{"@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/1390282681472082048.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4116/jaqua.26.3_227"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"3165104"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/3165104"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I3165104"}},{"identifier":{"@type":"NAID","@value":"130001562617"}}],"dc:title":[{"@language":"en","@value":"A Review of Late Quaternary Deep-sea Tephras Around Japan"},{"@value":"日本列島周辺の深海底に分布するテフラ"},{"@language":"ja-Kana","@value":"ニホン レットウ シュウヘン ノ シンカイテイ ニ ブンプスル テフラ"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"Studies on late Quaternary deep-sea tephras are briefly reviewed in oceans and seas of the world and around the Japanese islands. A great number of modern research has been carried out on deep-sea tephra layers especially in the eastern Mediterranean Sea, Atlantic Ocean, Caribbean Sea and Pacific Ocean. Researches focus on the magnitude and type of individual explosive volcanism, the mechanism of deposition of tephra, correlation of macroscopic tephra layers and biostratigraphic dating of tephra, and resulted in disclosing several explosive volcanic eruptions of extraordinarily great magnitude such as the eruption of Campanian Y 5 ash in the Mediterranean, Los Chocoyos ash around Central America, Wairakei ash around New Zealand and Toba ash in the Bengal Bay and Indian Ocean.<br>In deep-sea sediments around the Japanese islands there are numbers of tephra layers, which are characterized and identified by petrographic and chemical methods. In the Sea of Japan six tephra layers have been identified, three of which are alkalic and are the products of major plinian eruptions of two volcanoes situated on and near the Korean Peninsula: Baegdusan and Ulreung-do. The other three are subalkalic and are corelated with large-scale eruptions from caldera volcanoes in Kyushu: Kikai, Aira and Aso. They are recognized not only in the Sea of Japan but also in the East China Sea and northwest Pacific Ocean, together with widespread tephras derived from Ata and Kikai calderas. All of them are co-ignimbrite ash fall deposit, and well dated by radiometric and stratigraphic methods. Palaeooceanography of late Quaternary around Japan are successfully studied with the aid of such widespread and time-marker tephras. There remain several tephras unidentified around Japan. In addition detailed volcanological and interdisciplinary studies of deep-sea tephras will be one of the problems to be studied in near future."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658319722880","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10087009"},{"@type":"NRID","@value":"1000010087009"},{"@type":"NRID","@value":"9000397706567"},{"@type":"NRID","@value":"9000365537326"},{"@type":"NRID","@value":"9000018656040"},{"@type":"NRID","@value":"9000019105830"},{"@type":"NRID","@value":"9000021563419"},{"@type":"NRID","@value":"9000403976513"},{"@type":"NRID","@value":"9000021768338"},{"@type":"NRID","@value":"9000002496798"},{"@type":"NRID","@value":"9000345268613"},{"@type":"NRID","@value":"9000367423292"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0156630"}],"foaf:name":[{"@language":"en","@value":"MACHIDA Hiroshi"},{"@language":"ja","@value":"町田 洋"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Geography, Tokyo Metropolitan University"},{"@language":"ja","@value":"東京都立大学理学部地理学教室"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658328950275","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80008119"},{"@type":"NRID","@value":"1000080008119"},{"@type":"NRID","@value":"9000019087345"},{"@type":"NRID","@value":"9000002496398"}],"foaf:name":[{"@language":"en","@value":"ARAI Fusao"},{"@language":"ja","@value":"新井 房夫"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth Sciences, Gunma University"},{"@language":"ja","@value":"群馬大学教育学部地学教室"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"04182642"},{"@type":"LISSN","@value":"04182642"},{"@type":"EISSN","@value":"18818129"},{"@type":"NDL_BIB_ID","@value":"000000014125"},{"@type":"ISSN","@value":"04182642"},{"@type":"NCID","@value":"AN0034136X"}],"prism:publicationName":[{"@language":"en","@value":"The Quaternary Research (Daiyonki-Kenkyu)"},{"@language":"ja","@value":"第四紀研究"},{"@language":"en","@value":"The Quaternary Res."},{"@language":"en","@value":"The Quat. Res."},{"@language":"en","@value":"The Quat. Res. (Daiyonki-Kenkyu)"},{"@language":"ja","@value":"第四紀研究"},{"@language":"en","@value":"Daiyonki-kenkyu"}],"dc:publisher":[{"@language":"en","@value":"Japan Association for Quaternary Research"},{"@language":"ja","@value":"日本第四紀学会"}],"prism:publicationDate":"1988","prism:volume":"26","prism:number":"3","prism:startingPage":"227","prism:endingPage":"242"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/3165104"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I3165104"}],"availableAt":"1988","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390001204265919872","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"姶良Tn火山灰(AT)の等層厚線図と分布軸の再検討"},{"@language":"en","@value":"Revision of the isopach map and dispersal axis of Aira-Tn ash(AT)"},{"@language":"ja-Kana","@value":"アイラ Tn カザンバイ AT ノ トウソウコウセンズ ト ブンプジク ノ サイケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234599552","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Marine sediments and late Quaternary stratigraphy in the southeastern part of the Japan Sea. Concerning the timing of dark layer deposition."},{"@value":"日本海南東部における海底堆積物と後期第四紀層序　特に暗色層の形成時期に関連して"},{"@language":"ja-Kana","@value":"ニホンカイ ナントウブ ニ オケル カイテイ タイセキブツ ト コウキ ダイ4"}]},{"@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/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/1390001206497054592","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quaternary environments on the basis of tephrochronology in Japan : Review and prospects"},{"@language":"ja","@value":"日本列島と周辺地域のテフラを基礎とした第四紀環境変化 : 回顧と展望"},{"@value":"2009年度日本第四紀学会賞受賞記念論文 日本列島と周辺地域のテフラを基礎とした第四紀環境変化--回顧と展望"},{"@language":"ja-Kana","@value":"2009ネンド ニホン ダイ4キ ガッカイショウ ジュショウ キネン ロンブン ニホン レットウ ト シュウヘン チイキ ノ テフラ オ キソ ト シタ ダイ4キ カンキョウ ヘンカ カイコ ト テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679412183168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"四国沖から採取された2本のIMAGESコアを用いた第四紀後期におけるテフラ層序(<特集>西太平洋におけるIMAGESコアを用いた高時間解像度の環境復元)"},{"@language":"en","@value":"Late Quaternary tephrostratigraphy of two IMAGES cores taken from the off Shikoku in the Northwest Pacific"},{"@value":"四国沖から採取された2本のIMAGESコアを用いた第四紀後期におけるテフラ層序"},{"@language":"ja-Kana","@value":"シコクオキ カラ サイシュ サレタ 2ホン ノ IMAGES コア オ モチイタ ダイ4キ コウキ ニ オケル テフラソウ ジョ"}]},{"@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/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 paleoclimatology"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0034102538"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I3165104"},{"@type":"CROSSREF","@value":"10.4116/jaqua.26.3_227"},{"@type":"CIA","@value":"130001562617"},{"@type":"OPENAIRE","@value":"doi_dedup___::d52472660ea75dcb44fcf09d8b7ad4a2"},{"@type":"CROSSREF","@value":"10.4116/jaqua.50.1_references_DOI_JgHAbWCQClg09smdEsLgli9pqAU"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0068-z_references_DOI_JgHAbWCQClg09smdEsLgli9pqAU"}]}