Estimation of the Crustal Bulk Properties Beneath Mainland Portugal from P-Wave Teleseismic Receiver Functions

• Published in: Pure and applied geophysics 2016-06, Vol.173 (6), p.1949-1970
• Main Authors: Dündar, Süleyman, Dias, Nuno A., Silveira, Graça, Kind, Rainer, Vinnik, Lev, Matias, Luís, Bianchi, Marcelo
• Format: Article
• Language: English
• Subjects: Algorithms; Cenozoic; Coastal; Continental dynamics; Crusts; Earth and Environmental Science; Earth Sciences; Geophysics; Geophysics/Geodesy; Marine; Mesozoic; Orogeny; Paleozoic; Receivers; Rifting; Seismic properties; Seismology; Stacking; Sutures; Thinning
• ISSN: 0033-4553; 1420-9136
• DOI: 10.1007/s00024-016-1257-4

In this work, we present results from teleseismic P-wave receiver functions (PRFs) obtained in Portugal, Western Iberia. A dense seismic station deployment conducted between 2010 and 2012, in the scope of the WILAS project and covering the entire country, allowed the most spatially extensive probing on the bulk crustal seismic properties of Portugal up to date. The application of the H – κ stacking algorithm to the PRFs enabled us to estimate the crustal thickness ( H ) and the average crustal ratio of the P- and S-waves velocities V p / V s ( κ ) for the region. Observations of Moho conversions indicate that this interface is relatively smooth with the crustal thickness ranging between 24 and 34 km, with an average of 30 km. The highest V p / V s values are found on the Mesozoic–Cenozoic crust beneath the western and southern coastal domain of Portugal, whereas the lowest values correspond to Palaeozoic crust underlying the remaining part of the subject area. An average V p / V s is found to be 1.72, ranging 1.63–1.86 across the study area, indicating a predominantly felsic composition. Overall, we systematically observe a decrease of V p / V s with increasing crustal thickness. Taken as a whole, our results indicate a clear distinction between the geological zones of the Variscan Iberian Massif in Portugal, the overall shape of the anomalies conditioned by the shape of the Ibero-Armorican Arc, and associated Late Paleozoic suture zones, and the Meso-Cenozoic basin associated with Atlantic rifting stages. Thickened crust (30–34 km) across the studied region may be inherited from continental collision during the Paleozoic Variscan orogeny. An anomalous crustal thinning to around 28 km is observed beneath the central part of the Central Iberian Zone and the eastern part of South Portuguese Zone.