Upper Plate Controls on the Formation of Broken Foreland Basins in the Andean Retroarc Between 26°S and 28°S: From Cretaceous Rifting to Paleogene and Miocene Broken Foreland Basins

Abstract Marked along‐strike changes in stratigraphy, mountain belt morphology, basement exhumation, and deformation styles characterize the Andean retroarc; these changes have previously been related to spatiotemporal variations in the subduction angle. We modeled new apatite fission track and apat...

Full description

Bibliographic Details
Main Authors: S. Zapata, E. R. Sobel, C. Del Papa, J. Glodny
Format: Article
Language:English
Published: Wiley 2020-07-01
Series:Geochemistry, Geophysics, Geosystems
Online Access:https://doi.org/10.1029/2019GC008876