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dc.contributor.authorSchmelzbach, C.-
dc.contributor.authorZelt, Colin-
dc.contributor.authorJuhlin, C.-
dc.contributor.authorCarbonell, Ramón-
dc.date.accessioned2010-01-13T13:23:23Z-
dc.date.available2010-01-13T13:23:23Z-
dc.date.issued2008-08-
dc.identifier.citationGeophysical Journal International 175(2): 689 - 712(2008)en_US
dc.identifier.issn0956-540X-
dc.identifier.urihttp://hdl.handle.net/10261/20015-
dc.description.abstractImaging the architecture of the shallow crust of the South Portuguese Zone fold-and-thrust belt is essential to extend surface mapped geological information to depth and to help in developing models of the ore-bearing Iberian Pyrite Belt part of the Variscan orogeny. The recently acquired IBERSEIS seismic-reflection data set provides, for the first time, detailed images of the entire crust, but source-generated noise masks the earliest reflections and limits the shallowest observed signals to depths >500 m. We inverted P- and SV first-arrival traveltimes for the smoothest minimum-structure velocity models, imaging the shallowest few hundreds of metres along four in total ∼60-km-long profiles. A comparison of a 2-D and 2.5-D (3-D forward and 2-D inverse problem) crooked-line inversion scheme revealed that the crooked-line geometry has a negligible effect on the final images. Resolution of the final preferred models was assessed on the basis of an extensive series of checkerboard tests, showing a slightly lower resolution capability of the SV -data due to greater data uncertainty, fewer number of picks and more limited source–receiver offsets compared with the P-data. The preferred final models compare favourably with the mapped surface geology, showing relatively high and uniform velocities (>5.25 km s−1) for the flysch group in the southern part of the investigation area. Low velocities (∼4.5 km s−1) are found for the 'La Puebla de Guzman antiform' in the centre of the investigation area, where the phyllite–quartzite group is exposed. Velocities fluctuate the most along the northernmost ∼20 km. Velocity variations reflect more the state of tectonic deformation than being directly correlated with the mapped lithologies. Based on a comparison with coincident seismic-reflection data along the southern half of the area, we suggest that two areas of low to intermediate ratios (∼1.85–1.9) correspond to occurrences of thick and less deformed flysch-group units, whereas high ratios (∼1.95) are interpreted to indicate increased porosity due to intense fracturing.en_US
dc.format.extent2734282 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoengen_US
dc.publisherWiley-Blackwellen_US
dc.rightsclosedAccessen_US
dc.subjectInverse theoryen_US
dc.subjectControlled source seismologyen_US
dc.subjectBody wavesen_US
dc.subjectSeismic tomographyen_US
dc.subjectFractures and faultsen_US
dc.subjectCrustal structureen_US
dc.titleP- and SV-velocity structure of the South Portuguese Zone fold-and-thrust belt, SW Iberia, from traveltime tomographyen_US
dc.typeartículoen_US
dc.identifier.doi10.1111/j.1365-246X.2008.03937-
dc.description.peerreviewedPeer revieweden_US
dc.relation.publisherversionhttp://dx.doi.org/10.1111/j.1365-246X.2008.03937en_US
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