{"@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/1360574096282955008.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gl069967"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL069967"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL069967"}}],"dc:title":[{"@value":"Reconsidering earthquake scaling"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The relationship (scaling) between scalar moment, <jats:italic>M</jats:italic><jats:sub>0</jats:sub>, and duration, <jats:italic>T</jats:italic>, potentially provides key constraints on the physics governing fault slip. The prevailing interpretation of <jats:italic>M</jats:italic><jats:sub>0</jats:sub>‐<jats:italic>T</jats:italic> observations proposes different scaling for fast (earthquakes) and slow (mostly aseismic) slip populations and thus fundamentally different driving mechanisms. We show that a single model of slip events within bounded slip zones may explain nearly all fast and slow slip <jats:italic>M</jats:italic><jats:sub>0</jats:sub>‐<jats:italic>T</jats:italic> observations, and both slip populations have a change in scaling, where the slip area growth changes from 2‐D when too small to sense the boundaries to 1‐D when large enough to be bounded. We present new fast and slow slip <jats:italic>M</jats:italic><jats:sub>0</jats:sub>‐<jats:italic>T</jats:italic> observations that sample the change in scaling in each population, which are consistent with our interpretation. We suggest that a continuous but bimodal distribution of slip modes exists and <jats:italic>M</jats:italic><jats:sub>0</jats:sub>‐<jats:italic>T</jats:italic> observations alone may not imply a fundamental difference between fast and slow slip.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380013168718641048","@type":"Researcher","foaf:name":[{"@value":"J. Gomberg"}],"jpcoar:affiliationName":[{"@value":"U.S. Geological Survey University of Washington  Seattle Washington USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096282955011","@type":"Researcher","foaf:name":[{"@value":"A. Wech"}],"jpcoar:affiliationName":[{"@value":"U.S. Geological Survey  Anchorage Alaska USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096282955008","@type":"Researcher","foaf:name":[{"@value":"K. Creager"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Sciences University of Washington  Seattle Washington USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096282955010","@type":"Researcher","foaf:name":[{"@value":"K. Obara"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096282955012","@type":"Researcher","foaf:name":[{"@value":"D. Agnew"}],"jpcoar:affiliationName":[{"@value":"IGPP 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":"2016-06-28","prism:volume":"43","prism:number":"12","prism:startingPage":"6243","prism:endingPage":"6251"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GL069967"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL069967"}],"createdAt":"2016-06-15","modifiedAt":"2025-05-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal 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