{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282679280899200.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.18940/kazan.45.1_25"}},{"identifier":{"@type":"URI","@value":"http://hdl.handle.net/2298/36961"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"5309647"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/5309647"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I5309647"}},{"identifier":{"@type":"NAID","@value":"110003041178"}},{"identifier":{"@type":"NAID","@value":"10011070516"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"ja","@value":"阿蘇火山地獄温泉付近における水蒸気爆発とその堆積物"},{"@language":"en","@value":"Phreatic Explosions and Ejecta around Jigoku Spa, Southwestern Part of the Central Cones of Aso Volcano, Japan"},{"@language":"ja-Kana","@value":"アソ カザン ジゴク オンセン フキン ニ オケル スイジョウキ バクハツ ト ソノ タイセキブツ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Jigoku spa is located west of Ikenokubo basin of Yomineyama volcano, southwestern part of the central cones of Aso volcano. In this basin, “Ikenokubo tuff ring” and two smaller maars were developed. Two layers of ejecta, about 10<sup>5</sup> m<sup>3</sup> in bulk volume, formed by phreatic explosions were found in this area. They are very poorly sorted and mainly composed of altered fine-grained ash including lithic fragments. Kikai Akahoya ash erupted about 6,300 years BP (<sup>14</sup>C) is intercalated between two layers of phreatic ejecta in thick ash layers from Nakadake, the only active central cone. Based on <sup>14</sup>C ages of buried Andisols and the succession of the deposits, the eruption ages of the two ejecta are estimated at about 10,000 years BP for older deposit and at about 4,500 years BP for younger one. Distributions of thickness and maximum grain size of the lithic fragments suggest that the both of two phreatic ejecta were exploded not from “Ikenokubo tuff ring” and two maars but from the Jigoku explosion crater in the western area. Ejecta correlative to the “Ikenokubo tuff ring” Iies under the older of the phreatic ejecta layers. Consequently, the eruption age of “kenokubo tuff ring” is probably older than 10,000 years BP. Frequency of phreatic explosions, Iarger than 10<sup>5</sup> m<sup>3</sup> in volume, is considered to be once in about 5,000 years. This fact is noteworthy for volcanic hazards assessment in the surrounding area of Jigoku spa and adjacent Tarutama spa."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658337539845","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10040049"},{"@type":"NRID","@value":"1000010040049"},{"@type":"NRID","@value":"9000400194265"},{"@type":"NRID","@value":"9000007579129"},{"@type":"NRID","@value":"9000002616011"},{"@type":"NRID","@value":"9000004601029"},{"@type":"NRID","@value":"9000255922990"},{"@type":"NRID","@value":"9000254150238"},{"@type":"NRID","@value":"9000408608491"},{"@type":"NRID","@value":"9000408608921"},{"@type":"NRID","@value":"9000256757729"},{"@type":"NRID","@value":"9000408608885"},{"@type":"NRID","@value":"9000408608454"},{"@type":"NRID","@value":"9000018667986"},{"@type":"NRID","@value":"9000256755961"},{"@type":"NRID","@value":"9000002579829"},{"@type":"NRID","@value":"9000408608852"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0173011"}],"foaf:name":[{"@language":"ja","@value":"渡辺 一徳"},{"@language":"en","@value":"WATANABE Kazunori"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Faculty of Education, Kumamoto University"},{"@language":"ja","@value":"熊本大学教育学部"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276161674880","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30353874"},{"@type":"NRID","@value":"1000030353874"},{"@type":"ORCID","@value":"0000-0003-2246-5231"},{"@type":"NRID","@value":"9000375860594"},{"@type":"NRID","@value":"9000288834054"},{"@type":"NRID","@value":"9000414227709"},{"@type":"NRID","@value":"9000408782531"},{"@type":"NRID","@value":"9000408607570"},{"@type":"NRID","@value":"9000411843257"},{"@type":"NRID","@value":"9000414227704"},{"@type":"NRID","@value":"9000411952282"},{"@type":"NRID","@value":"9000408626230"},{"@type":"NRID","@value":"9000411826503"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/miyabuchi"}],"foaf:name":[{"@language":"ja","@value":"宮縁 育夫"},{"@language":"en","@value":"MIYABUCHI Yasuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Kyushu Research Center, Forestry and Forest Products Research Institute"},{"@language":"ja","@value":"森林総合研究所九州支所"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"04534360"},{"@type":"EISSN","@value":"21897182"},{"@type":"ISSN","@value":"04534360"},{"@type":"NDL_BIB_ID","@value":"000000003812"},{"@type":"LISSN","@value":"04534360"},{"@type":"NCID","@value":"AN10512786"}],"prism:publicationName":[{"@language":"en","@value":"BULLETIN OF THE VOLCANOLOGICAL SOCIETY OF JAPAN"},{"@language":"ja","@value":"火山"},{"@language":"en","@value":"BVSJ"}],"dc:publisher":[{"@language":"en","@value":"The Volcanological Society of Japan"},{"@language":"ja","@value":"特定非営利活動法人 日本火山学会"}],"prism:publicationDate":"2000","prism:volume":"45","prism:number":"1","prism:startingPage":"25","prism:endingPage":"32"},"url":[{"@id":"http://hdl.handle.net/2298/36961"},{"@id":"http://id.ndl.go.jp/bib/5309647"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I5309647"}],"availableAt":"2000","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=453.8","dc:title":"453.8"}],"dcterms:subject":[{"subjectScheme":"Other","notation":[{"@value":"453.8"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001337920457216","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hazard Maps of Naka-dake, Aso Volcano, Japan"},{"@language":"ja-Kana","@value":"Hazard Maps of Naka-dake Aso volcano