{"@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/1360565166809021696.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/srep05631"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/srep05631"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/srep05631.pdf"}},{"identifier":{"@type":"PMID","@value":"25005351"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Structural control on the Tohoku earthquake rupture process investigated by 3D FEM, tsunami and geodetic data"}],"description":[{"notation":[{"@value":"The 2011 Tohoku earthquake (Mw = 9.1) highlighted previously unobserved features for megathrust events, such as the large slip in a relatively limited area and the shallow rupture propagation. We use a Finite Element Model (FEM), taking into account the 3D geometrical and structural complexities up to the trench zone, and perform a joint inversion of tsunami and geodetic data to retrieve the earthquake slip distribution. We obtain a close spatial correlation between the main deep slip patch and the local seismic velocity anomalies, and large shallow slip extending also to the North coherently with a seismically observed low-frequency radiation. These observations suggest that the friction controlled the rupture, initially confining the deeper rupture and then driving its propagation up to the trench, where it spreads laterally. These findings are relevant to earthquake and tsunami hazard assessment because they may help to detect regions likely prone to rupture along the megathrust, and to constrain the probability of high slip near the trench. Our estimate of ~40 m slip value around the JFAST (Japan Trench Fast Drilling Project) drilling zone contributes to constrain the dynamic shear stress and friction coefficient of the fault obtained by temperature measurements to ~0.68 MPa and ~0.10, respectively."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285532400325410","@type":"Researcher","foaf:name":[{"@value":"F. Romano"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207113","@type":"Researcher","foaf:name":[{"@value":"E. Trasatti"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207107","@type":"Researcher","foaf:name":[{"@value":"S. Lorito"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207104","@type":"Researcher","foaf:name":[{"@value":"C. Piromallo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207111","@type":"Researcher","foaf:name":[{"@value":"A. Piatanesi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207110","@type":"Researcher","foaf:name":[{"@value":"Y. Ito"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207112","@type":"Researcher","foaf:name":[{"@value":"D. Zhao"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207109","@type":"Researcher","foaf:name":[{"@value":"K. Hirata"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207108","@type":"Researcher","foaf:name":[{"@value":"P. Lanucara"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869978207105","@type":"Researcher","foaf:name":[{"@value":"M. Cocco"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20452322"}],"prism:publicationName":[{"@value":"Scientific Reports"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2014-07-09","prism:volume":"4","prism:number":"1","prism:startingPage":"5631"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by-nc-sa/4.0","https://creativecommons.org/licenses/by-nc-sa/4.0"],"url":[{"@id":"https://www.nature.com/articles/srep05631"},{"@id":"https://www.nature.com/articles/srep05631.pdf"}],"createdAt":"2014-07-09","modifiedAt":"2023-01-06","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Article","dc:title":"Article"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782142697600","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23224012"},{"@type":"JGN","@value":"JP23224012"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23224012/"}],"notation":[{"@language":"ja","@value":"大陸成長史と構造浸食：第二大陸の成長とマントルダイナミクス"},{"@language":"en","@value":"Growth of the second continent and mantle dynamics: Insights from a history of continental growth and tectonic erosion"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782277971584","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26000002"},{"@type":"JGN","@value":"JP26000002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26000002/"}],"notation":[{"@language":"ja","@value":"深海調査で迫るプレート境界浅部すべりの謎～その過去・現在"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257259871104","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26257206"},{"@type":"JGN","@value":"JP26257206"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26257206/"}],"notation":[{"@language":"ja","@value":"沈み込み帯浅部のスロースリップはトラフ軸まで到達するか？"},{"@language":"en","@value":"Slow slip to the trench  ?"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202741712896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tomography and Dynamics of Western-Pacific Subduction Zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760675301632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frontal wedge deformation near the source region of the 2011 Tohoku-Oki earthquake"},{"@value":"Frontal wedge deformation near the source region of the 2011 Tohoku‐Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001113987061504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Optimization Methods in Geophysical Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216113788160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tomography of the source zone of the 2015 M 7.8 Nepal earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708835840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stuck in the mud? Earthquake nucleation and propagation through accretionary forearcs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708853248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupture process of the 2011 Tohoku-Oki mega-thrust earthquake (M9.0) inverted from strong-motion data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708889344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Joint inversion of strong motion, teleseismic, geodetic, and tsunami datasets for the rupture process of the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218438847488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218438851584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232324606464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 2011 Tohoku earthquake (Mw 9.0) sequence and subduction dynamics in Western Pacific and East Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236002955136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Learning from crustal deformation associated with the M9 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518171998976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Offshore Postseismic Deformation of the 2011 Tohoku Earthquake Revisited: Application of an Improved GPS‐Acoustic Positioning Method Considering Horizontal Gradient of Sound Speed Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142423994240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Decade of Lessons Learned from the 2011 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144258208512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"From 3-Hz P Waves to 0 S 2: No Evidence of A Slow Component to the Source of the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144651932288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupture