This paper provides a synthesis of current data and interpretations on the crustal structure of
the Pyrenean-Cantabrian orogenic belt, and presents new tectonic models for …

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 pandemic caused by COVID-19 has changed the mindset of many consumers. They are
increasingly aware of the risks of not caring for the planet. Before the pandemic, there was a …

The kinematic evolution of the Pyrenees was largely controlled by structural and thermal
heterogeneities inherited from a precursor rift system, resulting in complex along-strike …

We present new crust and lithosphere thickness maps of the African mainland based on
integrated modeling of elevation and geoid data and thermal analysis. The approach …

The study of fluvial network rearrangement provides a key to understand past and future
landscape evolution. Large perturbations of hydrographic basins such as the change from …

Recent models support the view that the Pyrenees were formed after the inversion of a
previously highly extended continental crust that included exhumed upper mantle rocks …

The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and
deformation belts with a wide variety of structural trends. The Spanish‐Portuguese Central …

Abstract The Bay of Biscay-Pyrenean rift system is a world-class example of an inverted
hyperextended rift. However, tectonic questions such as the linkage of the extensional …

In this work the thermal structure of the Iberian Peninsula is derived from magnetic data by
calculating the bottom of the magnetization, assumed to be the Curie‐point depth (CPD) …