Uncommonly long‐lived subduction and variable plate geometry along the South American
Andean Plate margin resulted in diverse relationships between magmatic flux and …

The intraplate fault-block mountains and intermontane deposits of the Gastre Basin, which
are recorded more than 550 km east of the Andean trench in central Patagonia, Argentina …

In this contribution we address the current controversial issues related to the age,
correlation, tectonic setting and paleogeographic links of the Cenozoic fossiliferous marine …

The Chachil depocenter is located in the Andean foreland, at∼ 39° S. Its origin relates to the
syn-rift phase of the Neuquén Basin, a large marine embayment developed along the …

Abstract During Mid-Cenozoic times, voluminous and genetically heterogeneous volcanism
took place across North Patagonia in response to a period of plate tectonic reorganization …

The Aluminé fold and thrust belt between 38° 30′ and 40° 30′ S is the result of two
periods of progression of deformation toward the foreland. The chronology of deformation …

Voluminous Paleogene magmatic rocks (44 to 29 Ma) are found in a retroarc position in the
Northern Patagonian to Southern Central Andes (~ 39–42° S), whose origin remains …

Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El
Maitén Belt constitute a partial record of the Andean exhumation, defining a synorogenic …

This paper analyzes the style, distribution, mechanics and timing of deformation of the
Andean retroarc zone between 39° and 40° S, in the North Patagonian Andes. Field …

Although extensional deformation plays a significant part of Andean history, the causes
behind its driving mechanisms and its impact throughout the geological record remain …