{"@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/1363951793683085696.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1190/geo2011-0086.1"}},{"identifier":{"@type":"URI","@value":"https://pubs.geoscienceworld.org/seg/geophysics/article-pdf/76/6/N47/3227445/geo2011-0086.pdf"}}],"dc:title":[{"@value":"Krauklis wave in a stack of alternating fluid-elastic layers"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>ABSTRACT</jats:title>\n                  <jats:p>The Krauklis wave is a slow dispersive wave mode that propagates in a fluid layer bounded by elastic media. In a model of alternating fluid and elastic layers, two interface waves can exist at low frequencies: The first wave propagates mostly in the elastic layer and has little dispersion, while the second wave can have strong dispersion and propagates as a Krauklis wave for some parameter combinations. Analytical conditions predict appearance of the Krauklis wave for higher frequencies and low porosities. Interface-wave velocities depend on model porosity, which potentially can be used for fracture mapping.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383951793683085696","@type":"Researcher","foaf:name":[{"@value":"Valeri A. Korneev"}],"jpcoar:affiliationName":[{"@value":"Lawrence Berkeley National Laboratory 1 , Berkeley, California, . E-mail: vakorneev@lbl.gov ."}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"19422156"},{"@type":"PISSN","@value":"00168033"}],"prism:publicationName":[{"@value":"Geophysics"}],"dc:publisher":[{"@value":"Society of Exploration Geophysicists"}],"prism:publicationDate":"2011-11-01","prism:volume":"76","prism:number":"6","prism:startingPage":"N47","prism:endingPage":"N53"},"reviewed":"false","url":[{"@id":"https://pubs.geoscienceworld.org/seg/geophysics/article-pdf/76/6/N47/3227445/geo2011-0086.pdf"}],"createdAt":"2011-12-22","modifiedAt":"2025-12-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/2050870367116787072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Linear stability of plane Poiseuille flow in an infinite elastic medium and volcanic tremors"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1190/geo2011-0086.1"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-19_references_DOI_ZWYQDLSBmku7QO3mKEW4sKo6zLV"}]}