{"@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/1360574096021363072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2001jb000424"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001JB000424"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001JB000424"}},{"identifier":{"@type":"NAID","@value":"80015132433"}}],"dc:title":[{"@value":"Crustal structure across the coseismic rupture zone of the 1944 Tonankai earthquake, the central Nankai Trough seismogenic zone"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Differences in the coseismic rupture process between the 1944 Tonankai   and the 1946 Nankaido earthquakes have been studied by many fault models. To   understand what factors control coseismic rupture zones, it is important to   investigate differences in deep crustal structures of the rupture zones between the   1944 and 1946 earthquakes. The previously published crustal structure of the rupture   zone of the 1946 earthquake shows that the coseismic rupture extends to the   Neogene‐Quaternary accretionary prism. However, little is known about the structure   of the rupture zone of the 1944 earthquake. To obtain a complete image of the   seismogenic zone of the 1944 earthquake, a wide‐angle seismic survey was performed   across the presumed coseismic rupture zone of the 1944 earthquake from ocean to   land. Our model for the crustal structure is based on ocean bottom seismographic   data. The crustal structure appears characteristic for subducting oceanic crust and   a Neogene‐Quaternary accretionary prism bounded by an island arc crust. The   Neogene‐Quaternary accretionary prism reaches a maximum thickness of 7 km at 50 km   distance landward from the deformation front. The subducting oceanic crust can be   traced down to 35 km. The subduction angle becomes steeper landward, reaching up to   11° beneath the island arc crust. The depth of the top of subducting oceanic   crust at the downdip limit of the rupture zone is 23 km, while the updip limit is   located beneath the island arc upper crust. Similar structures of the updip and   downdip limits are also published for several other subduction zones.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380567005542273156","@type":"Researcher","foaf:name":[{"@value":"Ayako Nakanishi"}],"jpcoar:affiliationName":[{"@value":"Institute for Frontier Research on Earth Evolution Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096021363073","@type":"Researcher","foaf:name":[{"@value":"Narumi Takahashi"}],"jpcoar:affiliationName":[{"@value":"Deep Sea Research Department Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579818731592320","@type":"Researcher","foaf:name":[{"@value":"Jin‐Oh Park"}],"jpcoar:affiliationName":[{"@value":"Institute for Frontier Research on Earth Evolution Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096021363075","@type":"Researcher","foaf:name":[{"@value":"Seiichi Miura"}],"jpcoar:affiliationName":[{"@value":"Institute for Frontier Research on Earth Evolution Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096021363078","@type":"Researcher","foaf:name":[{"@value":"Shuichi Kodaira"}],"jpcoar:affiliationName":[{"@value":"Institute for Frontier Research on Earth Evolution Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096021363080","@type":"Researcher","foaf:name":[{"@value":"Yoshiyuki Kaneda"}],"jpcoar:affiliationName":[{"@value":"Institute for Frontier Research on Earth Evolution Japan Marine Science and Technology Center  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096021363072","@type":"Researcher","foaf:name":[{"@value":"Naoshi Hirata"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801200163968","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70151719"},{"@type":"NRID","@value":"1000070151719"},{"@type":"NRID","@value":"9000254753796"},{"@type":"NRID","@value":"9000254262888"},{"@type":"NRID","@value":"9000254270741"},{"@type":"NRID","@value":"9000254741760"},{"@type":"NRID","@value":"9000004602253"},{"@type":"NRID","@value":"9000410904541"},{"@type":"NRID","@value":"9000413694882"},{"@type":"NRID","@value":"9000254753595"},{"@type":"NRID","@value":"9000410949604"},{"@type":"NRID","@value":"9000254270803"},{"@type":"NRID","@value":"9000400157697"},{"@type":"NRID","@value":"9000000774168"},{"@type":"NRID","@value":"9000391405458"},{"@type":"NRID","@value":"9000254753522"},{"@type":"NRID","@value":"9000254263101"},{"@type":"NRID","@value":"9000001755402"},{"@type":"NRID","@value":"9000254262834"},{"@type":"NRID","@value":"9000410949332"},{"@type":"NRID","@value":"9000403549786"},{"@type":"NRID","@value":"9000283228254"},{"@type":"NRID","@value":"9000391402104"},{"@type":"NRID","@value":"9000391405187"},{"@type":"NRID","@value":"9000410949812"},{"@type":"NRID","@value":"9000254753590"},{"@type":"NRID","@value":"9000403551953"},{"@type":"NRID","@value":"9000258411897"},{"@type":"NRID","@value":"9000254271201"},{"@type":"NRID","@value":"9000254741494"},{"@type":"NRID","@value":"9000017413614"},{"@type":"NRID","@value":"9000254753539"},{"@type":"NRID","@value":"9000254262969"},{"@type":"NRID","@value":"9000254270771"},{"@type":"NRID","@value":"9000410949853"},{"@type":"NRID","@value":"9000410948881"},{"@type":"NRID","@value":"9000254262818"},{"@type":"NRID","@value":"9000254270790"},{"@type":"NRID","@value":"9000258415648"},{"@type":"NRID","@value":"9000004598565"},{"@type":"NRID","@value":"9000254740635"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/iwasaki-t"}],"foaf:name":[{"@value":"Takaya