[HTML][HTML] Evolution of a low convergence collisional orogen: a review of Pyrenean orogenesis
The Pyrenees is a collisional orogen built by inversion of an immature rift system during
convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The …
convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The …