Data from deep boreholes, seismic surveys, and surface geology are used to reconstruct the
sedimentary infilling of the Cenozoic Madrid Basin. Eight main depositional sequences and …

The Madrid basin is intracratonic and triangular in form, being bounded on its three sides by
Tertiary mountain ranges: the Spanish Central System in the north, the Toledo mountains in …

The Valencia trough, located between the Spanish mainland and the Balearic islands,
corresponds to a late Oligocene to recent sedimentary basin that is characterized by a highly …

Abstract The Montalbân Basin (30× 15 km wide) is located within the Iberian Chain (N
Spain), and filled with syn-tectonic Tertiary (Eocene to Lower Miocene) deposits, with a …

The integration of subsurface data from the offshore Valencia trough areas and data
obtained from geological studies carried out on its emerged margins permits recognition of …

The Catalan margin belongs to the northern sector of the margin that separates the
extremely thinned continental crust of the Valencia trough from the undeformed or thickened …

The structure and evolution of the Valencia Trough (western Mediterranean), a Neogene
basin bordered in the north by prominent Oligocene-Early Miocene grabens in the Catalan …

The Palomares continental margin is located in the southeastern part of Spain. The margin
main structure was formed during Miocene times, and it is currently part of the wide …

Contractional deformation in the transition between the Iberian and Catalan Coastal Ranges
(Linking Zone) generated both thin‐skinned structures detached in low‐strength Triassic …

We present the structural study of the Cameros Massif (NW Iberian Chain, Spain), taking into
account data from surface geology, deep boreholes and seismic reflection profiles. The main …