A geodynamic model linking Cretaceous orogeny, arc migration, foreland dynamic subsidence and marine ingression in southern South America
This study synthesizes the tectonomagmatic evolution of the Andes between 35° 30′ S to
48° S with the aim to spotlight early contractional phases on Andean orogenic building and …
48° S with the aim to spotlight early contractional phases on Andean orogenic building and …
Thermochronological evidence for Eocene deformation in the southern Patagonian Andes: Linking orogenesis along the Patagonian orocline
AL Stevens Goddard, JC Fosdick, M Calderón… - …, 2023 - Wiley Online Library
Thermochronologic results from zircon fission track and (U‐Th)/He data collected across the
Patagonian batholith, basement and thrust belt of the southern Patagonian Andes between …
Patagonian batholith, basement and thrust belt of the southern Patagonian Andes between …
Mechanisms of subsidence and uplift of Southern Patagonia and offshore basins during slab window formation
Subduction of bathymetric anomalies (eg, an active ridge) can alter the morphology of
subducted slabs and their coupling to surface processes. A natural laboratory to study these …
subducted slabs and their coupling to surface processes. A natural laboratory to study these …
Lithospheric thinning and dynamic uplift effects during slab window formation, southern Patagonia (45-55 S)
Abstract The southernmost South America has been affected by the subduction of an
oceanic seismic ridge, which began to subduct below southern Patagonia at∼ 14 Ma. This …
oceanic seismic ridge, which began to subduct below southern Patagonia at∼ 14 Ma. This …
Early Cretaceous to Cenozoic growth of the Patagonian Andes as revealed by low‐temperature thermochronology
Abstract The Southern Patagonian Andes at the latitude of the Chile Triple junction in
Argentina and Chile (46°–47.5° S) are the object of an ongoing discussion regarding their …
Argentina and Chile (46°–47.5° S) are the object of an ongoing discussion regarding their …
Heat flow and lithospheric thickness analysis in the Patagonian asthenospheric windows, southern South America
The lithosphere–asthenosphere boundary (LAB) is a first-order discontinuity, essential to
understand the Earth composition and evolution. However, its detection has been critical …
understand the Earth composition and evolution. However, its detection has been critical …
Mesozoic–Cenozoic evolution of the southern Patagonian Andes fold and thrust belt (47°–48° S): Influence of the Rocas Verdes basin inversion and onset of …
Abstract The Southern Patagonian Andes (SPA) between 47°–48° S are characterized by
relatively high elevations (1500–4000 m) and a 200-km-wide, largely exhumed, basement …
relatively high elevations (1500–4000 m) and a 200-km-wide, largely exhumed, basement …
Cenozoic subsidence‐driving mechanisms in the southernmost Patagonian basins of Tierra del Fuego and SW Atlantic
Foreland basins are ideal laboratories to examine and quantify forces that contribute to
Earth's topography. The interaction of these driving mechanisms (atmospheric, lithospheric …
Earth's topography. The interaction of these driving mechanisms (atmospheric, lithospheric …
Maastrichtian-Danian Northpatagonian rocky shore, Argentina
N Foix, SM Ocampo, JM Paredes, JO Allard… - Sedimentary …, 2023 - Elsevier
Abstract The Atlantic Maastrichtian-Danian (K/P) transgression over northern-central extra-
Andean Patagonia (Argentina) covered both Mesozoic sedimentary basins and the …
Andean Patagonia (Argentina) covered both Mesozoic sedimentary basins and the …
Relative contributions of tectonics and dynamic topography to the Mesozoic-Cenozoic subsidence of southern Patagonia
Sedimentary basins result from a complex interaction between mantle, crustal and surficial
erosional-driven processes, which act at different time and spatial scales. While shortening …
erosional-driven processes, which act at different time and spatial scales. While shortening …