{"@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/1362825896142748416.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0025-3227(86)90103-9"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0025322786901039?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0025322786901039?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"80002913158"}}],"dc:title":[{"@value":"Widespread submarine tephras around Japan — Petrographic and chemical properties"}],"description":[{"notation":[{"@value":"Abstract   In deep-sea sediments around the Japanese Islands, tephra layers are frequently recognized, and some tephras can be identified by petrographic and chemical features and correlated to source volcanoes of both Japan and Korea. Most tephras distributed over more than several hundred kilometers from the source volcanoes were presumably carried away by the dominant westerly wind. Six characteristic marker tephras in deep-sea sediments can be identified and correlated according to their distribution and grain size, petrography, and chemistry. They play an important role in compiling the Late Quaternary chronology of the deep-sea sediments distributed around the Japanese Islands. Petrographic and geochemical studies reveal that the refractive index of volcanic glass shards in tephras is controlled by the amount of total transition metal oxides rather than the amount of SiO 2 . We propose a new equation relating refractive index to glass shard chemistry."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896142748416","@type":"Researcher","foaf:name":[{"@value":"Toshio Furuta"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896142748417","@type":"Researcher","foaf:name":[{"@value":"Kantaro Fujioka"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896142748418","@type":"Researcher","foaf:name":[{"@value":"Fusao Arai"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00253227"},{"@type":"NCID","@value":"AA00721562"}],"prism:publicationName":[{"@value":"Marine Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1986-06","prism:volume":"72","prism:number":"1-2","prism:startingPage":"125","prism:endingPage":"142"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0025322786901039?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0025322786901039?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025717367368320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Submarine pyroclastic deposits from 7.3 ka caldera-forming Kikai-Akahoya eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845762388079744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hadal disturbance in the Japan Trench induced by the 2011 Tohoku-Oki earthquake"},{"@value":"Hadal disturbance in the Japan Trench induced by the 2011 Tokohu-Oki earthquake"},{"@value":"Hadal disturbance in the Japan Trench induced by the 2011 Tohoku—Oki Earthquake"},{"@value":"Hadal disturbance in the Japan Trench as induced by the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216136879872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Widespread tephras in sediments from lake Ichi-no-Megata in northern Japan: Their description, correlation and significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232101087744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics and ages of tephra layers in the central Okhotsk Sea over the last 350kyr"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691114260096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Integrating the Holocene tephrostratigraphy for East Asia using a high-resolution cryptotephra study from Lake Suigetsu (SG14 core), central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691180784512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Quaternary tephrostratigraphy of Baegdusan and Ulleung Volcanoes using marine sediments in the Japan Sea/East Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166090943232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Identification of the Changbaishan ‘Millennium’ (B-Tm) eruption deposit in the Lake Suigetsu (SG06) sedimentary archive, Japan: Synchronisation of hemispheric-wide palaeoclimate archives"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657398971008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale reworking of tephra in alluvial to shallow marine settings: Distinguishing pseudo-isochrons from genuine ones"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412891977264640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Refining the eruptive history of Ulleungdo and Changbaishan volcanoes (East Asia) over the last 86 kyrs using distal sedimentary records"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845682922752","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Tyatya Volcano, southwestern Kuril arc: Recent eruptive activity inferred from widespread 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タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235206528","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re-examination of the eruption age of Aira-Tn Ash(AT) obtained from a piston core off Shikoku. Determined by AMS 14C dating of planktonic foraminifera."