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Successive reactivation of older structures under variable heat flow conditions evidenced by K-Ar fault gouge dating in Sierra de Ambato, northern Argentine broken foreland
(Pergamon-Elsevier Science Ltd, 2015-12)
The Argentine broken foreland has been the subject of continuous research to determine the uplift and exhumation history of the region. High-elevation mountains are the result of N-S reverse faults that disrupted a W-E ...
Tectonic vs. climate controls on the evolution of a miocene intermontane basin, Patagonian Andean foreland, Argentina
(Springer, 2021-07)
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 intermontane basins. The role ...
Tectonic development of the North Patagonian Andes and their related Miocene foreland basin (41°30'-43°S)
(American Geophysical Union, 2012-06)
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 Oligocene in the Precordilleran ...
Using sandstone and conglomerate petrofacies to unravel multiple provenance areas in broken-foreland basins: The vinchina formation (Miocene, NW Argentina) as a study case
(Pergamon-Elsevier Science Ltd, 2020-06)
The Vinchina Formation is a very thick succession (up to 6400 m-thick) of red-beds deposited in fluvial, fluvio-eolian, eolian, and lacustrine environments. This unit constitutes part of the Miocene sedimentary record of ...
Miocene block uplift and basin formation in the Patagonian foreland: The Gastre Basin, Argentina
(Elsevier Science, 2013)
Cretaceous-Cenozoic growth of the Patagonian broken foreland basin, Argentina: Chronostratigraphic framework and provenance variations during transitions in Andean subduction dynamics
(Pergamon-Elsevier Science Ltd, 2020-01)
The Cretaceous-Cenozoic evolution of the Patagonian broken foreland basin system at 42–43°S in the northern Chubut province of Argentina is associated with variable retroarc phases of fold-thrust belt shortening, extension, ...
Comment on "Dynamic topography in South America" by Federico M. Dávila & Carolina Lithgow-Bertelloni
(Elsevier, 2014-02)
In their article Dávila and Lithgow-Bertelloni (2013) propose that the Andes have been isostatically uncompensated throughout the Cenozoic and that additional forces induced by mantle flow were required to explain the ...
U-PB geochronology and magnetostratigraphy of a north Patagonian syn-orogenic Miocene succession: Tectono-stratigraphic implications for the foreland system configuration
(Elsevier Science, 2019-09)
The syn-orogenic Miocene deposits of the Patagonian Foreland System were the focus of numerous works in the latest years, due to their central role in the comprehension of the tectono-stratigraphy and tectonic evolution ...