{"@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/1361699995252579072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2003jb002393"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003JB002393"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003JB002393"}},{"identifier":{"@type":"NAID","@value":"30013330274"}}],"dc:title":[{"@value":"Rupture process of the 1944 Tonankai earthquake (<i>M</i><sub><i>s</i></sub> 8.1) from the inversion of teleseismic and regional seismograms"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We digitized teleseismic and regional records of the 1944 Tonankai earthquake. We used the multiple time window method to invert these records for the spatial and temporal distribution of slip and rake. We assume a 220 × 140 km fault with a spacing of 20 × 20 km and a maximum rupture velocity of 2.5 km/s. The inversion resolved an asperity along the accretionary wedge and under the Shima and Atsumi Peninsulas. The rupture propagated from southwest to northeast, and there was little slip near the hypocenter, consistent with the absence of uplift in the overlying submarine forearc basin. The peak slip is 2.3 m, and the total seismic moment is 2.4 × 10<jats:sup>28</jats:sup> dyn cm (<jats:italic>M</jats:italic><jats:sub><jats:italic>w</jats:italic></jats:sub> 8.2). We compared the predicted and observed vertical geodetic displacements and inferred that the limit of rupture is consistent with the change from subsidence to uplift west of the Atsumi Peninsula. This suggested that the earthquake did not rupture the plate interface in the Tokai gap. We modeled the tsunami using sea‐bottom displacements generated from this slip model. The tide gauge amplitudes and frequency content are consistent with those predicted. Resolution tests from inverting synthetic seismograms computed using a simplified slip model indicated that the combination of teleseismic and regional data sets best recovers the asperity locations and peak slips given similar station geometry and degrees of freedom. An inversion of the synthetic regional data set indicates that slip artifacts can occur early in the rupture process due to many clipped records while the inversion of synthetic teleseismic data set had less resolution and recovered only 50% of the peak slip.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995252579074","@type":"Researcher","foaf:name":[{"@value":"Gene A. Ichinose"}],"jpcoar:affiliationName":[{"@value":"URS Group, Inc.  Pasadena California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995252579076","@type":"Researcher","foaf:name":[{"@value":"Hong Kie Thio"}],"jpcoar:affiliationName":[{"@value":"URS Group, Inc.  Pasadena California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995252579075","@type":"Researcher","foaf:name":[{"@value":"Paul G. Somerville"}],"jpcoar:affiliationName":[{"@value":"URS Group, Inc.  Pasadena California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995252579072","@type":"Researcher","foaf:name":[{"@value":"Toshiaki Sato"}],"jpcoar:affiliationName":[{"@value":"Ohsaki Research Institute  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995252579073","@type":"Researcher","foaf:name":[{"@value":"Toru Ishii"}],"jpcoar:affiliationName":[{"@value":"Ohsaki Research Institute  Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/01480227"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2003-10","prism:volume":"108","prism:number":"B10","prism:startingPage":"2497"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003JB002393"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003JB002393"}],"createdAt":"2003-10-22","modifiedAt":"2023-10-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050289532527693952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geometrical dependence on the stress and slip tendency acting on the subduction megathrust of Nankai seismogenic zone off Kumano"},{"@value":"Geometrical dependence on the stress and slip tendency acting on the subduction megathrust of the Nankai seismogenic zone off Kumano"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229806477824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Near‐field observations of an offshore <i>M<sub>w</sub></i> 6.0 earthquake from an integrated seafloor and subseafloor monitoring network at the Nankai Trough, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004238580461056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"NanTroSEIZE Stage 3: NanTroSEIZE plate boundary deep riser 3"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004240201821568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"IODP Expedition 338: NanTroSEIZE Stage 3: NanTroSEIZE plate boundary deep riser 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seismograms"}]},{"@id":"https://cir.nii.ac.jp/crid/1390012158460889728","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Successive Occurrence of Large Earthquakes Along the Kuril Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280097920","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An Attempt at Simulation of Long Term Slow Slip Events and Seismic Cycle in the Tokai Region"},{"@value":"東海地域の長期的スロースリップイベントおよび地震サイクルの再現の試み"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280868864","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of the Short-Period Seismic Wave Radiation from the Historical Megathrust Earthquakes along the Nankai 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