{"@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/1390282681488085504.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03352380"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"5770490"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/5770490"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I5770490"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/8833486"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03352380.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03352380/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03352380"}},{"identifier":{"@type":"NAID","@value":"10007638734"}}],"dc:title":[{"@language":"en","@value":"Coseismic slip distribution of the 1946 Nankai earthquake and aseismic slips caused by the earthquake"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Coseismic slip distribution on the fault plane of the 1946 Nankai earthquake (M<SUB>w</SUB> 8.3) was estimated from inversion of tsunami waveforms. The following three improvements from the previous study (Satake, 1993) were made. (1) Larger number of smaller subfaults is used; (2) the subfaults fit better to the slab geometry; and (3) more detailed bathymetry data are used. The inversion result shows that the agreement between observed and synthetic waveforms is greatly improved from the previous study. In the western half of the source region off Shikoku, a large slip of about 6 m occurred near the down-dip end of the locked zone. The slip on the up-dip or shallow part was very small, indicating a weak seismic coupling in that region. In the eastern half of the source region off Kii peninsula, a large slip of about 3 m extended over the entire locked zone. Large slips on the splay faults in the upper plate estimated from geodetic data (Sagiya and Thatcher, 1999) were not required to explain the tsunami waveforms, suggesting that the large slips were aseismic. Two slip distributions on the down-dip end of the plate interface, one from geodetic data and the other from tsunami waveforms, agree well except for slip beneath Cape Muroto in Shikoku. This suggests that aseismic slip also occurred on the plate interface beneath Cape Muroto."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276162829440","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40354526"},{"@type":"NRID","@value":"1000040354526"},{"@type":"NRID","@value":"9000412574281"},{"@type":"NRID","@value":"9000409024197"},{"@type":"NRID","@value":"9000403164411"},{"@type":"NRID","@value":"9000254263376"},{"@type":"NRID","@value":"9000254328142"},{"@type":"NRID","@value":"9000410904510"},{"@type":"NRID","@value":"9000254263385"},{"@type":"NRID","@value":"9000254825758"},{"@type":"NRID","@value":"9000000648914"},{"@type":"NRID","@value":"9000254740937"},{"@type":"NRID","@value":"9000381460716"},{"@type":"NRID","@value":"9000254263529"},{"@type":"NRID","@value":"9000018697958"},{"@type":"NRID","@value":"9000019100520"},{"@type":"NRID","@value":"9000404660977"},{"@type":"NRID","@value":"9000411772479"},{"@type":"NRID","@value":"9000398829701"},{"@type":"NRID","@value":"9000014232026"},{"@type":"NRID","@value":"9000296666651"},{"@type":"NRID","@value":"9000367411115"},{"@type":"NRID","@value":"9000387918869"},{"@type":"NRID","@value":"9000397827191"},{"@type":"NRID","@value":"9000248238848"},{"@type":"NRID","@value":"9000403551935"},{"@type":"NRID","@value":"9000408484439"},{"@type":"NRID","@value":"9000404660924"},{"@type":"NRID","@value":"9000398646680"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/ytanioka"}],"foaf:name":[{"@language":"en","@value":"Tanioka Yuichiro"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751136973440","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20178685"},{"@type":"NRID","@value":"1000020178685"},{"@type":"CINII_AUTHOR_ID","@value":"DA0947384X"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA0947384X#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA0947384X"},{"@type":"NRID","@value":"9000254263339"},{"@type":"NRID","@value":"9000399241466"},{"@type":"NRID","@value":"9000347165940"},{"@type":"NRID","@value":"9000390430428"},{"@type":"NRID","@value":"9000254753659"},{"@type":"NRID","@value":"9000254263382"},{"@type":"NRID","@value":"9000254263384"},{"@type":"NRID","@value":"9000254270833"},{"@type":"NRID","@value":"9000001755309"},{"@type":"NRID","@value":"9000000648917"},{"@type":"NRID","@value":"9000014234244"},{"@type":"NRID","@value":"9000254271184"},{"@type":"NRID","@value":"9000254740938"},{"@type":"NRID","@value":"9000000267586"},{"@type":"NRID","@value":"9000018697960"},{"@type":"NRID","@value":"9000019055038"},{"@type":"NRID","@value":"9000411546160"},{"@type":"NRID","@value":"9000254263526"},{"@type":"NRID","@value":"9000018699061"},{"@type":"NRID","@value":"9000014139690"},{"@type":"NRID","@value":"9000014232040"},{"@type":"NRID","@value":"9000000465424"},{"@type":"NRID","@value":"9000018698280"},{"@type":"NRID","@value":"9000016889995"},{"@type":"NRID","@value":"9000399241536"},{"@type":"NRID","@value":"9000254271000"},{"@type":"NRID","@value":"9000403163323"},{"@type":"NRID","@value":"9000399241513"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/kenji_satake"}],"foaf:name":[{"@language":"en","@value":"Satake