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Please use this identifier to cite or link to this item: http://hdl.handle.net/1813/5282
Title: Lithospheric seismic velocity discontinuities beneath the Arabian Shield
Authors: Sandvol, E.
Seber, D.
Barazangi, M.
Vernon, F.
Mellors, R.
Al-Amri, A.
Keywords: Crustal structure of Arabian shield
Saudi Arabia
Receiver function
Seismology
Issue Date: 1998
Publisher: American Geophysical Union
Citation: Geophysical Research Letters, vol. 25, p. 2873-2876, 1998
Abstract: We determined crustal and lithospheric mantle velocity structure beneath the Arabian Shield through the modeling of receiver function stacks obtained from teleseismic P waves recorded by the 9 station temporary broadband array in western Saudi Arabia. The receiver function deconvolution technique was used to isolate the receiver-side PS mode conversions. A grid search method, which should yield an unbiased global minimum, was used to solve for a shear wave velocity model that is optimal and has the minimum number of layers needed to fit the receiver function waveform. Results from this analysis show that the crustal thickness in the shield area varies from 35 to 40 km in the west, adjacent to the Red Sea, to 45 km in central Arabia. Stability tests of each solution indicate that the models are relatively well constrained. We have also observed evidence for a large positive velocity contrast at sub-Moho depths at four stations at depths of 80 to 100 km. This discontinuity may represent a change in rheology in the lower part of the lithosphere or remnant structure from the formation of the Arabian Shield.
Description: An edited version of this paper was published by the American Geophysical Union (AGU). Copyright 1998, AGU. See also: http://www.agu.org/pubs/crossref/1998/98GL02214.shtml; http://atlas.geo.cornell.edu/SaudiArabia/publications/Sandvol1998.htm
URI: http://hdl.handle.net/1813/5282
ISSN: 0094-8276
Appears in Collections:Prof. Muawia Barazangi
Middle East and North Africa Region Projects

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