{"@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/1362544420791062016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2008jb005749"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2008JB005749"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2008JB005749"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2008JB005749"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008JB005749"}}],"dc:title":[{"@value":"Scaling of small repeating earthquakes explained by interaction of seismic and aseismic slip in a rate and state fault model"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Because of short recurrence times and known locations, small repeating earthquakes present a rare predictable opportunity for detailed field observations. They are used to study fault creeping velocities, earthquake nucleation, stress drops, and other aspects of tectonophysics, earthquake mechanics, and seismology. An intriguing observation about repeating earthquakes is their scaling of recurrence time with seismic moment, which is significantly different from the scaling based on a simple conceptual model of circular ruptures with stress drop independent of seismic moment and no aseismic slip. Here we show that a model of repeating earthquakes based on laboratory‐derived rate and state friction laws reproduces the observed scaling. In the model, a small fault patch governed by steady state velocity‐weakening friction is surrounded by a much larger velocity‐strengthening region. Long‐term slip behavior of the fault is simulated using a methodology that fully accounts for both aseismic slip and inertial effects of occasional seismic events. The model results in repeating earthquakes with typical stress drops and sizes comparable with observations. For a fixed set of friction parameters, the observed scaling is reproduced by varying the size of the velocity‐weakening patch. In simulations, a significant part of slip on the velocity‐weakening patches is accumulated aseismically, even though the patches also produce seismic events. The proposed model supplies a laboratory‐based framework for interpreting the wealth of observations about repeating earthquakes, provides indirect evidence that rate and state friction acts on natural faults, and has important implications for possible scenarios of slip partition into seismic and aseismic parts.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382544420791062016","@type":"Researcher","foaf:name":[{"@value":"Ting Chen"}],"jpcoar:affiliationName":[{"@value":"Seismological Laboratory California Institute of Technology  Pasadena California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420791062017","@type":"Researcher","foaf:name":[{"@value":"Nadia Lapusta"}],"jpcoar:affiliationName":[{"@value":"Division of Engineering and Applied Science and Seismological Laboratory California Institute of Technology  Pasadena California USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2009-01","prism:volume":"114","prism:number":"B1","prism:startingPage":"B01311"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2008JB005749"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2008JB005749"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2008JB005749"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008JB005749"}],"createdAt":"2009-01-23","modifiedAt":"2023-08-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050003824911645696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface creep rate distribution along the Philippine fault, Leyte Island, and possible repeating of Mw ~ 6.5 earthquakes on an isolated locked patch"}]},{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review on slow earthquakes in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1050303932805506432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fully dynamic earthquake sequence simulation of a fault in a viscoelastic medium using a spectral boundary integral equation method: does interseismic stress relaxation promote aseismic transients?"}]},{"@id":"https://cir.nii.ac.jp/crid/1050574181243945728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamic earthquake sequence simulation with a SBIEM without periodic boundaries"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214349012992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Under what circumstances does a seismogenic patch produce aseismic transients in the later interseismic period?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168816786816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical simulation of mixed aseismic/seismic fault-slip induced by fluid injection using coupled X-FEM analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689325704960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multiple slow‐slip events during a foreshock sequence of the 2014 Iquique, Chile <i>M<sub>w</sub></i> 8.1 earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691685765888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fixed recurrence and slip models better predict earthquake behavior than the time‐ and slip‐predictable models: 1. Repeating earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643699968256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depth variation of seismic moment and recurrence interval in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757339136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long‐term acceleration of aseismic slip preceding the <b><i>M</i><sub><i>w</i></sub></b> 9 Tohoku‐oki earthquake: Constraints from repeating earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183244461952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical Simulations of Earthquake Triggering by Dynamic and Static Stress Changes Based on a Revised Friction 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Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643368612224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Propagation of Slow Slip Leading Up to the 2011\n            <i>M</i>\n            <sub>w</sub>\n            9.0 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654734613760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Unexpectedly frequent occurrence of very small repeating earthquakes (−5.1 ≤ <i>M<sub>w</sub></i> ≤ −3.6) in a South African gold mine: Implications for monitoring intraplate faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065441664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pre- and postseismic slow slip surrounding the 2011 Tohoku-oki earthquake 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