Kenji"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geological Survey of Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"},{"@type":"NDL_BIB_ID","@value":"000000159136"},{"@type":"ISSN","@value":"13438832"},{"@type":"LISSN","@value":"13438832"},{"@type":"NCID","@value":"AA11211921"}],"prism:publicationName":[{"@language":"en","@value":"Earth, Planets and Space"},{"@language":"ja","@value":"Ｅａｒｔｈ，　Ｐｌａｎｅｔｓ　ａｎｄ　Ｓｐａｃｅ"},{"@language":"en","@value":"Earth Planets Space"},{"@language":"ja","@value":"Ｅａｒｔｈ　Ｐｌａｎｅｔｓ　Ｓｐａｃｅ"}],"dc:publisher":[{"@language":"en","@value":"Society of Geomagnetism and Earth, Planetary and Space Sciences, The Seismological Society of Japan, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences"},{"@language":"ja","@value":"地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会"}],"prism:publicationDate":"2001","prism:volume":"53","prism:number":"4","prism:startingPage":"235","prism:endingPage":"241"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/5770490"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I5770490"},{"@id":"https://dl.ndl.go.jp/pid/8833486"},{"@id":"https://link.springer.com/content/pdf/10.1186/BF03352380.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03352380/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03352380"}],"availableAt":"2001","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339198977664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological record of prehistoric tsunamis in Mugi town facing the Nankai Trough western 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Interpretation of the Slip Distributions Estimated Using Tsunami Waveforms for the 1944 Tonankai and 1946 Nankai Earthquakes."},{"@value":"次の南海トラフ巨大地震に備えて　　津波波形から推定された１９４４年東南海地震及び１９４６年南海地震のすべり量分布の解釈"},{"@language":"ja-Kana","@value":"ツナミ ハケイ カラ スイテイ サレタ 1944ネン トウナンカイ ジシン オヨビ 1946ネン ナンカイ ジシン ノ スベリ リョウ ブンプ ノ カイシャク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230790016","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Preparations for the Coming Large Earthquakes at the Nankai Trough. The Influence of Philipine Sea Plate Structure on Great Nankai Trough Earthquakes Inferred from the Rupture Process of the 1946 Nankai Earthquake."},{"@value":"次の南海トラフ巨大地震に備えて　　１９４６年南海地震震源過程から推定された南海トラフ巨大地震に対するフィリピン海プレート形状の影響"},{"@language":"ja-Kana","@value":"1946ネン ナンカイ ジシン シンゲン カテイ カラ スイテイ サレタ ナンカイ トラフキョダイジシン ニ タイスル フィリピンカイ プレート ケイジョウ ノ エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304347392","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Resonance Curve of the 1946 Nankai Tsunami at the Pacific Coast of Shikoku District"},{"@language":"ja","@value":"四国太平洋岸における1946年南海津波の共鳴曲線"},{"@language":"ja-Kana","@value":"シコク タイヘイヨウガン ニ オケル 1946ネン ナンカイ ツナミ ノ キョウメイ キョクセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240096128","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Researches on the tsunami deposits along the Nankai Trough:"},{"@language":"ja","@value":"南海トラフ沿岸の古津波堆積物の研究："},{"@value":"南海トラフ沿岸の古津波堆積物の研究 : その成果と課題"},{"@language":"ja-Kana","@value":"ナンカイ トラフ エンガン ノ コ ツナミ タイセキブツ ノ ケンキュウ : ソノ セイカ ト カダイ"},{"@value":"Researches on the tsunami deposits along the Nankai Trough: their achievements and upcoming challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511381120","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stress on the seismogenic and deep creep plate interface during the earthquake cycle in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511792896","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rupture process of the 2004 great Sumatra-Andaman earthquake estimated from tsunami waveforms"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512913024","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Onshore-offshore seismic transect from the eastern Nankai Trough to central Japan crossing a zone of the Tokai slow slip event"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513212672","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Error evaluation in acoustic positioning of a single transponder for seafloor crustal deformation measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513470848","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Silent earthquakes occurring in a stable-unstable transition zone and implications for earthquake prediction"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279779328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Researches on Earthquake Source Processes and Tsunami Generation Using Tsunami Data"},{"@language":"ja","@value":"津波データに基づく震源・津波発生過程の研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679282530688","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"西南日本の地震活動とテクトニクス"},{"@language":"en","@value":"Seismic Activity and Tectonics in Southwestern Japan"},{"@language":"ja-Kana","@value":"セイナン ニホン ノ ジシン カツドウ ト テクトニクス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488086400","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Splay fault and megathrust earthquake slip in the Nankai 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