{"@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/1362825895144485504.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1103961"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1103961"}},{"identifier":{"@type":"PMID","@value":"15498971"}},{"identifier":{"@type":"NAID","@value":"80017060468"}}],"dc:title":[{"@value":"Earth Tides Can Trigger Shallow Thrust Fault Earthquakes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We show a correlation between the occurrence of shallow thrust earthquakes and the occurrence of the strongest tides. The rate of earthquakes varies from the background rate by a factor of 3 with the tidal stress. The highest correlation is found when we assume a coefficient of friction of μ = 0.4 for the crust, although we see good correlation for μ between 0.2 and 0.6. Our results quantify the effect of applied stress on earthquake triggering, a key factor in understanding earthquake nucleation and cascades whereby one earthquake triggers others.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895144485506","@type":"Researcher","foaf:name":[{"@value":"Elizabeth S. Cochran"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095, USA."},{"@value":"Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Miyagi 980-8578, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895144485505","@type":"Researcher","foaf:name":[{"@value":"John E. Vidale"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095, USA."},{"@value":"Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Miyagi 980-8578, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895144485504","@type":"Researcher","foaf:name":[{"@value":"Sachiko Tanaka"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095, USA."},{"@value":"Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Miyagi 980-8578, Japan."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2004-11-12","prism:volume":"306","prism:number":"5699","prism:startingPage":"1164","prism:endingPage":"1166"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1103961"}],"createdAt":"2004-10-22","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050302172855284096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seasonal Modulation of Crustal Seismicity in Northeastern Japan Driven by Snow Load"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760746395392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic fatigue failure may have triggered the 2014 M  w  7.9 Rat Islands earthquake"},{"@value":"Seismic fatigue failure may have triggered the 2014 <i>M</i><sub><i>w</i></sub>7.9 Rat Islands 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