{"@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/2051714792045167232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"NDL_BIB_ID","@value":"9102971"}},{"identifier":{"@type":"DOI","@value":"10.5047/eps.2011.06.010"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/9102971"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/9102971"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.5047/eps.2011.06.010"}},{"identifier":{"@type":"NAID","@value":"20001073492"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Tsunami source of the 2011 off the Pacific coast of Tohoku Earthquake"}],"dcterms:alternative":[{"@value":"Tsunami source of the 2011 off the Pacific coast of Tohoku Earthquake"}],"dc:language":"en","description":[{"notation":[{"@value":"収集根拠 : オンライン資料収集制度"},{"@value":"資料形態 : テキストデータ"},{"@value":"コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326222826752","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60442836"},{"@type":"NRID","@value":"1000060442836"},{"@type":"NRID","@value":"9000003141509"},{"@type":"NRID","@value":"9000003139860"},{"@type":"NRID","@value":"9000391404714"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0162898"}],"foaf:name":[{"@value":"Yushiro Fujii"}]},{"@id":"https://cir.nii.ac.jp/crid/2061714792045167234","@type":"Researcher","foaf:name":[{"@value":"Shin’ichi Sakai"}]},{"@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":[{"@value":"Kenji Satake"}]}],"publication":{"publicationIdentifier":[{"@type":"ISSN","@value":"18805981"},{"@type":"LISSN","@value":"13438832"},{"@type":"PISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/13438832"}],"prism:publicationName":[{"@value":"EPS : Earth, Planets and Space"}],"dc:publisher":[{"@value":"Terrapub"}],"prism:publicationDate":"2011-09-27","prism:volume":"63(7)","prism:startingPage":"815","prism:endingPage":"820"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/digimeta/9102971"},{"@id":"https://dl.ndl.go.jp/pid/9102971"},{"@id":"http://link.springer.com/content/pdf/10.5047/eps.2011.06.010"}],"foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Space%20and%20Planetary%20Science","dc:title":"Space and Planetary Science"},{"@id":"https://cir.nii.ac.jp/all?q=Geology","dc:title":"Geology"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257044979456","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21310113"},{"@type":"JGN","@value":"JP21310113"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-21310113/"}],"notation":[{"@language":"ja","@value":"古津波調査に基づく環太平洋巨大地震の津波高確率予測"},{"@language":"en","@value":"Probabilistic estimates of tsunami heights from great earthquakes around the Pacific Ocean based on paleotsunami surveys"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050008244166887424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fault weakening caused by smectite swelling"}]},{"@id":"https://cir.nii.ac.jp/crid/1050025031474806912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cohesional Slip on a Plate Subduction Boundary During a Large Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810730081920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentary features observed in the tsunami deposits at Rikuzentakata City"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506456864128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Scaling of early afterslip velocity and possible detection of tsunami-induced subsidence by GPS measurements immediately after the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506457964032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Megaquake cycle at the Tohoku subduction zone with thermal fluid pressurization near the surface"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981429018368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981430888448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Opal-CT in chert beneath the toe of the Tohoku margin and its influence on the seismic aseismic transition in subduction zones"},{"@value":"Opal‐CT in chert beneath the toe of the Tohoku margin and its influence on the seismic aseismic transition in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760694761856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Potential tsunamigenic faults of the 2011 off the Pacific coast of Tohoku Earthquake"},{"@value":"Potential tsunamigenic faults of the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050850247206947840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source model for strong ground motion generation in the frequency range 0.1–10 Hz during the 2011 Tohoku earthquake"},{"@value":"Source model for strong ground motion generation in 0.1–10 Hz during the 2011 Tohoku earthquake"},{"@value":"Source model for strong ground motion in 0.1–10 Hz during the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456404213632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Back-Projection Imaging of a Tsunami Excitation Area With Ocean-Bottom Pressure Gauge Array Data"},{"@value":"Back‐Projection Imaging of a Tsunami Excitation Area With Ocean‐Bottom Pressure Gauge Array Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456408281216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Exchangeable cation composition of the smectite-rich plate boundary fault at the Japan Trench"},{"@value":"Exchangeable cation composition of the smectite‐rich plate boundary fault at the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348554112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Traveltime delay and initial phase reversal of distant tsunamis coupled with the self‐gravitating elastic Earth"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214351373440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An Adjoint Sensitivity Method Applied to Time Reverse Imaging of Tsunami Source for the 2009 Samoa Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215254631808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami Heights along the Pacific Coast of Northern Honshu Recorded from the 2011 Tohoku and Previous Great Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215254647552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New Insights into the Source of the Makran Tsunami of 27 November 1945 from Tsunami Waveforms and Coastal Deformation Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916334976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Documenting large earthquakes similar to the 2011 Tohoku-oki earthquake from sediments deposited in the Japan Trench over the past 1500 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708853248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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/1360002216708861824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"3D modeling of the cycle of a great Tohoku-oki earthquake, considering frictional