The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and Laurussia during the Carboniferous. From all swirls of this orogen, a double curve in Iberia stands out, the coupled Cantabrian Orocline and Central …
The Cantabrian Zone, in the Variscan belt of Western Europe, has one of the most continuous Ediacaran-Palaeozoic stratigraphic successions in the world. This succession has been previously extensively studied, including several detrital zircon U-Pb …
October 2018, Bruno and me sampled many different Devonian and Carboniferous volcanic rocks in SW Iberia
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the north and the Central Iberian curve, an alleged orocline belt of opposite curvature, to the south. The Cantabrian Orocline is kinematically well …
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW Iberia. The extensively studied kinematics of its core, the foreland of the orogen, indicates that the structure is secondary, i.e. acquired after the …
We performed a field trip to the Iberian range to evaluate the tectonic history from Devonian to now. Mark Diederen made an excellent B.Sc. thesis out of it that resulted in a paper in Tectonics
During my PhD Thesis I perfomed lots of fieldwork in the Cantabrian Zone, Several papers came out after these field seasons