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...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Wiley
2020-07-01
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Series: | Geochemistry, Geophysics, Geosystems |
Online Access: | https://doi.org/10.1029/2019GC008876 |