{"@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/1360292618936714752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/bf00874390"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1007/BF00874390.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1007/BF00874390/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/BF00874390"}},{"identifier":{"@type":"DOI","@value":"10.1007/978-3-0348-7279-9_18"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/978-3-0348-7279-9_18.pdf"}}],"dc:title":[{"@value":"Onshore tsunami deposits caused by the 1993 Southwest Hokkaido and 1983 Japan Sea earthquakes"}],"description":[{"notation":[{"@value":"Onshore tsunami deposits resulting from the 1993 Southwest Hokkaido and 1983 Japan Sea earthquakes were described to evaluate the feasibility of tsunami deposits for inferring paleoseismic events along submarine faults. Tsunami deposits were divided into three types, based on their composition and aerial distribution: (A) deposits consisting only of floating materials, (B) locally distributed siliclastic deposits, and (C) widespread siliclastic deposits. The most widely distributed tsunami deposits consist of the first two types. Type C deposits are mostly limited to areas where the higher tsunami runup was observed. The scale of tsunami represented by vertical tsunami runup is an important factor controlling the volume of tsunami deposits. The thickest deposits, about 10 cm, occur behind coastal dunes. To produce thick siliclastic tsunami deposits, a suitable source area, such as sand bar or dune, must be available in addition to sufficient vertical tsunami runup. Estimation of the amounts of erosion and deposition indicates that tsunami deposits were derived from both onshore and shoreface regions. The composition and grain size of the tsunami deposits strongly reflect the nature of the sedimentary materials of their source area. Sedimentary structures of the tsunami deposits suggest both low and high flow regimes. Consequently, it seems very difficult to identify tsunami deposits based only on grain size distribution or sedimentary structure of a single site in ancient successions."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380292618936714754","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Sato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292618936714755","@type":"Researcher","foaf:name":[{"@value":"Toshihiko Shimamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292618936714752","@type":"Researcher","foaf:name":[{"@value":"Akito Tsutsumi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292618936714753","@type":"Researcher","foaf:name":[{"@value":"Eiko Kawamoto"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00334553"},{"@type":"EISSN","@value":"14209136"},{"@type":"ISBN","@value":"9783764351021"},{"@type":"ISBN","@value":"9783034872799"}],"prism:publicationName":[{"@value":"pure and applied geophysics"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1995-09","prism:volume":"144","prism:number":"3-4","prism:startingPage":"693","prism:endingPage":"717"},"reviewed":"false","dc:rights":["https://www.springernature.com/gp/researchers/text-and-data-mining","https://www.springernature.com/gp/researchers/text-and-data-mining"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1007/BF00874390.pdf"},{"@id":"https://link.springer.com/article/10.1007/BF00874390/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/BF00874390"},{"@id":"http://link.springer.com/content/pdf/10.1007/978-3-0348-7279-9_18.pdf"}],"createdAt":"2004-12-28","modifiedAt":"2024-07-26","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050862623748407168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami deposits associated with the 1983 Nihonkai-Chubu earthquake tsunami in coastal forests near Happo Town, Akita Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617541111808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunamis caused by offshore active faults and their deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166017452672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial thickness variability of the 2011 Tohoku-oki tsunami deposits along the coastline of Sendai Bay"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496768768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地震津波堆積物 : 最近20年間のおもな進展と残された課題"},{"@language":"en","@value":"Seismic Tsunami Deposits : Major Advances over the Last 20 Years and Remaining Problems"},{"@language":"ja-Kana","@value":"ジシン ツナミ タイセキブツ サイキン 20ネンカン ノ オモナ シンテン ト ノコサレタ カダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216735488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunamis and possible tsunamigenic deposits along the eastern margin of the Japan Sea"},{"@language":"ja","@value":"日本海東縁の津波とイベント堆積物"},{"@language":"ja-Kana","@value":"ニホンカイ トウエン ノ ツナミ ト イベント タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488465408","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentary deposits of the 26 December 2004 tsunami on the northwest coast of Aceh, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238041001984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"1983年日本海中部地震津波の影響地域における過去の津波履歴の検討"},{"@language":"en","@value":"A STUDY OF PALEO-TSUNAMI HISTORY AROUND THE AREA AFFECTED BY THE 1983 JAPAN SEA EARTHQUAKE, COASTAL LOWLAND ON THE NORTHERN PART OF AKITA PREFECTURE, THE EASTERN MARGIN OF JAPAN SEA"},{"@language":"ja-Kana","@value":"1983ネン ニホンカイ チュウブ ジシン ツナミ ノ エイキョウ チイキ ニ オケル カコ ノ ツナミ リレキ ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390570176043963520","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Progress in tsunami sedimentology"},{"@language":"ja","@value":"津波堆積学の進展"},{"@language":"ja-Kana","@value":"ツナミ タイセキガク ノ シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1524232504698139264","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The impact on bottom sediments and ostracods in the Khlong Thom River mouth following the 2004 Indian Ocean 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