Publications

Late Carboniferous Paleomagnetism From North Qiangtang Block Reveals a Multibranched Paleo-Tethys Ocean
The North Qiangtang Block occupies a pivotal position within the eastern Tethyan realm, and its paleogeographic reconstruction is …
Late Carboniferous Paleomagnetism From North Qiangtang Block Reveals a Multibranched Paleo-Tethys Ocean
Neoproterozoic-Palaeozoic detrital sources in the Variscan foreland of northern Iberia: primary vs. recycled sediments
The Cantabrian Zone, in the Variscan belt of Western Europe, has one of the most continuous Ediacaran-Palaeozoic stratigraphic …
Progressive orocline formation in the Eastern Pontides–Lesser Caucasus
The Eastern Pontides–Lesser Caucasus fold–thrust belt displays a peculiar northwards arc-shaped geometry that was defined as an …
Paleomagnetism of the Central Iberian bend's hinge: too many oroclines in the Iberian variscides
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the north and the Central Iberian curve, …
Significance of detrital zircons in Siluro-Devonian rocks from Iberia
Seven samples of Siluro-Devonian sedimentary rocks from the Cantabrian and Central Iberian zones of the Iberian Variscan belt have been …
Dating of lithospheric buckling: 40Ar/39Ar ages of syn-orocline strike-slip shear zones in northwestern Iberia
Orogenic curvature is a ubiquitous feature of mountain belts, and the plate tectonic and geodynamic setting responsible for the …
Diachronous post‐orogenic magmatism within a developing orocline in Iberia, European Variscides
The amalgamation of Pangea during the Carboniferous produced a winding mountain belt the Variscan orogen of West Europe. In the Iberian …