{"@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/1363388846180031744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005gl025472"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL025472"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL025472"}}],"dc:title":[{"@value":"Strong shaking in Los Angeles expected from southern San Andreas earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The southernmost San Andreas fault has a high probability of rupturing in a large (greater than magnitude 7.5) earthquake sometime during the next few decades. New simulations show that the chain of sedimentary basins between San Bernardino and downtown Los Angeles form an effective waveguide that channels Love waves along the southern edge of the San Bernardino and San Gabriel Mountains. Earthquake scenarios with northward rupture, in which the guided wave is efficiently excited, produce unusually high long‐period ground motions over much of the greater Los Angeles region, including intense, localized amplitude modulations arising from variations in waveguide cross‐section.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380290617850296962","@type":"Researcher","foaf:name":[{"@value":"K. B. Olsen"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences San Diego State University  San Diego California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031744","@type":"Researcher","foaf:name":[{"@value":"S. M. Day"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences San Diego State University  San Diego California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031751","@type":"Researcher","foaf:name":[{"@value":"J. B. Minster"}],"jpcoar:affiliationName":[{"@value":"Scripps Institution of Oceanography University of California, San Diego  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031749","@type":"Researcher","foaf:name":[{"@value":"Y. Cui"}],"jpcoar:affiliationName":[{"@value":"San Diego Supercomputer Center University of California, San Diego  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031745","@type":"Researcher","foaf:name":[{"@value":"A. Chourasia"}],"jpcoar:affiliationName":[{"@value":"San Diego Supercomputer Center University of California, San Diego  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031752","@type":"Researcher","foaf:name":[{"@value":"M. Faerman"}],"jpcoar:affiliationName":[{"@value":"San Diego Supercomputer Center University of California, San Diego  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031750","@type":"Researcher","foaf:name":[{"@value":"R. Moore"}],"jpcoar:affiliationName":[{"@value":"San Diego Supercomputer Center University of California, San Diego  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031747","@type":"Researcher","foaf:name":[{"@value":"P. Maechling"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences University of Southern California  Los Angeles California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846180031748","@type":"Researcher","foaf:name":[{"@value":"T. Jordan"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences University of Southern California  Los Angeles 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":"2006-04","prism:volume":"33","prism:number":"7","prism:startingPage":"L07305"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL025472"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL025472"}],"createdAt":"2006-04-04","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567179757215104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long‐period ground motion simulation of a subduction earthquake using the offshore‐onshore ambient seismic field"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654738589952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic wavefield imaging of long‐period ground motion in the Tokyo metropolitan area, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942148523904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long-period ground motion simulation using centroid moment tensor inversion solutions based on the regional three-dimensional model in the Kanto region, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005gl025472"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01348-2_references_DOI_a2IrieaqEagUhAJOUXj0wQlJNB2"},{"@type":"CROSSREF","@value":"10.1002/2015gl064265_references_DOI_a2IrieaqEagUhAJOUXj0wQlJNB2"},{"@type":"CROSSREF","@value":"10.1002/2017jb014276_references_DOI_a2IrieaqEagUhAJOUXj0wQlJNB2"}]}