behavior at low to high slip velocities"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708889344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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/1360002216799083392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Prevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002217556329600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fast numerical simulation of crustal deformation using a three-dimensional high-fidelity model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218438847488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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":["isReferencedBy"],"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/1360004230362731136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interplate Coupling in and Around the Rupture Area of the 2011 Tohoku Earthquake (M9.0) Before Its Occurrence Based on Terrestrial and Seafloor Geodetic Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231143777280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami Source Inversion Using Tide Gauge and DART Tsunami Waveforms of the 2017 Mw8.2 Mexico Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135292416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Extension of continental crust by anelastic deformation during the 2011 Tohoku-oki earthquake: The role of extensional faulting in the generation of a great tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135326848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami source of the 2011 Tohoku earthquake detected by an ocean-bottom magnetometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232451070080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The March 11, 2011 Tōhoku M9.0 earthquake-induced tsunami and coastal inundation along the Japanese coast: A model assessment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523511680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Source of high tsunamis along the southernmost Ryukyu trench inferred from tsunami stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233291076608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami Waves and Tsunami‐Induced Natural Oscillations Determined by HF Radar in Ise Bay, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233291892608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Periodic Oscillations in the <i>D</i> Region Ionosphere After the 2011 Tohoku Earthquake Using LF Standard Radio Waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236002473216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pelagic smectite as an important factor in tsunamigenic slip along the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236003004416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Laboratory measurements quantifying elastic properties of accretionary wedge sediments: Implications for slip to the trench during the 2011 Mw 9.0 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236254739712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological studies in tsunami research since the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004238580344320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Japan Trench Fast Drilling Project (JFAST)"}]},{"@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/1360009142863993472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Method of Real-Time Tsunami Detection Using Ensemble Empirical Mode Decomposition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142885214848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large Coseismic Slip to the Trench During the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870443278592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abrupt water temperature increases near seafloor during the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021395469197056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Progress in modeling the Tohoku-oki megathrust earthquake cycle and associated crustal deformation processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022306717277312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Full Waveform Inversion for Imaging Faulted Structures; a Case Study from Japan Trench Forearc Slope"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025030626632064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic activity around shallow plate boundary near westernmost Nankai Trough revealed by ocean bottom seismometer observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689327422592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"REGARD: A new GNSS‐based real‐time finite fault modeling system for GEONET"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691685615616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 2011 Japan tsunami current velocity measurements from survivor videos at Kesennuma Bay using LiDAR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691686407040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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/1360283691783878144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693415358720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress State in the Largest Displacement Area of the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693563780224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nationwide Post Event Survey and Analysis of the 2011 Tohoku Earthquake Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704780066944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structure and lithology of the Japan Trench subduction plate boundary fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704785337856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Time Domain Simulation of Tsunami‐Generated Electromagnetic Fields: Application to the 2011 Tohoku Earthquake Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704785364480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Improved Phase Corrections for Transoceanic Tsunami Data in Spatial and Temporal Source Estimation: Application to the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705151956864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐dimensional tsunami propagation simulations using an unstructured mesh finite element model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706358491776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of mass sedimentation events after the 2011 off the Pacific coast of Tohoku Earthquake on benthic prokaryotes and meiofauna inhabiting the upper bathyal sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707111967488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami run-up associated with co-seismic thrust slip produced by the 2011 Mw 9.0 Off Pacific Coast of Tohoku earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707264121088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A computational model for large-scale oil spill fires on water in tsunamis: Simulation of oil spill fires at Kesennuma Bay in the 2011 Great East Japan Earthquake and Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707329611648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical and micropaleontological impacts caused by the 2011 Tohoku-oki tsunami in Matsushima Bay, northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711828442880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Advances in earthquake and tsunami sciences and disaster risk reduction since the 2004 Indian ocean tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711828553600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami source and inundation features around Sendai Coast, Japan, due to the November 22, 2016 Mw 6.9 Fukushima earthquake"}]},{"@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/1360292617909532032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New, improved version of generic mapping tools released"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620354778496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Traces of Tsunami Preserved in Inter-Tidal Lacustrine and Marsh Deposits: Some Examples from Northeast Japan"}]},{"@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/1360292621388170624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surface deformation due to shear and tensile faults in a half-space"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643708664960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Review on Recent Progress in Near-Field Tsunami Forecasting Using Offshore Tsunami Measurements: Source Inversion and Data Assimilation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643778618368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Correlation between molecular microbial community and nitrogen cycling on ornithogenic soil affected by tsunami in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298337112216320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stick-slip behavior of a clayey crustal fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298755637399552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Simulated effectiveness of coastal forests on reduction in loss of lives from a tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869625344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Change in stress field after the 2011 great Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869657984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fluid transport properties in sediments and their role in large slip near the surface of the plate boundary fault in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869690496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural and thermal control of seismic activity and megathrust rupture dynamics in subduction zones: Lessons from the Mw 9.0, 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869739008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Re-estimated fault model of the 17th century great earthquake off Hokkaido using tsunami deposit data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166056219008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Accurate numerical simulation of the far-field tsunami caused by the 2011 Tohoku earthquake, including the effects of Boussinesq dispersion, seawater density stratification, elastic loading, and gravitational potential change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662274560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Atmospheric boundary waves excited by the tsunami generation related to the 2011 great Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662987392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Regional extent of the large coseismic slip zone of the 2011 Mw 9.0 Tohoku‐Oki earthquake delineated by on‐fault aftershocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166809021696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural control on the Tohoku earthquake rupture process investigated by 3D FEM, tsunami and geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168562352768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial variability in sediment lithology and sedimentary processes along the Japan Trench: use of deep-sea turbidite records to reconstruct past large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757119488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in seismicity before and after the 2011 Tohoku earthquake around its southern limit revealed by dense ocean bottom seismic array data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181097159424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fault Slip Distribution of the 2016 Fukushima Earthquake Estimated from Tsunami Waveforms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088746880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Aftershocks near the updip end of the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182306256640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Possible submarine tsunami deposits on the outer shelf of Sendai Bay, Japan resulting from the 2011 earthquake and tsunami off the Pacific coast of Tohoku"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185956366080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depth-varying structural characters in the rupture zone of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186250363776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global Positioning System (GPS) and GPS-Acoustic Observations: Insight into Slip Along the Subduction Zones Around Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186805261952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Different depths of near-trench slips of the 1896 Sanriku and 2011 Tohoku earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567189440865920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Analysis of Spatio-Temporal Tsunami Source Models for Reproducing Tsunami Inundation Features"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568465785932672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural-morphological and sedimentary features of forearc slope off Miyagi, NE Japan: implications for development of forearc basins and plumbing systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568468306041984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tomography of the source zone of the great 2011 Tohoku earthquake"}]},{"@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/1360574092891912704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismological evidence for a lithospheric normal faulting — the Sanriku earthquake of 