Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/140935
COMPARTIR / EXPORTAR:
logo share SHARE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Invitar a revisión por pares abierta
Campo DC Valor Lengua/Idioma
dc.contributor.authorGómez de la Peña, L.-
dc.contributor.authorRanero, César R.-
dc.contributor.authorGràcia, Eulàlia-
dc.contributor.authorBartolomé, Rafael-
dc.date.accessioned2016-11-29T13:05:02Z-
dc.date.available2016-11-29T13:05:02Z-
dc.date.issued2015-04-13-
dc.identifierissn: 1607-7962-
dc.identifier.citationGeophysical Research Abstracts 17: EGU2015-14076 (2015)-
dc.identifier.urihttp://hdl.handle.net/10261/140935-
dc.descriptionEuropean Geosciences Union General Assembly 2015 (EGU2015), 12-17 April 2015, Vienna, Austria.-- 1 page-
dc.description.abstractThe Alboran Basin (Western Mediterranean) is located between the Iberian Peninsula and Africa. Along this basin runs the diffuse plate boundary between Iberia and Africa. In order to improve the knowledge of the lithospheric structure in this region, the TOPOMED-GASSIS cruise took place during October 2011 on board the RV Sarmiento de Gamboa. During this cruise, the new deep multichannel seismic acquisition system was used for the first time. The equipment used were two high volume G-gun arrays (2000 psi / 2500 psi) and up to 6 km long Sercel multichannel digital streamer (408 / 480 active channels) towed behind the vessel. The results correspond to a series of multichannel seismic profiles with unprecedented quality, which allows us to apply state of the art processing and imaging techniques to obtain the deep tectonic structure of the plate boundary while keeping a good resolution in the sedimentary infill of the basin. A complete processing sequence has been used in order to increase the signal to noise ratio, including deconvolution, multiple attenuation and time migration. A high-quality deep penetration dataset has been acquired using the new instrumentation allowing to image the whole basin at a crustal scale. The results are high-quality sections for interpretation through frequency preservation, effective multiple attenuation and velocity analysis. Moreover, we will carry out Pre-Stack Depth Migration algorithms to selected profiles, in order to obtain the real geometry of the structures at depth-
dc.publisherEuropean Geosciences Union-
dc.relation.isversionofPublisher's version-
dc.rightsopenAccess-
dc.titleNew deep multichannel seismic reflection images from the Alboran Basin: The TOPOMED-GASSIS dataset-
dc.typepóster de congreso-
dc.relation.publisherversionhttp://meetingorganizer.copernicus.org/EGU2015/posters/17514-
dc.date.updated2016-11-29T13:05:03Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066eng-
dc.rights.licensehttps://creativecommons.org/licenses/by/3.0/legalcode-
dc.relation.csic-
dc.type.coarhttp://purl.org/coar/resource_type/c_6670es_ES
item.openairetypepóster de congreso-
item.grantfulltextopen-
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
Aparece en las colecciones: (ICM) Comunicaciones congresos
Ficheros en este ítem:
Fichero Descripción Tamaño Formato
Gomez_de_la_Peña_et_al_2015_EGU2015-14076.pdf17,77 kBAdobe PDFVista previa
Visualizar/Abrir
Show simple item record

CORE Recommender

Page view(s)

112
checked on 23-abr-2024

Download(s)

57
checked on 23-abr-2024

Google ScholarTM

Check


Este item está licenciado bajo una Licencia Creative Commons Creative Commons