Constraints on the Neogene growth of the central Patagonian Andes at the latitude of the Chile triple junction (45–47°S) using U/Pb geochronology in synorogenic strata

@article{Folguera2018ConstraintsOT,
  title={Constraints on the Neogene growth of the central Patagonian Andes at the latitude of the Chile triple junction (45–47°S) using U/Pb geochronology in synorogenic strata},
  author={Andr{\'e}s Folguera and A. Encinas and A. Echaurren and Guido M Gianni and Dar{\'i}o Leandro Orts and V. Valencia and Gabriel Carrasco},
  journal={Tectonophysics},
  year={2018}
}
The role of slab geometry in the exhumation of cordilleran-type orogens and their forelands: Insights from northern Patagonia
In cordilleran-type orogens, subduction geometry exerts a fundamental control on the tectonic behavior of the overriding plate. An integrated low-temperature, large thermochronological data set is
Tectonic vs. climate controls on the evolution of a miocene intermontane basin, Patagonian Andean foreland, Argentina
The interaction of tectonics and climate is considered the main determining factor in the development of different depositional systems (from aeolian to alluvial to lacustrine environments) in
TECTONOSTRATIGRAPHIC SIGNIFICANCE OF THE NEOGENE SEDIMENTARY RECORD OF NORTHWESTERN AUSTRAL-MAGALLANES BASIN, ARGENTINEAN PATAGONIA
Despite their geodynamic significance, the stratigraphy and paleoenvironments of the lower-middle Miocene clastic deposits, genetically related to subduction-driven lithospheric processes at the
Quantifying Tectonic and Glacial Controls on Topography in the Patagonian Andes (46.5°S) From Integrated Thermochronometry and Thermo‐Kinematic Modeling
The Patagonian Andes have been used to illustrate the dependency of major topographic changes in response to glacial erosion processes dominating over tectonic deformation and uplift. Here, we
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Fission track (FT) analysis is applied to assess the Mesozoic and Cenozoic thermal and denudational history of the Patagonian Andes between 44° and 51°S and the geologic and geomorphic response of
Tectonic development of the North Patagonian Andes and their related Miocene foreland basin (41°30′‐43°S)
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tectonic inversion of extensional structures of Early to Middle Jurassic age in the Main Andes to
Late Cenozoic geomorphic and tectonic evolution of the Patagonian Andes between latitudes 42°S and 46°S: An appraisal based on fission-track results from the transpressional intra-arc Liquiñe-Ofqui fault zone
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Neogene uplift of central eastern Patagonia: Dynamic response to active spreading ridge subduction?
The Chile Triple Junction (CTJ) episodically migrated northward during the past 14 Ma from 54°S to its present‐day position at 46°30′S, as different almost trench‐parallel spreading segments entered
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