Abstract. Normal incidence seismic data provide the best images of the crust and
lithosphere. When properly designed and continuous, these sections greatly
contribute to understanding the geometry of orogens and, along with
surface geology, unraveling their evolution. In this paper we present the
most complete transect, to date, of the Iberian Massif, the westernmost
exposure of the European Variscides. Despite the heterogeneity of the
dataset, acquired during the last 30 years, the images resulting from
reprocessing the data with a homogeneous workflow allow us to clearly define the
crustal thickness and its internal architecture. The Iberian Massif crust,
formed by the amalgamation of continental pieces belonging to Gondwana and
Laurussia (Avalonian margin), is well structured in the upper and lower crust. A
conspicuous mid-crustal discontinuity is clearly defined by the top of the
reflective lower crust and by the asymptotic geometry of reflections that
merge into it, suggesting that it has often acted as a detachment. The
geometry and position of this discontinuity can give us insights into the
evolution of the orogen (i.e., of the magnitude of compression and the
effects and extent of later-Variscan gravitational collapse). Moreover, the
limited thickness of the lower crust below, in central and northwestern Iberia, might
have constrained the response of the Iberian microplate to Alpine
shortening. Here, this discontinuity, featuring a Vp (P-wave velocity) increase, is observed as
an orogen-scale boundary with characteristics compatible with those of the
globally debated Conrad discontinuity.