{"@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/1390282679280882432.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.18940/kazan.40.1_33"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"3624090"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/3624090"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I3624090"}},{"identifier":{"@type":"NAID","@value":"10004653754"}},{"identifier":{"@type":"NAID","@value":"110003041025"}}],"dc:title":[{"@language":"ja","@value":"大規模珪長質火山活動と地殻歪速度"},{"@language":"en","@value":"Large-volume Felsic Volcanism and Crustal Strain Rate"},{"@language":"ja-Kana","@value":"ダイキボ ケイチョウシツ カザン カツドウ ト チカク ヒズミソクド"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"There is no positive correlation between the long-term eruption rate of large-scale felsic volcanism and its discharge volume of a single eruptive episode. This means that the storage of voluminous felsic magma at high-level in the crust is caused not by high magma production rate but by continuous accumulation of magma during a long repose time, if the long-term eruption rate reflects the averaged magma production rate. If the cruslal defomation is weak, the magma chamber could be stable in the crust; it is favorable for efficient accumulation of voluminous magma. In fact, the large-volume felsic volcanism occurs exclusively in the region of low crustal strain rate. The low crustal strain rate is considered to be essential for the formation of large-scale felsic volcanism. The large-volume felsic volcanic activity is present in the compressional tectonic stress field as well as in the extensional one; the difference in arrangement of principal stress axes is not related to the occurrence of voluminous felsic volcanism."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282679280882432","@type":"Researcher","foaf:name":[{"@language":"ja","@value":"高橋 正樹"},{"@language":"en","@value":"TAKAHASHI Masaki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth Sciences, Ibaraki University"},{"@language":"ja","@value":"茨城大学理学部地球科学教室"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"04534360"},{"@type":"EISSN","@value":"21897182"},{"@type":"NDL_BIB_ID","@value":"000000003812"},{"@type":"ISSN","@value":"04534360"},{"@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":"1995","prism:volume":"40","prism:number":"1","prism:startingPage":"33","prism:endingPage":"42"},"url":[{"@id":"http://id.ndl.go.jp/bib/3624090"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I3624090"}],"availableAt":"1995","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845762383369472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"岡山県北西部, 白亜紀新見コールドロン"},{"@language":"en","@value":"Cretaceous Niimi Cauldron in the northwestern part of Okayama Prefecture, Southwest Japan"},{"@language":"ja-Kana","@value":"オカヤマケン ホクセイブ ハクアキ ニイミ コールドロン"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143600969728","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Experimental determination of the fluid-absent melting relations in the pelitic system"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266385152","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"いろは坂溶結凝灰岩類の噴出機構と西南日本内帯後期白亜紀火成活動への対比"},{"@language":"en","@value":"Eruptive system of the Irohazaka Welded Tuffs and correlation to the Late Cretaceous igneous activity of the Inner Zone of Southwest Japan"},{"@language":"ja-Kana","@value":"イロハザカ ヨウ ケツ ギョウカイガンルイ ノ フンシュツ キコウ ト セイナン ニホン ナイタイ コウキ ハクアキ カセイカツドウ エ ノ タイヒ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303335552","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北日本, 火山フロント付近の 2.O Ma 以降の火山活動とテクトニクスの推移"},{"@language":"en","@value":"Sequence of the Volcanism and Tectonics during the Last 2.0 Million Years along the Volcanic Front in Tohoku District, NE Japan"},{"@value":"東北日本,火山フロント付近の2.0Ma以降の火山活動とテクトニクスの推移"},{"@language":"ja-Kana","@value":"トウホク ニホン カザン フロント フキン ノ 2.0Ma イコウ ノ カザン カツドウ ト テクトニクス