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

Native hydrogen (H2) may represent a new carbon free‐energy resource, but to date there is
no specific exploration guide to target H2‐fertile geological settings. Here, we present the …

Three crustal-scale sequentially restored cross-sections along the Central External Betic
Cordillera enable us to pinpoint the role of extreme crustal thinning, tectonic inheritance and …

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 …

Fault barriers are key structures for studying seismic hazard in regions of intense brittle
deformation. The interaction between fault sets affects their seismogenic behavior, if some of …

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 …

Critical gravity and magnetic data suggest the presence of a continuous zigzag exhumed
mantle body inside the attenuated crust of the north Iberia continental margin. We propose …

Understanding active tectonics and seismicity in extensional settings requires the analysis of
high‐angle normal faults (HANFs) and the transfer of deformation at depth. The debate …

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 …