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dc.contributor.author
Picotti, Stefano  
dc.contributor.author
Carcione, José Carlos  
dc.contributor.author
Santos, Juan Enrique  
dc.contributor.author
Gei, Davide  
dc.date.available
2020-04-21T16:23:27Z  
dc.date.issued
2010-03  
dc.identifier.citation
Picotti, Stefano; Carcione, José Carlos; Santos, Juan Enrique; Gei, Davide; Q -anisotropy in finely-layered media; American Geophysical Union; Geophysical Research Letters; 37; 6; 3-2010; 1-13  
dc.identifier.issn
0096-3941  
dc.identifier.uri
http://hdl.handle.net/11336/103176  
dc.description.abstract
Finely-layered media behaves as a transversely isotropic medium at long wavelengths. If the constituent media are anelastic, Q-anisotropy is described by Postma averaging for two periodic layers and by Backus averaging for an stationary sequence of many layers. In order to test the theory, we perform numerical simulations of wave propagation in a periodic sequence of sandstone and limestone and compute the Q-factor of qP waves as a function of the propagation direction.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
American Geophysical Union  
dc.relation
Corrección de este artículo en https://doi.org/10.1029/2011GL047613  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
anisotropy  
dc.subject
finite element  
dc.subject
finely-layered  
dc.subject
attenuation  
dc.subject.classification
Geoquímica y Geofísica  
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente  
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS  
dc.title
Q -anisotropy in finely-layered media  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2020-03-04T17:34:27Z  
dc.identifier.eissn
0094-8276  
dc.journal.volume
37  
dc.journal.number
6  
dc.journal.pagination
1-13  
dc.journal.pais
Estados Unidos  
dc.journal.ciudad
Washington DC  
dc.description.fil
Fil: Picotti, Stefano. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia  
dc.description.fil
Fil: Carcione, José Carlos. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia  
dc.description.fil
Fil: Santos, Juan Enrique. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física. Grupo de Geofísica Aplicada; Argentina. Purdue University; Estados Unidos  
dc.description.fil
Fil: Gei, Davide. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia  
dc.journal.title
Geophysical Research Letters  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2009GL042046  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1029/2009GL042046  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.semanticscholar.org/paper/Q%E2%80%90anisotropy-in-finely%E2%80%90layered-media-Picotti-Carcione/0af642d94c5b7a01c26e4eee17a9b3e45c2ccf19  

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