ノ スイイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206122594048","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"島弧火山の深部プロセスの定量的モデル化(第1部 マグマの生成・上昇)"},{"@language":"en","@value":"Modelling of Deep Processes of Island Arc Volcanoes(Session 1)"},{"@value":"島弧火山の深部プロセスの定量的モデル化"},{"@language":"ja-Kana","@value":"トウコ カザン ノ シンブ プロセス ノ テイリョウテキ モデルカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206233629824","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Volcanostratigraphy and geologic structure of the Enrei Formation on the southwest side of Lake Suwa, Nagano Prefecture, Central Japan. A Late Pliocene to Early Pleistocene volcanic history in a junction of island arcs."},{"@value":"長野県諏訪湖南西方における塩嶺累層の火山層序と地質構造　　島弧会合部における後期鮮新世～前期更新世の火山活動史"},{"@language":"ja-Kana","@value":"ナガノケン スワコ ナンセイホウ ニ オケル エンレイルイソウ ノ カザン ソウジョ ト チシツ コウゾウ トウコ カイゴウブ ニ オケル コウキ センシンセイ ゼンキ コウシンセイ ノ カザン カツドウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234254720","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Neogene volcanism in Central-Eastern Hokkaido: Beginning and evolution of arc volcanism inferred from volcanological parameters and geochemistry."},{"@value":"北海道中央部～東部の新第三紀火山活動　　火山学的データおよび全岩化学組成からみた島弧火山活動の成立と変遷"},{"@language":"ja-Kana","@value":"ホッカイドウ チュウオウブ トウブ ノ シンダイ3キ カザン カツドウ カザンガクテキ データ オヨビ ゼン ガン カガク ソセイ カラ ミタ シマ コ カザン カツドウ ノ セイリツ ト ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235456512","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Volcanic sequence of caldera-fill deposits 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Japan."},{"@language":"ja","@value":"中部日本，北八ヶ岳火山北麓に分布する前期更新世火山岩類の火山層序"},{"@value":"中部日本,北八ヶ岳火山北麓に分布する前期更新世火山岩類の火山層序--北八ヶ岳～塩嶺地域における大規模マグマ活動について"},{"@language":"ja-Kana","@value":"チュウブ ニホン キタヤツガタケ カザン ホクロク ニ ブンプ スル ゼンキ コウシン セイ カザンガンルイ ノ カザンソウ ジョ キタヤツガタケ エンレイチイキ ニ オケル ダイキボ マグマ カツドウ ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679210994816","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北本州弧における後期新生代の火成活動史(<特集>島弧の深部構造-地質・地震・地震波トモグラフィによる解析(II))"},{"@language":"en","@value":"Late Cenozoic Magmatism in the northeast Honshu Arc, Japan(<Special issue>Deep Structure under Island Arcs from the Viewpoints of Geology, Seismology and Seismic Tomography (II))"},{"@value":"東北本州弧における後期新生代の火成活動史"},{"@language":"ja-Kana","@value":"トウホクホンシュウ コ ニ オケル コウキ シンセイダイ ノ カセイカツドウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280909440","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"応力比からみた陥没カルデラ構造と応力場"},{"@language":"en","@value":"Stress Ratio of Caldera Bounding Faults as a Guide to Aspects of Regional Stress Regime"},{"@value":"応力比から見た陥没カルデラ構造と応力場"},{"@language":"ja-Kana","@value":"オウリョクヒ カラ ミタ カンボツ カルデラ コウゾウ ト オウリョクバ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213404160","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"尾鈴山酸性岩の地質"},{"@language":"en","@value":"Geology of the Osuzuyama acid rocks, Miyazaki Prefecture, Kyushu, Japan"},{"@language":"ja-Kana","@value":"ビレイサン サンセイガン ノ チシツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213579136","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Middle Miocene ash-flow calderas at the compressive margin of southwest Japan arc: Review and synthesis"},{"@language":"ja","@value":"西南日本弧前縁の圧縮テクトニクスと中期中新世カルデラ火山"},{"@language":"ja-Kana","@value":"セイナン ニホン コ ゼンエン ノ アッシュク テクトニクス ト チュウキ チュウシンセイ カルデラ カザン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473644544","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Spatial and Temporal Relationship between Uplifting and Magmatism in the Hida Mountain Range, Central Japan"},{"@value":"飛騨山脈の隆起と火成活動の時空的関連"},{"@language":"ja-Kana","@value":"ヒダ サンミャク ノ リュウキ ト カセイカツドウ ノ ジクウテキ カンレン"}]},{"@id":"https://cir.nii.ac.jp/crid/1523388079559565568","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"日本海の形成機構--新しい背弧海盆拡大モデル"},{"@language":"ja-Kana","@value":"ニホンカイ ノ ケイセイ キコウ アタラシイ ハイコ カイボン カクダイ 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