The surface of the Earth is the ever-changing expression of the dynamic processes
occurring at depth and at or above its surface. However, our ability to “read” landscapes in …

The dimensions, the geographical position and the complex geological history of the Iberian
Peninsula makes it a unique and singular target to study its crustal and upper mantle …

Although many different mechanisms for subduction initiation have been proposed, only few
of them are viable in terms of consistency with observations and reproducibility in numerical …

Surface geology, well data, and seismic profiles confirm the occurrence of an extensive salt
canopy in the western Betic Cordillera. Upper Triassic (Keuper) evaporites were emplaced …

Abstract The Canary and Madeira provinces in the Central‐East Atlantic Ocean are
characterized by an irregular spatio‐temporal distribution of volcanism along the hotspot …

Abstract The High Atlas intracontinental belt is an inverted rift formed along the Northwest
African Craton, between the Central Atlantic Ocean and the Africa-Eurasia plates' …

In typical subduction systems, plate convergence is subperpendicular to the trench. The
Gibraltar Arc System is exceptional, with its narrow subduction arc oriented N‐S and laterally …

Abstract The Atlas‐Meseta intracontinental orographic system of Morocco experienced
recent, large‐scale surface uplift as documented by elevated late Miocene, shallow‐water …

A long-standing question in geodynamics is whether mantle flow is driven by the plate
motion alone, or mantle upwelling makes a significant contribution to it. Subducting slabs …

For seismic exploration, excellent seismic records are of extreme significance. However,
because of extensive mining over a long period, spare natural resources are primarily …