A review about the quaternary upper-plate deformation in the Southern Central Andes (36–38° S): A plausible interaction between mantle dynamics and tectonics

L Sagripanti, B Colavitto, L Jagoe, F Andrés… - Journal of South …, 2018 - Elsevier
Quaternary deformation in the Southern Central Andes between 36° and 38° S is
disconnected, noncontinuous and not particularly tracing the main mountain topographic …

Reviewing the geodynamic impact of aseismic ridges subduction on the tectonic-magmatic evolution of the Southern Puna plateau

W Báez, E Bustos, A Chiodi, HPA García… - Journal of South …, 2023 - Elsevier
Abstract The Southern Puna (∼ 24° S to 27° S) is an outstanding segment of the Central
Andes where the subduction of aseismic ridges, multi-scale lithospheric foundering, and the …

The Cara Cura intrusive complex, Neuquén Basin, Argentina: a field analogue of a whole igneous petroleum system

JO Palma, O Rabbel, JB Spacapan… - Geological Society …, 2024 - lyellcollection.org
This contribution presents a detailed geological study of a well-exposed igneous petroleum
system at Sierra de Cara Cura, Neuquén Basin, Argentina, which consists of sills, dykes …

Transcontinental retroarc sediment routing controlled by subduction geometry and climate change (Central and Southern Andes, Argentina)

E Garzanti, T Capaldi, G Vezzoli, M Limonta, N Sosa - Basin Research, 2021 - earthdoc.org
Abstract Central Argentina from the Pampean flat‐slab segment to northern Patagonia (27°–
41° S) represents a classic example of a broken retroarc basin with strong tectonic and …

[PDF][PDF] Alternating contraction and extension in the Southern Central Andes (35°–37° S)

LM Fennell, SB Iannelli, A Encinas… - American Journal of …, 2019 - ajsonline.org
The Andes are thought to be formed through discrete contractional stages separated by
periods of little to no orogenic construction. This paper analyzes the intervals between the …

Evolution of Eocene to Oligocene arc-related volcanism in the North Patagonian Andes (39–41 S), prior to the break-up of the Farallon plate

SB Iannelli, VD Litvak, LF Paz, A Folguera, ME Ramos… - Tectonophysics, 2017 - Elsevier
Voluminous Paleogene magmatic rocks (44 to 29 Ma) are found in a retroarc position in the
Northern Patagonian to Southern Central Andes (~ 39–42° S), whose origin remains …

[HTML][HTML] 3-dimensional trapdoor structure of laccolith-induced doming and implications for laccolith emplacement, Pampa Amarilla, Mendoza Province, Argentina

O Galland, H de la Cal, J Mescua, O Rabbel - Tectonophysics, 2022 - Elsevier
Laccolith emplacement and growth are controlled by doming of overburden rocks.
Understanding the mechanics and structural evolution of laccolith-induced doming is …

Geochemical and tectonic evolution of Late Cretaceous to early Paleocene magmatism along the Southern Central Andes (35-36° S)

SB Iannelli, LM Fennell, VD Litvak, LF Paz… - Journal of South …, 2018 - Elsevier
Abstract Late Cretaceous-early Paleocene magmatism at Southern Central Andes is
represented by incomplete and not well-preserved outcrops. A recent U-Pb age from a …

Plume overriding triggers shallow subduction and orogeny in the southern Central Andes

GM Gianni, HPA García, M Lupari, A Pesce… - Gondwana …, 2017 - Elsevier
Plate tectonic theory implies that mantle plumes may be eventually overridden by
lithosphere during continental drift. These events have particular tectonomagmatic …

[HTML][HTML] Triassic to Neogene evolution of the south-central Andean arc determined by detrital zircon U-Pb and Hf analysis of Neuquén Basin strata, central Argentina …

EA Balgord - Lithosphere, 2017 - pubs.geoscienceworld.org
Abstract The Andes Mountains provide an ideal natural laboratory to analyze the
relationship between the tectonic evolution of a subduction margin, basin morphology, and …