Pangea

Conical folding in the core of an orocline

I presented this Mondrian style poster at EGU 2013

Supercontinent and Superplate?

This poster won the NAC14 (National Earth Sciences congress of the Netherlands) poster award in 2016

Extending the Cantabrian Orocline to two continents (Gondwana and Laurussia). Paleomagnetism from South Ireland.

Regional Variscan structure in southern Ireland follows a gentle arcuate trend of ca. 25° concave to the SE that apparently follows the geometry of the Cantabrian Orocline (NW Iberia) when Iberia is restored to its position prior to the opening of …

One or two oroclines in the Variscan orogen of Iberia? Implications for Pangea amalgamation

The supercontinent Pangea formed in the late Carboniferous as a result of the Gondwana-Laurussia collision, producing the strongly sinuous Variscan–Alleghanian orogen. Iberia is interpreted to comprise two Variscan bends, forming an S-shaped orogenic …

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 development of curved orogens is a subject of debate. In order to distinguish between different models of orocline …