A kinematic reconstruction of Iberia using intracontinental strike‐slip corridors

Despite considerable progress in restoring rifted margins, none of the current kinematic models can restore Mesozoic motion Iberian block full agreement with circum-Iberian geology. This conflict requires a revision description at onset divergence. The region has unique geological dataset that allows calibration and testing reconstructions therefore it is an ideal candidate for intracontinental restoration approaches. Here we define deforming regions, referred to as strike-slip corridors, based on alignments rift basins and/or transfer zones bordering rigid continental blocks. We use these corridors data from southern N-Atlantic Tethys path Flemish Cap, Ebro Iberia resulting model compatible recently published interpretations describing Large-scale may offer valid boundary condition reconstructing divergence settings.