{"@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/1362825893362465152.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature11703"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature11703.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature11703"}},{"identifier":{"@type":"PMID","@value":"23302798"}}],"dc:title":[{"@value":"Stable creeping fault segments can become destructive as a result of dynamic weakening"}],"description":[{"notation":[{"@value":"Faults in Earth's crust accommodate slow relative motion between tectonic plates through either similarly slow slip or fast, seismic-wave-producing rupture events perceived as earthquakes. These types of behaviour are often assumed to be separated in space and to occur on two different types of fault segment: one with stable, rate-strengthening friction and the other with rate-weakening friction that leads to stick-slip. The 2011 Tohoku-Oki earthquake with moment magnitude M(w) = 9.0 challenged such assumptions by accumulating its largest seismic slip in the area that had been assumed to be creeping. Here we propose a model in which stable, rate-strengthening behaviour at low slip rates is combined with coseismic weakening due to rapid shear heating of pore fluids, allowing unstable slip to occur in segments that can creep between events. The model parameters are based on laboratory measurements on samples from the fault of the M(w) 7.6 1999 Chi-Chi earthquake. The long-term slip behaviour of the model, which we examine using a unique numerical approach that includes all wave effects, reproduces and explains a number of both long-term and coseismic observations-some of them seemingly contradictory-about the faults at which the Tohoku-Oki and Chi-Chi earthquakes occurred, including there being more high-frequency radiation from areas of lower slip, the largest seismic slip in the Tohoku-Oki earthquake having occurred in a potentially creeping segment, the overall pattern of previous events in the area and the complexity of the Tohoku-Oki rupture. The implication that earthquake rupture may break through large portions of creeping segments, which are at present considered to be barriers, requires a re-evaluation of seismic hazard in many areas."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326210845568","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50619640"},{"@type":"NRID","@value":"1000050619640"},{"@type":"ORCID","@value":"0000-0001-7201-2578"},{"@type":"NRID","@value":"9000254572406"},{"@type":"NRID","@value":"9000016991593"},{"@type":"NRID","@value":"9000000288170"},{"@type":"NRID","@value":"9000000287900"},{"@type":"NRID","@value":"9000292881275"},{"@type":"NRID","@value":"9000257810390"},{"@type":"NRID","@value":"9000257811310"},{"@type":"NRID","@value":"9000255316051"},{"@type":"NRID","@value":"9000283715704"},{"@type":"NRID","@value":"9000258705245"},{"@type":"NRID","@value":"9000256009019"},{"@type":"NRID","@value":"9000257809139"},{"@type":"NRID","@value":"9000241779305"},{"@type":"NRID","@value":"9000392721179"},{"@type":"NRID","@value":"9000020014212"},{"@type":"NRID","@value":"9000350559922"},{"@type":"NRID","@value":"9000411514091"},{"@type":"NRID","@value":"9000256017897"},{"@type":"NRID","@value":"9000256009782"},{"@type":"NRID","@value":"9000257810350"},{"@type":"NRID","@value":"9000000286867"},{"@type":"NRID","@value":"9000000125510"},{"@type":"NRID","@value":"9000254573015"},{"@type":"NRID","@value":"9000252986244"},{"@type":"NRID","@value":"9000003940010"},{"@type":"NRID","@value":"9000297484596"},{"@type":"NRID","@value":"9000403426916"},{"@type":"NRID","@value":"9000258701346"},{"@type":"NRID","@value":"9000006033416"},{"@type":"NRID","@value":"9000022038751"},{"@type":"NRID","@value":"9000286626084"},{"@type":"NRID","@value":"9000401633310"},{"@type":"NRID","@value":"9000255699347"},{"@type":"NRID","@value":"9000254575368"},{"@type":"NRID","@value":"9000254142128"},{"@type":"NRID","@value":"9000410320295"},{"@type":"NRID","@value":"9000256018575"},{"@type":"NRID","@value":"9000017180686"},{"@type":"NRID","@value":"9000411517725"},{"@type":"NRID","@value":"9000347083440"},{"@type":"NRID","@value":"9000254141670"},{"@type":"NRID","@value":"9000254141657"},{"@type":"NRID","@value":"9000256010018"},{"@type":"NRID","@value":"9000009562294"},{"@type":"NRID","@value":"9000399495905"},{"@type":"NRID","@value":"9000256023071"},{"@type":"NRID","@value":"9000257809206"},{"@type":"NRID","@value":"9000346936622"},{"@type":"NRID","@value":"9000409996516"},{"@type":"NRID","@value":"9000283343638"},{"@type":"NRID","@value":"9000283649665"},{"@type":"NRID","@value":"9000257708280"},{"@type":"NRID","@value":"9000254142194"},{"@type":"NRID","@value":"9000254141837"},{"@type":"NRID","@value":"9000001380132"},{"@type":"NRID","@value":"9000254141679"},{"@type":"NRID","@value":"9000403164061"},{"@type":"NRID","@value":"9000257830333"},{"@type":"NRID","@value":"9000009562083"},{"@type":"NRID","@value":"9000003813039"},{"@type":"NRID","@value":"9000254142077"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000015400"}],"foaf:name":[{"@value":"Hiroyuki Noda"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893362465152","@type":"Researcher","foaf:name":[{"@value":"Nadia Lapusta"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2013-01","prism:volume":"493","prism:number":"7433","prism:startingPage":"518","prism:endingPage":"521"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/nature11703.pdf"},{"@id":"http://www.nature.com/articles/nature11703"}],"createdAt":"2013-01-08","modifiedAt":"2023-05-18","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335764454144","@type":"Article","resourceType":"学術雑誌論文(journal 