},{"creatorName":"TAGUCHI, Sachihiro","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"110075","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"HEDENQUIST, Jeffrey W.","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"110076","nameIdentifierScheme":"WEKO"}]}]},"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","filename":"AN10030752_v11_p41-70.pdf","filesize":[{"value":"14.4 MB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"AN10030752_v11_p41-70.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/5220/files/AN10030752_v11_p41-70.pdf"},"version_id":"eba3a331-6e4f-4036-84a1-561e08804f7f"}]},"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":"ニュージーランドの地熱系","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"ニュージーランドの地熱系","subitem_title_language":"ja"},{"subitem_title":"Geothermal Systems in New Zealand","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["5412","94"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-06-08"},"publish_date":"2015-06-08","publish_status":"0","recid":"5220","relation_version_is_last":true,"title":["ニュージーランドの地熱系"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-06-24T08:44:33.494316+00:00"}