Show simple item record

dc.contributor.authorCalvert, A.
dc.contributor.authorSandvol, E.
dc.contributor.authorSeber, D.
dc.contributor.authorBarazangi, M.
dc.contributor.authorRoecker, S.
dc.contributor.authorMourabit, T.
dc.contributor.authorVidal, F.
dc.contributor.authorAlguacil, G.
dc.contributor.authorJabour, N.
dc.date.accessioned2007-01-26T16:24:19Z
dc.date.available2007-01-26T16:24:19Z
dc.date.issued2000
dc.identifier.citationJournal of Geophysical Research, vol. 105, p. 10871-10898, 2000en_US
dc.identifier.issn0148-0227
dc.identifier.urihttps://hdl.handle.net/1813/5275
dc.descriptionAn edited version of this paper was published by the American Geophysical Union. Copyright 2000, AGU. See also: http://www.agu.org/pubs/crossref/2000/2000JB900024.shtml; http://atlas.geo.cornell.edu/morocco/publications/calvert2000.htmen_US
dc.description.abstractA number of different geodynamic models have been proposed to explain the extension that occurred during the Miocene in the Alboran Sea region of the western Mediterranean despite the continued convergence and shortening of northern Africa and southern Iberia. In an effort to provide additional geophysical constraints on these models, we performed a local, regional, and teleseismic tomographic travel time inversion for the lithospheric and upper mantle velocity structure and earthquake locations beneath the Alboran region in an area of 800 x 800 km^2. We picked P and S arrival times from digital and analog seismograms recorded by 96 seismic stations in Morocco and Spain between 1989 and 1996 and combined them with arrivals carefully selected from local and global catalogs (1964-1998) to generate a starting data set containing over 100,000 arrival times. Our results indicate that a N-S line of intermediate depth earthquakes extending from crustal depths significantly inland from the southern Iberian coat to depths of over 100 km beneath the center of the Alboran Sea coincided with a W to E transition from high to low velocities imaged in the uppermost mantle. A high-velocity body, striking approximately NE-SW, is imaged to dip southeastwards from lithospheric depths beneath the low-velocity region to depths of ~350 km. Between 350 and 500 km the imaged velocity anomalies become more diffuse. However, pronounced high-velocity anomalies are again imaged at 600 km near an isolated cluster of deep earthquakes. In addition to standard tomographic methods of error assessment, the effects of systematic and random errors were assessed using block shifting and bootstrap resampling techniques, respectively. We interpret the upper mantle high-velocity anomalies as regions of colder mantle that originate from lithospheric depths. These observations, when combined with results from other studies, suggest that delamination of a continental lithosphere played an important role in the Neogene and Quaternary evolution of the region.en_US
dc.format.extent6807673 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoenen_US
dc.publisherAmerican Geophysical Unionen_US
dc.subjectWestern Mediterraneanen_US
dc.subjectAlboran Seaen_US
dc.subjectVelocity Tomographyen_US
dc.subjectEarthquakesen_US
dc.subjectBetic Mountainsen_US
dc.subjectRif Mountainsen_US
dc.subjectGeodynamic Evolution of northern Moroccoen_US
dc.titleGeodynamic evolution of the lithosphere and upper mantle beneath the Alboran region of the western Mediterranean: Constraints from travel time tomographyen_US
dc.typeperiodicalen_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

Statistics