{"@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/1363388844667273600.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2013gl058607"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058607"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013GL058607"}}],"dc:title":[{"@value":"Slip rate and tremor genesis in Cascadia"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>At many plate boundaries, conditions in the transition zone between seismogenic and stable slip produce slow earthquakes. In the Cascadia subduction zone, these events are consistently observed as slow, aseismic slip on the plate interface accompanied by persistent tectonic tremor. However, not all slow slip at other plate boundaries coincides spatially and temporally with tremor, leaving the physics of tremor genesis poorly understood. Here we analyze seismic, geodetic, and strainmeter data in Cascadia to observe for the first time a large, tremor‐generating slow earthquake change from tremor‐genic to silent and back again. The tremor falls silent at reduced slip speeds when the migrating slip front pauses as it loads the stronger adjacent fault segment to failure. The finding suggests that rheology and slip‐speed‐regulated stressing rate control tremor genesis, and the same section of fault can slip both with and without detectable tremor, limiting tremor's use as a proxy for slip.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844667273600","@type":"Researcher","foaf:name":[{"@value":"Aaron G. Wech"}],"jpcoar:affiliationName":[{"@value":"Volcano Science Center U.S. Geological Survey  Anchorage Alaska USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844667273601","@type":"Researcher","foaf:name":[{"@value":"Noel M. Bartlow"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California, San Diego  La Jolla California USA"}]}],"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":"2014-01-28","prism:volume":"41","prism:number":"2","prism:startingPage":"392","prism:endingPage":"398"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058607"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013GL058607"}],"createdAt":"2014-01-13","modifiedAt":"2023-09-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339107234432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connecting slow earthquakes to huge earthquakes"},{"@value":"Connecting slow earthquakes to large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050011340342223872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake Source"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282677887377024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Evolution of Recurrent Slow Slip Events Along the Southern Ryukyu Subduction Zone, Japan, From 2010 to 2013"}]},{"@id":"https://cir.nii.ac.jp/crid/1050298355878422912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Systematic Detection of Short‐Term Slow Slip Events in Southcentral Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1050852901090021632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frictional Strengths of Subduction Thrust Rocks in the Region of Shallow Slow Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050855656203614464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of a detection method for short-term slow slip events using GNSS data and its application to the Nankai subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348947712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Universality of slow earthquakes in the very low frequency band"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229807854720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tidal Response in Shallow Tectonic Tremors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168843679616","@type":"Article","resourceType":"学術雑誌論文(journal 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302866834991616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of Slow Slip Events Explained by Rate‐Strengthening Faults Subject to Periodic Pore Fluid Pressure Changes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755443072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Imaging of the early acceleration phase of the 2013–2014 Boso slow slip event"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755954304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial distribution of seismic energy rate of tectonic tremors in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641753424128","@type":"Article","resourceType":"学術雑誌論文(journal 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