1933"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118746056576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development and Operation of an Ocean Bottom Cable Seismic and Tsunami (OBCST) Observation System in the Source Region of the Tohoku‐oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584341823557120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface Physicochemical Properties of Smectite‐Rich Fault Gouge: A Case Study of the Japan Trench Plate‐Boundary Fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379392270464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Adjoint Synthesis for Trans‐Oceanic Tsunami Waveforms and Simultaneous Inversion of Fault Geometry and Slip Distribution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380157109760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Revising the seismic source of the 1979 Tumaco-Colombia earthquake (Mw = 8.1) for future tsunami hazard assessment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639279179008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fault slip distribution of the 2014 Iquique, Chile, earthquake estimated from ocean‐wide tsunami waveforms and GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846306944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A unified source model for the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641639189888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quasi real‐time fault model estimation for near‐field tsunami forecasting based on RTK‐GPS analysis: Application to the 2011 Tohoku‐Oki earthquake (<i>M</i><sub>w</sub> 9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654734697856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami source uncertainty estimation: The 2011 Japan tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654738018944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complete Implementation of the Green's Function Based Time Reverse Imaging and Sensitivity Analysis of Reversed Time Tsunami Source Inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655052334592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High‐resolution seismic imaging in the Japan Trench axis area off Miyagi, northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655464631808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evidence for Mass Transport Deposits at the IODP JFAST-Site in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656073912832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quasi-Dynamic 3D Modeling of the Generation and Afterslip of a Tohoku-oki Earthquake Considering Thermal Pressurization and Frictional Properties of the Shallow Plate Boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065384320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Runaway slip to the trench due to rupture of highly pressurized megathrust beneath the middle trench slope: The tsunamigenesis of the 2011 Tohoku earthquake off the east coast of northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065404800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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/1360848658218369664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pore pressure distribution along plate interface that causes a shallow asperity of the 2011 great Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567815319936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigating a tsunamigenic megathrust earthquake in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593678873728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid assessment of tsunami source impacts on low-lying coastal areas using offshore wave superposition and static sweep of onshore terrain"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861704795763840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Connection between high pore-fluid pressure and frictional instability at tsunamigenic plate boundary fault of 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855565730816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diatom and Radiolarian Biostratigraphy in the Vicinity of the 2011 Tohoku Earthquake Source Fault in\n                    <scp>IODP</scp>\n                    Hole 343‐\n                    <scp>C0019E</scp>\n                    of\n                    <scp>JFAST</scp>"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131415403399296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Residual Tsunami Risk After the Reconstruction Projects in Fukushima Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520530791808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tsunami Source of the 2004 Sumatra–Andaman Earthquake Inferred from Tide Gauge and Satellite Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694369969999872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Performance Evaluation of Multi-UAV System in Post-Disaster Application: Validated by HITL Simulator"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694371173476992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami Modeling for the Deep Sea and Inside Focal Areas"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975841749509760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Time lapse seismic analysis of the Tohoku-Oki 2011 earthquake"}]},{"@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/1390001204306119040","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"断層力学·モデリングに基づく震源過程の多面的研究"},{"@language":"en","@value":"Source Processes Based on Fault Mechanics and Modeling"},{"@value":"断層力学・モデリングに基づく震源過程の多面的研究"},{"@language":"ja-Kana","@value":"ダンソウ リキガク ・ モデリング ニ モトズク シンゲン カテイ ノ タメンテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319012608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influences of Time Integration on the Accuracy of Inversion based on Ocean Radar"},{"@language":"ja","@value":"海洋レーダを利用したインバージョンに対するレーダ観測時間の影響"},{"@language":"ja-Kana","@value":"カイヨウ レーダ オ リヨウ シタ インバージョン ニ タイスル レーダ カンソク ジカン ノ エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319191424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami Damage Simulation of KOIZUMI Bridge"},{"@language":"ja","@value":"小泉大橋の津波被害再現解析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319254656","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami Simulation Using VOF Method and Falling Mechanism of a Building in Tohoku-Pacific Coast Earthquake"},{"@language":"ja","@value":"VOF法を用いた東北地方太平洋沖地震津波の再現と建物の転倒メカニズムの解明"},{"@language":"ja-Kana","@value":"VOFホウ オ モチイタ トウホク チホウ タイヘイヨウオキ ジシン ツナミ ノ サイゲン ト タテモノ ノ テントウ メカニズム ノ カイメイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319431424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami Source Inversion for the 2011 off the Pacific Coast of Tohoku Earthquake with Geodetic Data from the Global Positioning System and Its