High resolution Moho topography map beneath Iberia and Northern Morocco from receiver function analysis

• Published in: Tectonophysics 2015-11, Vol.663, p.203-211
• Main Authors: Mancilla, Flor de Lis, Diaz, Jordi
• Format: Article
• Language: English
• Subjects: Crustal depth map; H–κ; Iberia and Northern Morocco; Receiver functions
• ISSN: 0040-1951; 1879-3266
• DOI: 10.1016/j.tecto.2015.06.017

Crustal thickness maps at regional scales are typically compiled using estimations inferred from different geophysical datasets providing a variable coverage of the investigated area. Consequently, spurious effects related to changes in data resolution or artifacts in grid interpolation may affect significant zones of those maps. The TopoIberia-IberArray broad-band seismic network, covering the Iberian Peninsula and Northern Morocco with stations distributed on a regular 60×60km grid provides a unique opportunity to avoid such technical problems and to obtain a crustal thickness map derived from a same method sampling evenly all the region. Data from more than 340 stations has been gathered and analyzed using the P-to-S conversion phases at the Moho discontinuity (receiver functions). The crustal thickness has been inferred applying the classical H–κ stacking technique, though in regions of complex crustal structure, we have preferred to estimate the thickness directly from the arrival time of the converted phase at some sites. The topography of the Moho discontinuity is strongly correlated with tectonic processes. The investigated area, extending from the Sahara platform to the Bay of Biscay, has a great geodynamic diversity, including, North to South, crustal imbrication in the Pyrenean and Cantabrian range, a large and relatively undisturbed Variscan Massif in the center of Iberia and areas of complex and still not completely understood geodynamics in the Alboran crust domain and the Atlas range. The crustal thickness map reflects this diversity, showing variations reaching 30km between the thickest and thinnest zones of continental crust. The final map has an overall similarity with previous estimations of the crustal thickness using independent data, as those coming from more sparse deep seismic sounding profiles, but provides further constraints at regional scale. •New crustal thickness map of the westernmost Mediterranean from RF analysis.•The topography of the Moho discontinuity is strongly correlated with tectonic processes.•The crustal thickness map shows variations reaching 30km.•New RF data confirms the presence of a thick crust beneath the Rif domain.