The origin of the depressions interrupting the eastern Sierra Pampeanas broken foreland, explained by localized crustal extension through the juan Fernández ridge path, using gravimetric data

Author:

Gimenez MarioORCID,Villegas A Raquel J.,Richarte Daniel,Lince Kinger Federico,Alvarez Orlando,Nacif Silvina,Folguera Andrés

Funder

Agencia Nacional de Promoción Científica y Tecnológica

Consejo Nacional de Investigaciones Científicas y Técnicas

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference36 articles.

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3. Geometry and brittle deformation of the subducting Nazca Plate, central Chile, and Argentina;Anderson;Geophys. J. Int.,2007

4. Models of crustal thickness for South America from seismic refraction, receiver functions, and surface wave tomography;Assumpção;Tectonophysics,2013

5. Predicted path for hotspot tracks off South America since Paleocene times: tectonic implications of ridge-trench collision along the Andean margin;Bello-González;Gondwana Res.,2018

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