Sebastián Parra Irribarra

Onshore surface–subsurface correlation of orogenic structures and the continuation of the late Paleozoic Gondwanides in the Tierra del Fuego fold-and-thrust belt, southern Patagonia

Background The Cretaceous–Cenozoic Tierra del Fuego fold-and-thrust belt in southern Patagonia exposes Paleozoic–Cenozoic rocks recording the protracted, subduction-dominated tectonic evolution of South America, from Cambrian–Ordovician magmatism to Permian metamorphism, Jurassic...