Tectono-thermal history of the intraplate San Bernardo fold and thrust belt in central Patagonia inferred by low-temperature thermochronology
Author:
Funder
Universita degli Studi di Padova
CNRS
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geology
Reference93 articles.
1. Comparative structural analysis of inverted structures in the San Bernardo fold belt (Golfo San Jorge basin, Argentina): inversion controls and tecto-sedimentary context of the Chubut Group;Allard;J. S. Am. Earth Sci.,2020
2. Innovations in (U–Th)/He, fission track, and trapped charge thermochronometry with applications to earthquakes, weathering, surface-mantle connections, and the growth and decay of mountains;Ault;Tectonics,2019
3. Heat flow and lithospheric thickness analysis in the Patagonian asthenospheric windows, southern South America;Ávila;Tectonophysics,2018
4. Lithospheric thinning and dynamic uplift effects during slab window formation, southern Patagonia (45°-55° S);Ávila;J. Geodyn.,2020
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1. Strain partitioning in the Patagonian Broken Foreland: influence of structural inheritance of early Andean deformation;Journal of the Geological Society;2024-03-07
2. Denudation of the Cordillera and intraplate belt in central Patagonia inferred by detrital multi-dating of foreland basin deposits;Sedimentary Geology;2022-10
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