Applicability"},{"@language":"ja","@value":"GPS地殻変位データを用いた東北地方太平洋沖地震津波の波源域の逆推定およびその精度に関する研究"},{"@language":"ja-Kana","@value":"GPS チカク ヘンイ データ オ モチイタ トウホク チホウ タイヘイヨウオキ ジシン ツナミ ノ ナミ ゲンイキ ノ ギャクスイテイ オヨビ ソノ セイド ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320047104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"DISASTER REDUCTION FUNCTION OF SEAWALLS AGAINST OVERFLOWING CATASTROPHIC TSUNAMI"},{"@value":"越流を伴う巨大津波に対する海岸堤防の減災機能の検証"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320215168","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波波力に基づく建物倒壊を考慮した津波解析の検討"},{"@language":"en","@value":"STUDY OF THE TSUNAMI SIMULATION INCLUDING BUILDING COLLAPSE DUE TO TSUNAMI WAVE FORCE"},{"@language":"ja-Kana","@value":"ツナミハリョク ニ モトズク タテモノ トウカイ オ コウリョ シタ ツナミ カイセキ ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205349624320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"CLARIFICATION OF TSUNAMI WAVEFORMS ACTING ON A BRIDGE STRUCTURE SUBJECTED TO THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE TSUNAMI"},{"@language":"ja","@value":"橋梁構造物に入射する津波の時系列波形とその類型化"},{"@value":"Development of Damage Functions on Road Infrastructures Subjected to Extreme Ground Excitations by Analyzing Damage in the 2011 off the Pacific Coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205353075840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻変位データを用いた地震断層の走向，傾斜角およびすべり量の推定精度に関する研究"},{"@language":"en","@value":"GEODETIC DATA INVERSION USING A BAYESIAN INFORMATION CRITERION FOR STRIKE, DIP AND SPATIAL SLIP DISTRIBUTION OFAFAULT"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205353393920","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北上川における津波の河川遡上と津波氾濫流解析から導かれる現地観測データの解釈"},{"@language":"en","@value":"DISUCUSSION ABOUT OBSERVED DATA BASED ON THE SIMULATION OF TSUNAMI RUN-UP AND INUNDATION IN THE KITAKAMI RIVER"},{"@language":"ja-Kana","@value":"キタカミガワ ニ オケル ツナミ ノ カセン ソジョウ ト ツナミ ハンランリュウ カイセキ カラ ミチビカレル ゲンチ カンソク データ ノ カイシャク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205357507328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2011年東北地方太平洋沖地震における強震動生成域からの長周期地震動"},{"@language":"en","@value":"Long-Period Ground Motions from Strong Motion Generation Area during the 2011 Mw 9.0 the Pacific Coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205358318720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analysis and Verification of the 2011 Tohoku Earthquake Tsunami at Nuclear Power Plant Sites"},{"@language":"ja","@value":"原子力サイトにおける2011 東北地震津波の検証"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240354304","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The generation process of the Tohoku earthquake:"},{"@language":"ja","@value":"東北地方太平洋沖地震の発生過程："},{"@value":"東北地方太平洋沖地震の発生過程 : なぜM9が発生したのか?"},{"@language":"ja-Kana","@value":"トウホク チホウ タイヘイヨウオキ ジシン ノ ハッセイ カテイ : ナゼ M9 ガ ハッセイ シタ ノ カ?"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241265152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Absolute strain release in the 2011 Tohoku-oki Earthquake:"},{"@language":"ja","@value":"2011年東北地方太平洋沖地震による絶対歪みの解放："},{"@value":"2011年東北地方太平洋沖地震による絶対歪みの解放 : 遠地実体波インバージョン解析と動的摩擦弱化"},{"@language":"ja-Kana","@value":"2011ネン トウホク チホウ タイヘイヨウオキ ジシン ニ ヨル ゼッタイ ヒズミ ノ カイホウ : エンチ ジッタイハ インバージョン カイセキ ト ドウテキ マサツ ジャッカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288089695104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"確率論的津波ハザード評価におけるGR則の適用可能性の検討"},{"@language":"en","@value":"BASIC EXAMINATION OF APPLICABILITY OF GR LAW IN PROBABILISTIC TSUNAMI HAZARD ASSESSMENT"},{"@language":"ja-Kana","@value":"カクリツロンテキ ツナミ ハザード ヒョウカ ニ オケル GRソク ノ テキヨウ カノウセイ ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288150830848","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Radiation and Generation of Short- and Long-Period Ground Motions from the 2011 Off Tohoku, Japan, bi M<sub>w</sub>9.0 Earthquake"},{"@value":"Radiation and Generation of Short- and Long-Period Ground Motions from the 2011 Off Tohoku, Japan,<i>M<sub>w</sub></i>9.0 Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288151348736","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review: Source Models of the 2011 Tohoku Earthquake and Long-Term Forecast of Large Earthquakes"},{"@value":"Source Models of the 2011 Tohoku Earthquake and Long-Term Forecast of Large Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390012801490264192","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Comparison between Slip Distributions in the 2011 Tohoku Earthquake Tsunami Evaluated by Different Methods for Considering Tsunami Generation by Horizontal Crustal Displacement"},{"@language":"ja","@value":"地殻変動の水平変位寄与分の考慮方法の違いによる2011年東北地方太平洋沖地震津波の推定波源のすべり量分布の比較"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679124679168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of the 2011 Tohoku Tsunami and introduction of two level tsunamis for tsunami disaster mitigation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679214265728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"沈み込み帯におけるプレート境界面の不均質と地震活動"},{"@language":"en","@value":"Relationship between Heterogeneity of Plate Interface and Seismicity at Subduction Zones: The Japan Trench and Hikurangi Subduction Zones as Examples"},{"@value":"沈み込み帯におけるプレート境界面の不均質と地震活動 : 日本海溝およびヒクランギ沈み込み帯を例として"},{"@language":"ja-Kana","@value":"シズミ コミ タイ ニ オケル プレート キョウカイメン ノ フキンシツ ト ジシン カツドウ : ニホン カイコウ オヨビ ヒクランギ シズミ コミ タイ オ レイ ト シテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679214816896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波遡上高の詳細分布から推定される2011年東北地方太平洋沖地震の断層モデル"},{"@language":"en","@value":"Source Fault Model of the 2011 off the Pacific Coast of Tohoku Earthquake, Estimated from the Detailed Distribution of Tsunami Run-up Heights"},{"@language":"ja-Kana","@value":"ツナミ ソジョウ ダカ ノ ショウサイ ブンプ カラ スイテイ サレル 2011ネン トウホク チホウ タイヘイヨウオキ ジシン ノ ダンソウ モデル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280388992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strong Motion Characteristics of the 2011 Tohoku-Oki Earthquake"},{"@value":"2011年東北地方太平洋沖地震の強震動"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296052992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Basic Study of Tsunami Risk Map based on Extreme Value Analysis"},{"@language":"ja","@value":"極値統計法に基づく極低頻度までを対象とした津波リスクマップの基礎的研究"},{"@language":"ja-Kana","@value":"ゴクチ トウケイホウ ニ モトズク ゴクテイ ヒンド マデ オ タイショウ ト シタ ツナミ リスクマップ ノ キソテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296144384","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami Characteristics in Tokai Coastal Area Due to the 2011 Tohoku Earthquake"},{"@language":"ja","@value":"東北地方太平洋沖地震による東海地方の津波特性"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296165376","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effect of Offshore Tsunami Station Array Configuration on Accuracy of Near-Field Tsunami