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http://hdl.handle.net/10261/20015
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Campo DC | Valor | Lengua/Idioma |
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dc.contributor.author | Schmelzbach, C. | - |
dc.contributor.author | Zelt, Colin | - |
dc.contributor.author | Juhlin, C. | - |
dc.contributor.author | Carbonell, Ramón | - |
dc.date.accessioned | 2010-01-13T13:23:23Z | - |
dc.date.available | 2010-01-13T13:23:23Z | - |
dc.date.issued | 2008-08 | - |
dc.identifier.citation | Geophysical Journal International 175(2): 689 - 712(2008) | en_US |
dc.identifier.issn | 0956-540X | - |
dc.identifier.uri | http://hdl.handle.net/10261/20015 | - |
dc.description.abstract | Imaging 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.extent | 2734282 bytes | - |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | en_US |
dc.publisher | Wiley-Blackwell | en_US |
dc.rights | closedAccess | en_US |
dc.subject | Inverse theory | en_US |
dc.subject | Controlled source seismology | en_US |
dc.subject | Body waves | en_US |
dc.subject | Seismic tomography | en_US |
dc.subject | Fractures and faults | en_US |
dc.subject | Crustal structure | en_US |
dc.title | P- and SV-velocity structure of the South Portuguese Zone fold-and-thrust belt, SW Iberia, from traveltime tomography | en_US |
dc.type | artículo | en_US |
dc.identifier.doi | 10.1111/j.1365-246X.2008.03937 | - |
dc.description.peerreviewed | Peer reviewed | en_US |
dc.relation.publisherversion | http://dx.doi.org/10.1111/j.1365-246X.2008.03937 | en_US |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairetype | artículo | - |
item.grantfulltext | none | - |
item.cerifentitytype | Publications | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | No Fulltext | - |
item.languageiso639-1 | en | - |
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