English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/71826
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorMancilla, Flor de Lis-
dc.contributor.authorStich, D.-
dc.contributor.authorMorales, José-
dc.contributor.authorJulià, Jordi-
dc.contributor.authorDiaz, J.-
dc.contributor.authorPazos, Antonio-
dc.contributor.authorCórdoba, Diego-
dc.contributor.authorPulgar, J. A.-
dc.contributor.authorIbarra, Pedro-
dc.contributor.authorHarnafi, M.-
dc.contributor.authorGonzález-Lodeiro, Francisco-
dc.date.issued2012-
dc.identifierdoi: 10.1029/2011JB008608-
dc.identifierissn: 0148-0227-
dc.identifier.citationJournal of Geophysical Research 117 B02312 (2012)-
dc.identifier.urihttp://hdl.handle.net/10261/71826-
dc.description.abstractDuring the TopoIberia experiment, a total of 26 seismic broadband stations were recording in northern Morocco, providing for the first time extended regional coverage for investigating structure and seismotectonics of the southern branch of the Betic-Rif arc, its foreland, and the Atlas domain. Here, we analyze P-to-S converted waves in teleseismic receiver functions to infer gross crustal properties as thickness and V p/V s ratio. Strong lateral variations of the crustal thickness are observed throughout the region. Crustal thicknesses vary between 22 and 44 km and display a simple geographic pattern that divides the study area into three domains: entire northwestern Morocco underlain by a thickened crust with crustal thicknesses between 35 and 44 km; northeastern Morocco affected by significant crustal thinning, with crustal thicknesses ranging from 22 to 30 km, with the shallowest Moho along the Mediterranean coast; and an extended domain of 27-34 km thick crust, farther south which includes the Atlas domain and its foreland regions. V p/V s ratios show normal values of ∼1.75 for most stations except for the Atlas domain, where several stations give low V p/V s ratios of around 1.71. The very sharp transition from thick crust in northwestern Morocco to thin crust in northeastern Morocco is attributed to regional geodynamics, possibly the realm of present-day subcrustal dynamics in the final stage of western Mediterranean subduction. Crustal thicknesses just slightly above 30 km in the southern domain are intriguing, showing that high topography in this region is not isostatically compensated at crustal level. Copyright © 2012 by the American Geophysical Union.-
dc.description.sponsorshipThis is a contribution of the Consolider-Ingenio 2010 project TOPO-IBERIA (CSD2006-00041). Additional funding is provided by projects CGL2006-01171, CGL2008-01830, and P09-RNM-5100.-
dc.language.isoeng-
dc.publisherWilliam Byrd Press for Johns Hopkins Press-
dc.rightsopenAccess-
dc.titleCrustal thickness variations in northern Morocco-
dc.typeartículo-
dc.identifier.doi10.1029/2011JB008608-
dc.relation.publisherversionhttp://dx.doi.org/10.1029/2011JB008608-
dc.date.updated2013-03-11T08:22:03Z-
dc.description.versionPeer Reviewed-
Appears in Collections:(IGEO) Artículos
(ICTJA) Artículos
Files in This Item:
File Description SizeFormat 
Diaz Cusi jgrb17010.pdf2,78 MBAdobe PDFThumbnail
View/Open
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.