Process of the 2004 Sumatra–Andaman Earthquake from Tsunami  Waveform Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145369799808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three‐dimensional velocity structure, seismicity, and fault structure in the Parkfield Region, central California"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145762411264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Importance of horizontal seafloor motion on tsunami height for the 2011 Mw=9.0 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013247873637376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic site effects and the spatial interpolation of earthquake seismograms: Results using aftershocks of the 1986 North Palm Springs, California, earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691685598592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trench-normal variation in observed seafloor displacements associated with the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691686407040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693415558272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature Measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710917655936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dangers of Being Thin and Weak"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617906781952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fault parameters of the 1896 Sanriku Tsunami Earthquake estimated from Tsunami Numerical Modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621180573568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanism of tsunami earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621233476352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Inversion of high-rate (1 sps) GPS data for rupture process of the 11 March 2011 Tohoku earthquake (M<sub>w</sub>9.1)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164304786688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seafloor Displacement After the 2011 Tohoku‐oki Earthquake in the Northern Japan Trench Examined by Repeated Bathymetric Surveys"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168391795456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shallow Dynamic Overshoot and Energetic Deep Rupture in the 2011\n            <i>M</i>\n            <sub>w</sub>\n            9.0 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168540501632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Risk Assessment and Design of Prevention Structures for Enhanced Tsunami Disaster Resilience (RAPSODI)/Euro-Japan Collaboration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092458494080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical modeling of tsunami: advances and future challenges after the 2011 Tohoku earthquake and tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092891528064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Displacement Above the Hypocenter of the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641638988672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Survey of 2011 Tohoku earthquake tsunami inundation and run-up"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643366537216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-trench variation in seafloor displacements after the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846644791679360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time and Space Distribution of Coseismic Slip of the 2011 Tohoku Earthquake as Inferred from Tsunami Waveform Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065404800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Smooth and rapid slip near the Japan Trench during the 2011 Tohoku-oki earthquake revealed by a hybrid back-projection method"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567862099968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Along‐arc structural variation of the plate boundary at the Japan Trench margin: Implication of interplate coupling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568829692928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling near-field tsunami observations to improve finite-fault slip models for the 11 March 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569888109568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relocating the 2011 Tohoku-oki earthquakes (M 6.0–9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571509565568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic heterogeneity and anisotropy of the Honshu arc from the Japan Trench to the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855133802240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Forecasting strong subsequent earthquakes in Japan using an improved version of NESTORE machine learning algorithm"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043660472320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural controls on the Mw 9.0 2011 Offshore-Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045310069632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Limited overlap between the seismic gap and coseismic slip of the great 2010 Chile earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519906597248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamics of subduction and plate motion in laboratory experiments: Insights into the “plate tectonics” behavior of the Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993445708032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slab1.0: A three‐dimensional model of global subduction zone geometries"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993742595584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupture process of the 9 March, 2011 Mw 7.4 Sanriku-Oki, Japan earthquake constrained by jointly inverting teleseismic waveforms, strong motion data and GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994501509632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Twin ruptures grew to build up the giant 2011 Tohoku, Japan, earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994601648128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slip instability and state variable friction laws"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468699655680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Initiation of the great Mw 9.0 Tohoku–Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469239709056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonlinear one-dimensional seismic waveform inversion using simulated annealing"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470313930752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source process of the September 12, 2007, M<sub>W</sub> 8.4 southern Sumatra earthquake from tsunami tide gauge record inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943385017472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mapping the mantle wedge and interplate thrust zone of the northeast Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944153921792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Finite element inversion of DInSAR data from the Mw 6.3 L'Aquila earthquake, 2009 (Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944312784128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stability of Steady Frictional Slipping"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944582865152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geodetic