Ja"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810901720192","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"降下テフラからみた水蒸気噴火の規模・頻度"},{"@language":"en","@value":"Magnitude and Frequency of Phreatic Eruptions, Inferred from Tephra-stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303846912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"埋没黒ボク土層の<sup>14</sup>C年代からみた完新世阿蘇火山テフラの噴出年代"},{"@language":"en","@value":"Eruption Ages of Holocene Tephras from Aso Volcano, Southwestern Japan, Inferred from <sup>14</sup>C Ages of Buried Andisols"},{"@value":"埋没黒ボク土層の14C年代からみた完新世阿蘇火山テフラの噴出年代"},{"@language":"ja-Kana","@value":"マイボツ クロボク ドソウ ノ 14C ネンダイ カラ ミタ カンシンセイ ア"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304494464","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"阿蘇火山中岳の灰噴火とその噴出物(＜特集＞堆積物による火山噴火史研究)"},{"@language":"en","@value":"Ash Eruption of Nakadake Volcano, Aso Caldera, and its Products(＜Special Section＞Volcanic History and Eruptive Deposits)"},{"@value":"阿蘇火山中岳の灰噴火とその噴出物"},{"@language":"ja-Kana","@value":"アソカ ザンナカダケ ノ カイフンカ ト ソノ フンシュツブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279880192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"阿蘇中央火口丘群西側斜面で発見された岩屑堆積物とそれらの<sup>14</sup>C年代"},{"@language":"en","@value":"<sup>14</sup>C Ages of Volcaniclastic Deposits Discovered on the Western Slope of Aso Central Cones, Southwestern Japan"},{"@value":"寄書 阿蘇中央火口丘群西側斜面で発見された岩屑堆積物とそれらの14C年代"},{"@language":"ja-Kana","@value":"キショ アソチュウオウ カコウキュウグン ニシガワ シャメン デ ハッケン サレタ ガンセツ タイセキブツ ト ソレラ ノ 14C ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280884352","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"阿蘇火山吉岡温泉で2006年に起きた地熱活動の定量的評価"},{"@language":"en","@value":"Quantitative Analysis of Geothermal Events at the Yoshioka Hot Spring, Aso Volcano, in 2006 Aso Volcano, in 2006"},{"@language":"ja-Kana","@value":"アソ カザン ヨシオカ オンセン デ 2006ネン ニ オキタ チネツ カツドウ ノ テイリョウテキ ヒョウカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211554304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Eruptive history of Kita-Hakkoda volcanic group during the last 6000 years, Northeast Japan."},{"@value":"北八甲田火山群における最近６０００年間の噴火活動史"},{"@language":"ja-Kana","@value":"キタハッコウダ カザングン ニ オケル サイキン 6000ネンカン ノ フンカ カツドウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472660096","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Akahoya Ash-A Holocene Widespread Tephra Erupted from the Kikai Caldera, South Kyushu, Japan"},{"@value":"南九州鬼界カルデラから噴出した広域テフラ―アカホヤ火山灰"},{"@language":"ja-Kana","@value":"ミナミ キュウシュウ キカイ カルデラ カラ フンシュツシタ コウイキ テフラ"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009749183029376","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009749341866624","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1570009749341869312","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1570291224159742080","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山杵島岳 往生岳の噴出物と黒ボク土に関する知見について"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854174113162112","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山地質図(5万分の1)"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854174271997824","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1570854174271999104","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山1958年6月\"大爆発\"概報"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854174272001280","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"1979年の阿蘇山の活動"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698599202129536","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山における温泉観測"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698599202131840","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"垂玉温泉再興願"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698599202132992","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"熊本県阿蘇青年の家付近の阿蘇中央火口丘テフラ"}]},{"@id":"https://cir.nii.ac.jp/crid/1572543024132262656","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"垂玉温泉再興願(2)"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824499108973440","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"火山噴出物の地質学的 岩石学的研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824499108975872","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山岩類のK-Ar年代測定-火山層序との整合性と火砕流試料への適応-"}]},{"@id":"https://cir.nii.ac.jp/crid/1573105974085686144","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1573387449062397824","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"阿蘇火山地質報文"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387449389613440","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"比抵抗法とIP法による熱水変質帯の抽出"},{"@language":"en","@value":"Detection of Hydrothermally Altered Zones by Resistuvity and Induced Polarization Methods"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668923923908224","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Measures of describing the size distribution of sediments."}]},{"@id":"https://cir.nii.ac.jp/crid/1573668924039105792","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1573950399015815552","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"平成2年度全国地熱資源総合調査(第3次)広域熱水流動系調査 阿蘇地域"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401452044032","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Another look at the calculation of fallout tephra volumes"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791869787264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of the 2016 Kumamoto earthquakes on the Aso volcanic edifice"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2001960003"},{"@type":"IRDB","@value":"oai:irdb.nii.ac.jp:01242:0003289131"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I5309647"},{"@type":"CIA","@value":"10011070516"},{"@type":"CIA","@value":"110003041178"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0646-y_references_DOI_8BpH1jLDkSMqlw1STW7zNV9zBS9"}]}