Abstract During the Paleogene and Neogene the NE Iberian plate underwent significant
paleogeographic changes driven by the Iberian and European plate collision and the …

We present new 3D seismic and well data from the Ebro Margin, NW Mediterranean Sea, to
shed new light on the processes that formed the Messinian Erosion Surfaces (MES) of the …

We study the structure of the Llevant ranges in Mallorca with special emphasis on the
Cenozoic extensional evolution of the island, which we integrate in a new geodynamic …

Karst fills from the onshore Penedès Basin and offshore València Trough display red, pink,
orange and ochre colours. Their Mössbauer spectra indicate that Fe3+ contained in goethite …

Different types of fractures and fault rocks occur within the major normal fault zones
bordering the NW of the Neogene Penedès basin (NE Spain). In the southwest part of the …

Los primeros hallazgos de vertebrados continentales en la cuenca del Vallès-Penedès se
remontan a las últimas décadas del siglo XIX, poco después de que se iniciara la …

The Miocene siliciclastic sediments infilling the Vallès‐Penedès half‐graben are affected by
two sets of structures developed during the extensional tectonics that created the basin. The …

Las numerosas obras de Ingeniería Civil que se han realizado en los últimos años en la
depresión de Barcelona (ampliación del aeropuerto, ampliación del metro y AVE …

Minor normal faults affecting Miocene conglomerates of the Barcelona Plain are constituted
by a poorly developed fault core without a damage zone. Fault rocks are made of a red …

Processes influencing the thermal state of the continental crust, such as heat upwelling
related to rifting and isotherm reorganization due to mass redistribution by erosion …