We review a widespread project database for Devonian–Carboniferous magmatism in the
Sierras Pampeanas and Frontal Cordillera between 27° and 35° S, including petrological …

Abstract Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina
were driven by subduction, and interrupted by collision of continental ribbons of Laurentian …

Abstract The proto-Andean and Early Andean evolution of the southwestern Gondwana
margin comprises three stages that differ in their magmatic evolution and deformational …

Permian to Triassic igneous rocks cropping out in the Coastal and Frontal cordilleras in
northern Chile between 28 degrees 00'S and 30 degrees 15'S have long been interpreted to …

We present a new conceptual model to explain the first order Permian-Triassic evolution of
the whole> 30 000 km long Pangea margin facing the Panthalassa ocean. Compilation of …

A temporal and tectonic framework for the initiation of the Andean magmatism at its earliest
stages is presented in this work, based on the current geological, geochemical, and …

Under hyperarid climate conditions, pedogenesis is driven by the atmospheric deposition
and subsequent accumulation of easily to moderately soluble salts forming extreme types of …

Abstract The Arrayán Formation comprises a thick, well stratified, strongly folded turbiditic
succession, exposed along the Chilean coast, between 31° 30′ and 32° S. It is interpreted …

Triassic rock units of northern Chile (28-29 degrees S) record the transition, both in time and
space, between two major orogenies that affected the southwestern margin of South …

In the region of Pichilemu (Central Chile), the exhumed roots of the Carboniferous paleo-
accretionary wedge developed during subduction of an oceanic realm underneath the …