Crustal anatomy and evolution of a subduction-related orogenic system: Insights from the Southern Central Andes (22-35 S)
As the archetype of mountain building in subduction zones, the Central Andes has
constituted an excellent example for investigating mountain-building processes for decades …
constituted an excellent example for investigating mountain-building processes for decades …
[HTML][HTML] Broken foreland basins and the influence of subduction dynamics, tectonic inheritance, and mechanical triggers
Broken foreland basins are caused by crustal-scale contractional basement structures that
compartmentalize (or break) a contiguous retroarc or collisional foreland basin into smaller …
compartmentalize (or break) a contiguous retroarc or collisional foreland basin into smaller …
Kinematic analysis of the mesozoic-Early Cenozoic deformation in the paipote basin (27° 10′ S)
M Peña, R Quiroga, G Fuentes, M Arellano… - Journal of South …, 2023 - Elsevier
An integrated structural and kinematic study focused on the characterization of an Andean
Mesozoic basin was carried out in the upper stream of the Paipote Creek, in the western limit …
Mesozoic basin was carried out in the upper stream of the Paipote Creek, in the western limit …
Paipote fold-and-thrust belt, a key element in understanding the upper crustal shortening mechanisms of the Central Andean forearc
The crustal shortening of the Andean forearc in northern Chile was accommodated by a
combination of both thin-and thick-sinned structural styles. However, fold-related inversion of …
combination of both thin-and thick-sinned structural styles. However, fold-related inversion of …
Boundary effects of orogenic plateaus in the evolution of the stress field: The southern Puna study case (26 30′–27 30′ S)
R Quiroga, L Giambiagi, A Echaurren, J Mescua… - …, 2024 - Wiley Online Library
We present a study in the southern Puna (26° 30′–27° 30′ S), aiming to explore the late
Cenozoic evolution of the deformation and the stress field during its uplift. Through U‐Pb …
Cenozoic evolution of the deformation and the stress field during its uplift. Through U‐Pb …
U–Pb ages and paleoenvironmental evolution of the guanchín formation (neogene fiambalá foreland basin), Central Andes, Argentina
Abstract The Guanchín Formation is a sedimentary unit that was deposited during the
Andean orogeny and is preserved in the Fiambalá Basin in NW Argentina. It records an …
Andean orogeny and is preserved in the Fiambalá Basin in NW Argentina. It records an …
[PDF][PDF] DECIPHERING THE ORIGIN OF LINEAR LANDFORMS USING DIFFERENT SEDIMENTOLOGICAL TOOLS IN THE FIAMBALÁ VALLEY (CATAMARCA)
DF Molina, PL Ciccioli, LD Serpa, PA Silvero - researchgate.net
The current study is centered on the morphological, textural, and compositional
characterization of several linear landforms identified in the west and center of the Fiambalá …
characterization of several linear landforms identified in the west and center of the Fiambalá …
New advances in paleomagnetic and magnetic fabric studies in Latin America: An introduction
AE Rapalini, F Poblete, CC Miranda… - Journal of South American …, 2021 - Elsevier
Abstract The Special Issue on Paleomagnetism and Magnetic Fabrics in Latin America
contains twenty-one original contributions ranging from Paleogeography and Tectonics to …
contains twenty-one original contributions ranging from Paleogeography and Tectonics to …