Forecast"},{"@value":"沖合津波観測点配置の違いが逆解析に基づく近地津波予測の精度に与える影響"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296173568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Amplification Mechanisms of The 2011 Tohoku Tsunami in Ryori Bay"},{"@language":"ja","@value":"東北地方太平洋沖地震津波の綾里湾における増幅機構"},{"@language":"ja-Kana","@value":"トウホク チホウ タイヘイヨウオキ ジシン ツナミ ノ アヤ リワン ニ オケル ゾウフク キコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296411776","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"各種確率論的津波ハザード解析手法の高頻度から極低頻度までの評価能力の比較"},{"@language":"en","@value":"COMPARISON ON CAPACITY OF PROBALISTIC TSUNAMI HAZARD ANALYSIS FROM HIGH FREQUENCY TO LOW FREQUENCY"},{"@language":"ja-Kana","@value":"カクシュ カクリツロンテキ ツナミ ハザード カイセキ シュホウ ノ コウヒンド カラ ゴクテイ ヒンド マデ ノ ヒョウカ ノウリョク ノ ヒカク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680297071360","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波漂流物モデルの現地スケール問題への適用に関する考察"},{"@language":"en","@value":"APPLICABILITY OF OBJECTS DRIFTING MODEL BY TSUNAMI FOR PRACTICAL PROBLEMS"},{"@language":"ja-Kana","@value":"ツナミ ヒョウリュウブツ モデル ノ ゲンチ スケール モンダイ エ ノ テキヨウ ニ カンスル コウサツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680326128128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A STUDY ON CHARACTERISTICS OF TSUNAMI GENERATED BY SPLAY FAULT RUPTURING"},{"@language":"ja","@value":"海溝型地震の分岐断層破壊シナリオで発生する津波の特徴に関する一考察"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680328886272","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"APPLICATION OF NUMERICAL TSUNAMI-FLOOD SIMULATION TO EARLY DETERMINATION FOR SPATIAL DISTRIBUTION OF CHEMICAL POLLUTION IN TSUNAMI DEPOSIT"},{"@value":"津波氾濫解析を応用した津波堆積物の化学物質汚染の空間分布早期推定に関する考察"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680329235328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A STUDY ON INFLUENCES OF NUMERICAL CONDITIONS OF TSUNAMI SIMULATION AND CHARACTERISTICS OF TSUNAMI PROPAGATION OF THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE TSUNAMI IN TOKYO BAY"},{"@language":"ja","@value":"東京湾内における東北津波の伝播特性および計算条件の違いによる計算精度の検討"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680329312768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波襲来時における伊勢湾海域の水塊構造に関する数値的検討"},{"@language":"en","@value":"NUMERICAL EXAMINATION ON WATER STRUCTURE VARIATION IN ISE BAY AREA UNDER TSUNAMI ATTACK"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680331006848","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"TSUNAMI SIMULATION CONSIDERING INTERRELATED EARTHQUAKES AND ITS REMAINING PROBLEM"},{"@language":"ja","@value":"断層領域の連動を考慮した津波解析とその課題"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680334094848","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Characterizing Model for Tsunami Source regarding the Inter-plate Earthquake Tsunami"},{"@language":"ja","@value":"プレート間地震による津波の特性化波源モデルの提案"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680335025152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source Modeling of the 2011 Off the Pacific Coast of Tohoku Earthquake"},{"@language":"ja","@value":"2011 年東北地方太平洋沖地震の震源のモデル化"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680407451776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"EARTHQUAKE SOURCE AND GROUND MOTION CHARACTERISTICS IN EASTERN JAPAN DURING THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217064448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal deformation of northeastern Japan based on geodetic data for recent 120 years"},{"@language":"ja","@value":"測地観測データに基づく東北日本の最近120年間の地殻変動"},{"@language":"ja-Kana","@value":"ソクチ カンソク データ ニ モトズク トウホク ニホン ノ サイキン 120ネンカン ノ チカク ヘンドウ"},{"@value":"Crustal deformation of northeastern Japan based on geodetic data for recent 120 years [in Japanese with English abstract]"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218550016","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Co-seismic displacement of the 2011 Tohoku-oki Earthquake reaching to the trench axis detected by differential bathymetry survey"},{"@language":"ja","@value":"2011年東北地方太平洋沖地震：海底地形データから明らかにされた海底変動"},{"@language":"ja-Kana","@value":"2011ネン トウホク チホウ タイヘイヨウオキ ジシン : カイテイ チケイ データ カラ アキラカ ニ サレタ カイテイ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681463206400","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami arrival time characteristics of the 2011 East Japan Tsunami obtained from eyewitness accounts, evidence and numerical simulation"},{"@value":"Tsunami arrival time characteristics of the 2011 Great East Japan tsunami revealed from eyewitness, evidences and numerical simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763021728256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Total Electron Content Observations by Dense Regional and Worldwide International Networks of GNSS"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763128053120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review on Near-Field Tsunami Forecasting from Offshore Tsunami Data and Onshore GNSS Data for Tsunami Early Warning"}]},{"@id":"https://cir.nii.ac.jp/crid/1390287441188818304","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"TIME-FREQUENCY ANALYSIS AND DECAY PROPERTIES OF TSUNAMIS"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238095098496","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"DEVELOPMENT OF TSUNAMI INUNDATION DATABASE BASED ON POST-EVENT SURVEY RESULTS FOR INUNDATION ANALYSIS"},{"@language":"ja","@value":"痕跡調査結果に基づく津波遡上解析のための遡上高・浸水高データベースの作成"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238103264768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Real-Time Tsunami Inundation Forecast for a Recurrence of 17<sup>th</sup> Century Great Hokkaido Earthquake in Japan"},{"@value":"Real-Time Tsunami Inundation Forecast for a Recurrence of 17th Century Great Hokkaido Earthquake in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390583502303724288","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"BASIC RESEARCH ON TSUNAMI DISASTER ATTENUATION EFFECTIVENESS OF LOCAL INFRASTRUCTURE IN OARAI TOWN, IBARAKI PREFECTURE IN JAPAN"},{"@language":"ja","@value":"茨城県大洗町における地域インフラの津波減衰効果に関する基礎的研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1390587528328701440","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"COMPARATIVE ANALYSIS OF DYNAMIC RUPTURE AND STATIC FAULT MODELS FOR TSUNAMI PREDICTION USING T-STOC"}]},{"@id":"https://cir.nii.ac.jp/crid/1390587675161654272","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波減災効果と意識調査に基づく大洗町旧堤防の保全価値"},{"@language":"en","@value":"CONSERVATION VALUE OF OARAI TOWN'S OLD SEAWALLS BASED ON TSUNAMI REDUCTION EFFECTIVENESS ANALYSIS AND AWARENESS SURVEYS"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713014917248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Damage Assessment of Road Bridges Subjected to the 2011 Tohoku Pacific Earthquake Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713079952000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent Issues Affecting Forecast of Subduction Zone Great Earthquakes in Japan Through Paleoseismological Study"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713080982400","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow Slip Transients Before the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1391130851448222080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A BASIC STUDY ON INTEGRATED RISK ASSESSMENT ON TSUNAMI AND STORM SURGE"},{"@language":"ja","@value":"茨城県沿岸における津波と高潮の統合リスク評価の基礎的検討"},{"@language":"ja-Kana","@value":"イバラキケン エンガン ニ オケル ツナミ ト タカシオ ノ トウゴウ リスク ヒョウカ ノ キソテキ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1522825130298098944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ionospheric disturbances detected by GPS total electron content observation after the 2011 off the Pacific coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1523388080358623360","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Along-trench structural variation and seismic coupling in the northern Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942184946048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A scenario for the generation process of the 2011 Tohoku earthquake based on dynamic rupture simulation : role of stress concentration and thermal fluid pressurization"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892138327040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical simulations of atmospheric waves excited by the 2011 off the Pacific coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367116815744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Friction properties of the plate boundary megathrust beneath the frontal wedge near the Japan Trench : an inference from topographic variation"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317068451072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coupling coefficient, hierarchical structure, and earthquake cycle for the source area of the 2011 off the Pacific coast of Tohoku earthquake inferred from small repeating earthquake data"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317070233344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Outer-rise normal fault development and influence on near-trench décollement propagation along the Japan Trench, off Tohoku"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266977822464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frequency-dependent amplification of the Sanriku tsunamis in Ryori Bay"}]}],"dataSourceIdentifier":[{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R100000039-I9102971"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.06.010"},{"@type":"CIA","@value":"20001073492"},{"@type":"KAKEN","@value":"PRODUCT-12620251"},{"@type":"OPENAIRE","@value":"doi_dedup___::1ded5c7330bced08c87ebf0a2f10ac48"},{"@type":"CROSSREF","@value":"10.1002/2013jb010841_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2017gl076031_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-014-0779-x_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-014-0948-y_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011gl049136_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011gl049308_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011gl050098_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1038/nature13778_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1093/gji/ggt320_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1126/science.1243485_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1126/science.1243719_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0281_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.05.028_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.05.003_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2016gl068283_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/1345_2015_48_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-017-1760-2_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2017jc013626_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2018ja025289_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1130/g35948.1_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1130/ges01630.1_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1144/sp456.12_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2204/iodp.pr.343343t.2012_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.05.016_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.76.2_i_1243_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2018jb017135_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.04.002_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejseee.70.i_210_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.i_436_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.i_186_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejoe.68.i_168_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-060313-054614_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0023_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.72.i_427_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5610/jaee.17.2_1_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-135_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0040_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1785/0220200115_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-071719-055216_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5610/jaee.22.5_25_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00556-0_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejj.25-17096_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02122-4_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2016jb013485_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011gl050686_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2012jb009186_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1038/ngeo1547_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1126/science.1229379_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1142/s0578563412500015_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0339_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.07.006_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2014tc003695_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2017jb014839_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2017jb015070_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/jgrb.50225_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s10872-015-0293-5_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40562-014-0015-7_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40562-017-0100-9_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0153-3_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0278-x_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.4294/zisin.64.169_