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Temporal Decrease of the Gutenberg-Richter b-Value Prior to a Large Earthquake"},{"@value":"Physical Mechanism for a Temporal Decrease of the Gutenberg‐Richter <i>b</i>‐Value Prior to a Large Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022457828784768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Implementation into earthquake sequence simulations of a rate- and state-dependent friction law incorporating pressure solution creep"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810792973312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku-Oki earthquake"},{"@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku‐Oki 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megathrust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617865614848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Presence of interplate channel layer controls of slip during and after the 2011 Tohoku-Oki earthquake through the frictional characteristics"}]},{"@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/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/1360567179755836928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquake model experiments in a viscoelastic fluid: A scaling of decreasing magnitudes of earthquakes with depth"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755972352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic imaging of potential seismogenic asperities on the Xianshuihe‐Anninghe‐Zemuhe fault system, southwest China, with a new 3‐D viscoelastic interseismic coupling model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181097114880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Apparent Dependence of Rate- and State-Dependent Friction Parameters on Loading Velocity and Cumulative Displacement Inferred from Large-Scale Biaxial Friction Experiments"}]},{"@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/1360584339757796352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Incoming plate structure at the Japan Trench subduction zone revealed in densely spaced reflection seismic profiles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379360806272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Relationships between fault friction, slip time, and physical parameters explored by experiment-based friction model: A machine learning approach using recurrent neural networks (RNNs)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639280836480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Active thrusting of the Longquan Fault in the central Sichuan basin, China, and the seismotectonic behavior in the Longmen Shan fold‐and‐thrust belt"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846352384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Episodic deformation and inferred slow slip at the Nankai subduction zone during the first decade of CORK borehole pressure and VLFE monitoring"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641732891008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large fault slip peaking at trench in the 2011 Tohoku-oki earthquake"}]},{"@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/1360848657453482368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contrasting hydrological and mechanical properties of clayey and silty muds cored from the shallow Nankai Trough accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453491072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structures and high-velocity frictional properties of the Pingxi fault zone in the Longmenshan fault system, Sichuan, China, activated during the 2008 Wenchuan earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567354121216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Relationship Between Seismic and Aseismic Slip on the Philippine Fault on Leyte Island: Bayesian Modeling of Fault Slip and Geothermal Subsidence"}]},{"@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/1360869854370617472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Community‐Driven Code Comparisons for Simulations of Fluid‐Induced Aseismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131416055518976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structural records and mechanical characteristics of seismic slip along an active fault crosscutting unconsolidated Quaternary sediments: Suryum fault, SE Korea"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412896196728192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The State of Stress on the Fault Before, During, and After a Major Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390004222631008640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamic Earthquake Cycle Simulations Considering Changes in Dominant Deformation Mechanisms of a Fault Slip"},{"@language":"ja","@value":"断層滑りの支配的な変形機構の遷移を考慮に入れた動的地震サイクルシミュレーション"},{"@language":"ja-Kana","@value":"ダンソウ スベリ ノ シハイテキ ナ ヘンケイ キコウ ノ センイ オ コウリョ ニ イレタ ドウテキ ジシン サイクルシミュレーション"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238108729600","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Probing Earthquake Physics Using Multidisciplinary Approaches"},{"@language":"ja","@value":"分野横断的なアプローチを用いた地震の物理の研究"},{"@language":"ja-Kana","@value":"ブンヤ オウダンテキ ナ アプローチ オ モチイタ ジシン ノ ブツリ ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942151020672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional stability of porous tuff breccia under subsurface pressure conditions and implications for shallow seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367116798080","@type":"Article","resourceType":"学術雑誌論文(journal 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