},{"@value":"四国沖ピストンコア試料を用いたＡＴ火山灰噴出年代の再検討　タンデトロン加速器質量分析計による浮遊性有孔虫の｀１４´Ｃ年代"},{"@language":"ja-Kana","@value":"シコクオキ ピストン コア シリョウ オ モチイタ AT カザンバイ フンシュ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235331584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tephrostratigraphy of the piston cored sediment KT96-17 P-2 in the southern Japan Sea. The eruption age of Daisen-Kusadanihara Pumice (KsP)."},{"@value":"日本海南部ＫＴ９６‐１７　Ｐ‐２コアの火山灰層序　　大山草谷原軽石層（ＫｓＰ）の噴出年代"},{"@language":"ja-Kana","@value":"ニホンカイ ナンブ KT96 17 P 2 コア ノ カザンバイ ソウジョ ダイセン クサダニハラ カルイシソウ KsP ノ フンシュツ ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238408960","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reappraisal for recent faulting history of the Hakushu fault, the southern part of the Itoigawa"},{"@language":"ja","@value":"糸魚川—静岡構造線活断層系南部, 白州断層の活動履歴の再検討"},{"@value":"糸魚川-静岡構造線活断層系南部,白州断層の活動履歴の再検討--横手地点トレンチ調査"},{"@language":"ja-Kana","@value":"イトイガワ シズオカ コウゾウセンカツダンソウケイ ナンブ ハクシュウ ダンソウ ノ カツドウ リレキ ノ サイケントウ ヨコテ チテン トレンチ チョウサ"},{"@value":"Reappraisal for recent faulting history of the Hakushu fault, the southern part of the Itoigawa-Shizuoka Tectonic Line, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495278592","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evidence in Ulleung Basin Sediment Cores for a Termination II (Penultimate Deglaciation) Eruption of the Aso-3 Tephra"},{"@language":"ja","@value":"Termination IIに噴出した阿蘇3火山灰-東海(日本海)対馬海盆堆積物からの証拠"},{"@value":"Evidence in Ulleung Basin Sediment Cores for a Termination 2 (Penultimate Deglaciation) Eruption of the Aso-3 Tephra"},{"@value":"Evidence in Ulleung Basin sediment cores for a Termination (penultimate deglaciation) eruption of the Aso-3 Tephra"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496153728","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origin and Correlation of Three Tephras That Erupted During Oxygen Isotope Stage 3 Found in Cores from the Yamato Basin, Central Japan Sea"},{"@value":"日本海中部大和海盆から採取された酸素同位体ステージ３に噴出した３枚の火山灰"},{"@language":"ja-Kana","@value":"ニホンカイ チュウブ ヤマトカイボン カラ サイシュ サレタ サンソ ドウイタイ ステージ 3 ニ フンシュツシタ 3マイ ノ カザンバイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496511104","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Identification and Chronostratigraphy of Middle to Upper Quaternary Marker Tephras Occurring in the Anden Coast Based on Comparison with ODP Cores in the Sea of Japan."},{"@value":"ＯＤＰ日本海試料との対比に基づく男鹿半島安田海岸更新世中‐後期テフラの同定と年代"},{"@language":"ja-Kana","@value":"ODP ニホンカイ シリョウ ト ノ タイヒ ニ モトズク オガ ハントウ ア"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497431296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Identification of volcanic products around the southern foot of Haruna Volcano, central Japan : An example of identifying volcanic products using refractive indices of plagioclase phenocrysts"},{"@language":"ja","@value":"斜長石斑晶の屈折率を用いた火山噴出物の識別<BR>—榛名火山南麓を中心に分布する噴出物を例に"},{"@value":"斜長石斑晶の屈折率を用いた火山噴出物の識 別 : 榛名火山南麓を中心に分布する噴出物を例に"},{"@language":"ja-Kana","@value":"シャ チョウセキ ハンショウ ノ クッセツリツ オ モチイタ カザン フンシュツブツ ノ シキ ベツ : ハルナ カザン ナンロク オ チュウシン ニ ブンプ スル フンシュツブツ オ レイ ニ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288036863104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analysis of matrix effect in laser ablation inductively coupled plasma mass spectrometry for rhyolitic glass: Critical evaluation with new Aso-4 b-W synthetic glass blocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390013043977303424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Pleistocene to Holocene tephrastratigraphy in the off Wakasa Bay sediment cores and correlation with widespread tephras"},{"@language":"ja","@value":"若狭湾沖海底堆積物コアに挟まる後期更新世から完新世テフラの層序と広域テフラとの対比"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206833536","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Environments of Ocean and Primary Productivity during the Late Quaternary. Paleoceanography of East Asian Marginal Seas-Their environmental changes and its global linkage."