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1108-5_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.68.i_211_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.09.007_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/journalofjsce.1.1_329_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.i_831_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.i_1351_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.70.i_156_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.06.037_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5610/jaee.13.2_2_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.09.015_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2183/pjab.91.262_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.73.i_1495_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2017.p0079_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2020gl088395_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejhe.74.i_451_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-021-02910-z_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.egg.2022.100114_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1103/physrevresearch.4.013211_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1109/access.2019.2917070_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.ijdrr.2022.102954_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011gl049146_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2012gl052220_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1038/srep05631_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1144/sp456.9_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0272_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0330_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0358_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.06.035_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.07.015_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2015gl063140_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2016gl071784_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-017-1590-2_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1093/gji/ggt256_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1130/ges01489.1_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40562-017-0099-y_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2018.p0535_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.3390/geosciences8010003_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00367-020-00636-w_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.12.038_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1038/s41467-020-14745-8_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.04.047_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejseee.69.i_750_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.i_171_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2013.08.052_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.01.026_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.4294/zisin.2016-18_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2020.103498_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2020ea001359_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejj.24-17069_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2023gl104271_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/journalofjsce.25-18159_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2024jb028750_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2025.107344_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2014gl062604_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011jb008750_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0311_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2015jb012764_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/2017gl074528_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1002/grl.50364_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/978-3-319-00972-8_4_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-018-02089-w_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2011gl048902_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2328/jnds.34.91_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.08.042_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2012.08.012_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1128-1_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/journalofjsce.9.1_113_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2018.10.007_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.i_181_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejoe.69.i_437_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejhe.68.i_1519_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0052_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5610/jaee.14.5_1_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.74.i_433_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5610/jaee.15.3_114_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/s00024-021-02727-w_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1126/science.abe1169_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1080/21664250.2021.2005364_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-16578-5_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1029/2022jc018480_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00575-x_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1111/iar.70009_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.69.23_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1007/978-981-15-0291-0_184_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.09.009_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.08.018_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejoe.71.i_377_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejoe.72.i_139_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.ocemod.2017.01.002_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2014.01.002_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.177_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.ijggc.2019.01.002_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2015.10.009_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-071719-054845_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.11.007_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5026/jgeography.126.207_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2014.01.001_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0027_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.5610/jaee.13.2_75_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.jlp.2018.02.009_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/kaigan.71.i_163_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.2208/jscejhe.72.i_415_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.04.009_references_DOI_NbsyLYMmEvpQL9XyzMr0o5IIJM9"}]}