{"@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/1363388846259871616.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018gl077579"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL077579"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL077579"}}],"dc:title":[{"@value":"Fast and Slow Slip Events Emerge Due to Fault Geometrical Complexity"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Active faults release elastic strain energy via a whole continuum of modes of slip, ranging from devastating earthquakes to slow slip events (SSEs) and persistent creep. Understanding the mechanisms controlling the occurrence of rapid, dynamic slip radiating seismic waves (i.e., earthquakes) or slow, silent slip (i.e., SSEs) is a fundamental point in the estimation of seismic hazard along subduction zones. Using the numerical implementation of a simple rate‐weakening fault model, we show that the simplest of fault geometrical complexities with uniform rate‐weakening friction properties give rise to both SSEs and fast earthquakes without appealing to complex rheologies or mechanisms. We argue that the spontaneous occurrence, the characteristics and the scaling relationship of SSEs and earthquakes emerge from geometrical complexities. The geometry of active faults should be considered as a complementary mechanism to current numerical models of SSEs and fast earthquakes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388846259871617","@type":"Researcher","foaf:name":[{"@value":"Pierre Romanet"}],"jpcoar:affiliationName":[{"@value":"Institut de Physique du Globe de Paris, CNRS‐UMR 7154 Sorbonne Paris Cité  Paris France"},{"@value":"Laboratoire de Géologie, École Normale Supérieure, CNRS‐UMR 8538 PSL Research University  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846259871618","@type":"Researcher","foaf:name":[{"@value":"Harsha S. Bhat"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géologie, École Normale Supérieure, CNRS‐UMR 8538 PSL Research University  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846259871616","@type":"Researcher","foaf:name":[{"@value":"Romain Jolivet"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géologie, École Normale Supérieure, CNRS‐UMR 8538 PSL Research University  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846259871619","@type":"Researcher","foaf:name":[{"@value":"Raúl Madariaga"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géologie, École Normale Supérieure, CNRS‐UMR 8538 PSL Research University  Paris France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2018-05-28","prism:volume":"45","prism:number":"10","prism:startingPage":"4809","prism:endingPage":"4819"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL077579"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL077579"}],"createdAt":"2018-05-08","modifiedAt":"2023-09-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001201681542144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Elastic interaction of parallel rate-and-state-dependent frictional faults with aging and slip laws: slow-slip faults can sometimes host fast events"}]},{"@id":"https://cir.nii.ac.jp/crid/1050003824911645696","@type":"Article","resourceType":"学術雑誌論文(journal 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