},{"@value":"第四紀後期の海洋環境と生物生産　　縁海の古海洋学　縁海の海洋環境変遷とその重要性"},{"@language":"ja-Kana","@value":"エンカイ ノ コ カイヨウガク エンカイ ノ カイヨウ カンキョウ ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211300352","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Identification of tephra based on statistical analysis of refractive index and morphological classification of volcanic glass shards."},{"@value":"火山ガラスの屈折率測定および形態分類とその統計的な解析に基づくテフラの識別"},{"@language":"ja-Kana","@value":"カザン ガラス ノ クッセツリツ ソクテイ オヨビ ケイタイ ブンルイ ト ソ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472441728","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Drifting Pumice Clasts Derived from Ulleung Island in Early Holocene Sediments at Oda, Shimane Prefecture, Southwestern Japan."},{"@value":"島根県大田市の掘削コアから発見された欝陵島の完新世初期火山活動由来の漂着軽石"},{"@language":"ja-Kana","@value":"シマネケン オオダシ ノ クッサク コア カラ ハッケンサレタ ウツリョウトウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472817920","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quaternary Widespread Tephra Catalog in and around Japan : Recent Progress."},{"@value":"Quatemary Widespread Tephra Catalog in and around Japan"},{"@value":"Quaternary widespread tephra catalogue in and around Japan: recent progress"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472904832","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation and Correction of EDS Results of the Glass Shards from Some Representative Tephra by Comparison with XRF Analysis"},{"@value":"ＸＲＦ分析との比較によるテフラガラス片のＥＤＳ分析結果の評価と補正"},{"@language":"ja-Kana","@value":"XRF ブンセキ ト ノ ヒカク ニ ヨル テフラガラスヘン ノ EDS ブンセキ ケッカ ノ ヒョウカ ト ホセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473689088","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Quaternary Tephrostratigraphy of Marine Core KH94-3, LM-8 off Sanriku, Japan."},{"@value":"三陸沖海底コアＫＨ９４‐３，ＬＭ‐８の後期更新世テフラ層序"},{"@language":"ja-Kana","@value":"サンリクオキ カイテイ コア KH94 3 LM 8 ノ コウキ コウシン セイ テフラソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473851392","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tephra Studies on Quaternary Explosive Eruptions in the Japanese Islands"},{"@language":"ja","@value":"日本列島の爆発的噴火に関するテフラ研究の動向"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473938944","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Pleistocene tephrostratigraphy of the sediment core MD01-2421 collected off the Kashima coast, Japan"},{"@language":"ja","@value":"鹿島沖海底コアMD01-2421の後期更新世テフラ層序"},{"@language":"ja-Kana","@value":"カシマオキ カイテイ コア MD01 2421 ノ コウキ コウシンセイ テフラ ソウジョ"},{"@value":"Late Pleistocene tephrostratigraphy of the sediment core MD01-2421 collected off the Kashima coast, Japan (in Japanese with English summary)"},{"@value":"Late Pleistocene tephrostratigraphy of the sediment core MD01-2421 collected off the Kashima coast"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473979008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relationship between Major Element Composition and Refractive Index of Volcanic Glass"},{"@value":"火山ガラスの主要成分含有量と屈折率との関係"},{"@language":"ja-Kana","@value":"カザン ガラス ノ シュヨウ セイブン ガンユウリョウ ト クッセツリツ ト ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681474154368","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Vegetation and climate history since MIS 7 in the Kenbuchi Basin, northern Hokkaido : Comparison between MIS 6/5e and MIS 2/1"},{"@language":"ja","@value":"北部北海道の剣淵盆地におけるMIS7以降の植生と気候の変遷史－特にMIS 6/5eとMIS 2/1について"},{"@language":"ja-Kana","@value":"ホクブ ホッカイドウ ノ ケン エン ボンチ ニ オケル MIS7 イコウ ノ ショクセイ ト キコウ ノ ヘンセンシ : トクニ MIS6/5e ト MIS2/1 ニ ツイテ"},{"@value":"Vegetation and climate history since MIS 7 in the Kenbuchi Basin, northern Hokkaido: comparison between MIS 6/5e and MIS 2/1 (in Japanese, with English summary)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763129469824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Correlation between Alkaline Tephra (Hm-2 Tephra) Distributed on Hakusan Volcano, Central Japan and Tephras on Ulleung Island Based on Major Element Compositions and <sup>14</sup>C 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Years"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291226053726848","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemical characterization of the organic matter, pore water constituents and shallow methane gas in the eastern part of the Ulleung Basin, East Sea (Japan Sea)"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400241522304","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tephrostratigraphy and paleoenvironmental variation in late Quaternary core sediments of the southwestern Ulleung Basin, East Sea (Sea of Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842097198848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine tephra in the Japan Sea sediments as a tool for paleoceanography and 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