imaging of plate motions, slip rates, and partitioning of deformation in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944587753472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Further evidence for the compound nature of slow earthquakes: The Prince Edward Island earthquake of April 28, 1997"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945251347968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slip distribution of the 2003 Tokachi‐oki <i>M</i><sub><i>w</i></sub> 8.1 earthquake from joint inversion of tsunami waveforms and geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945548311680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural heterogeneities around the megathrust zone of the 2011 Tohoku earthquake from tomographic inversion of onshore and offshore seismic observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419007623040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tsunami generation by horizontal displacement of ocean bottom"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893362465152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stable creeping fault segments can become destructive as a result of dynamic weakening"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893791324672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Automatic estimation of large residual statics corrections"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895037841664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mapping the Tohoku forearc: Implications for the mechanism of the 2011 East Japan earthquake (Mw 9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368763690752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Kinematics and source zone properties of the 2004 Sumatra‐Andaman earthquake and tsunami: Nonlinear joint inversion of tide gauge, satellite altimetry, and GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369082335616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A slump in the trench: Tracking the impact of the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369322883456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Scaling of the Source Dimensions of Interface and Intraslab Subduction-zone Earthquakes with Moment Magnitude"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369747480576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Clues from joint inversion of tsunami and geodetic data of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843865944960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic features of the Japan Trench convergent margin off Sanriku, northeastern Japan, revealed by multichannel seismic reflection data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845538622848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural characteristics off Miyagi forearc region, the Japan Trench seismogenic zone, deduced from a wide-angle reflection and refraction study"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319368043648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geodetic slip model of the 2011 M9.0 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319548045696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupture process of the 2007 Niigata‐ken Chuetsu‐oki earthquake by non‐linear joint inversion of strong motion and GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320109014656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source Rupture Models for the Mw 9.0 2011 Tohoku Earthquake from Joint Inversions of High-Rate Geodetic and Seismic Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793235750016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth‐integrated, non‐hydrostatic model for wave breaking and run‐up"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795803207296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Simulation of the 2011 Tohoku Tsunami Based on a New Transient FEM Co-seismic Source: Comparison to Far- and Near-Field Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795855598336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth‐integrated, non‐hydrostatic model with grid nesting for tsunami generation, propagation, and run‐up"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268510069888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High‐frequency source radiation during the 2011 Tohoku‐Oki earthquake, Japan, inferred from KiK‐net strong‐motion seismograms"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269343338880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Towards inferring earthquake patterns from geodetic observations of interseismic coupling"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269799006592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Insights from the great 2011 Japan earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270800977024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source Process of the 2011 Tohoku Earthquake Estimated from the Joint Inversion of Teleseismic Body Waves and Geodetic Data Including Seafloor Observation Data: Source Model with Enhanced Reliability by Using Objectively Determined Inversion Settings"}]},{"@id":"https://cir.nii.ac.jp/crid/1370565166809021732","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1390564238096711936","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re-examination of the Tsunami Source Model of the 2011 off Pacific coast of Tohoku Earthquake"},{"@language":"ja","@value":"2011年東北地方太平洋沖震の津波断層モデルの再検討"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417119872384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological structures controlled the rupture process of the 2011 M9.0 Tohoku-Oki earthquake in the Northeast Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317068449664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data : was the asperity in Miyagi-oki ruptured？"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792045157120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source process of the 2011 off the Pacific coast of Tohoku Earthquake with the combination of teleseismic and strong motion data"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792045167232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tsunami source of the 2011 off the Pacific coast of Tohoku Earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/srep05631"},{"@type":"KAKEN","@value":"PRODUCT-13785600"},{"@type":"KAKEN","@value":"PRODUCT-15187469"},{"@type":"KAKEN","@value":"PRODUCT-15207573"},{"@type":"OPENAIRE","@value":"doi_dedup___::3bf8b6ea4fa44b6dc091a8eb6540178c"},{"@type":"CROSSREF","@value":"10.1029/2018jb017135_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.5610/jaee.19.2_25_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2016.01.008_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1002/2017gl075839_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1142/s057856341640012x_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2020.103498_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1130/ges01531.1_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1126/sciadv.1700113_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01212-3_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2025.102016_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2014.10.022_references_DOI_Odnj9uoYN3rAS8WUOR2U4GUl8wE"}]}