Iwasaki"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096021363074","@type":"Researcher","foaf:name":[{"@value":"Masao Nakamura"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2002-01","prism:volume":"107","prism:number":"B1","prism:startingPage":"1"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001JB000424"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001JB000424"}],"createdAt":"2002-10-27","modifiedAt":"2023-10-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004230175252224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A synthesis of heat flow determinations and thermal modeling along the Nankai Trough, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231402358528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detectability analysis of interplate fault slips in the Nankai subduction thrust using seafloor 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カツドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305456768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"紀伊半島南部地域の重力異常と深部比抵抗構造から推定される地熱構造"},{"@language":"en","@value":"Geothermal Structure of the Southern Part of the Kii Peninsula Estimated from the Gravity Anomaly and the Deep Resistivity Structure"},{"@language":"ja-Kana","@value":"キイハントウ ナンブ チイキ ノ ジュウリョク イジョウ ト シンブヒ テイコウ コウゾウ カラ スイテイ サレル チネツ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205317582464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Orientations of DONET seismometers estimated from seismic waveforms"},{"@value":"地震動波形から推定したDONET地震計の方位"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205317616896","@type":"Article","resourceType":"学術雑誌論文(journal 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Experiment"},{"@language":"ja","@value":"南海トラフ地震発生帯掘削計画の概要"},{"@language":"ja-Kana","@value":"ナンカイ トラフ ジシン ハッセイタイ クッサク ケイカク ノ ガイヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237224448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Shallow, deep slow earthquake families associated with the subduction of the Philippine Sea plate"},{"@language":"ja","@value":"フィリピン海プレート沈み込みに伴う浅部および深部スロー地震群"},{"@language":"ja-Kana","@value":"フィリピンカイ プレート シズミ コミ ニ トモナウ センブ オヨビ シンブ スロー ジシングン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206458910080","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aftershock Observation of the 2004 off the Kii Peninsula Earthquake Using Ocean Bottom Seismometers"},{"@value":"海底地震計を用いた2004年紀伊半島南東沖の地震の余震観測"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512002048","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-period ground motion simulation in the Kinki area during the M<SUB>J</SUB> 7.1 foreshock of the 2004 off the Kii peninsula earthquakes"},{"@value":"Long-period ground motion simulation in the Kinki area during the MJ 7.1 foreshock of the 2004 off the Kii peninsula earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512003072","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Resistivity image of the Philippine Sea Plate around the 1944 Tonankai earthquake zone deduced by Marine and Land MT surveys"}]},{"@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/1390282679282196224","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"震源分布からみた伊勢湾から四国西部にかけてのフィリピン海スラブの形状"},{"@language":"en","@value":"Geometry of the Seismic Philippine Sea Slab beneath the Region from Ise Bay to Western Shikoku, Southwest Japan"},{"@language":"ja-Kana","@value":"シンゲン ブンプ カラ ミタ イセワン カラ シコク セイブ ニ カケテ ノ フィリピンカイ スラブ ノ ケイジョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472844288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A high-resolution 3D seismic reflection survey and prestack depth imaging in the Nankai Trough off southeast Kii Peninsula"},{"@language":"ja","@value":"紀伊半島南東沖南海トラフでの高分解能3次元反射法地震探査と重合前深度マイグレーション処理"},{"@language":"ja-Kana","@value":"キイ ハントウ ナントウオキ ナンカイ トラフ デノ コウブンカイノウ 3ジゲン ハンシャホウ ジシン タンサ ト ジュウゴウマエ シンド マイグレーション ショリ"},{"@value":"High-resolution 3D seismic reflection survey and prestack depth imaging in the Nankai Trough off southeast Kii Peninsula"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473543552","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Neotectonics in and around the Kinki Triangle in relation to the geometry of the subducted Philippine Sea plate"},{"@language":"ja","@value":"沈み込んだフィリピン海プレートの形状からみた近畿三角帯周辺のネオテクトニクス"},{"@language":"ja-Kana","@value":"シズミコンダ フィリピンカイ プレート ノ ケイジョウ カラ ミタ キンキ サンカクタイ シュウヘン ノ ネオテクトニクス"},{"@value":"Neotectonocs in and around the Kinki Triangle in relation to the geometry of the subducted Philippine Sea plate (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488603264","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An improved double-difference earthquake location algorithm using <I>sP</I> phases: application to the foreshock and aftershock sequences of the 2004 earthquake offshore of the Kii peninsula, Japan (M<SUB>w</SUB>=7.5)"},{"@value":"An improved double-difference earthquake location algorithm using sP phases: application to the foreshock and aftershock sequences of the 2004 earthquake offshore of the Kii peninsula, Japan (Mw=7.5)"},{"@language":"ja-Kana","@value":"improved double difference earthquake location algorithm using sP phases application to the foreshock and aftershock sequences of the 2004 earthquake offshore of the Kii peninsula Japan Mw 7 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