Investigating the shallow to mid-depth (> 100–300 C) continental crust evolution with (U-Th)/He thermochronology: a review
Quantifying geological processes has greatly benefited from the development and use of
thermochronometric methods over the last fifty years. Among them is the (U-Th)/He dating …
thermochronometric methods over the last fifty years. Among them is the (U-Th)/He dating …
Reconstructing the South American Miocene puzzle: An integrated analysis of the Paraná Formation (Argentina)
In recent decades, Miocene marine transgressions in South America have sparked ongoing
debates concerning their boundaries, number of events, regional connectivity, and the …
debates concerning their boundaries, number of events, regional connectivity, and the …
Dating recurrent shear zone activity and the transition from ductile to brittle deformation: White mica geochronology applied to the Neoproterozoic Dom Feliciano Belt …
Argon geochronology of white mica has a good potential of recording recurrent dynamic
recrystallization in shear zones in the transition from ductile to brittle deformation, as …
recrystallization in shear zones in the transition from ductile to brittle deformation, as …
Seismic stratigraphy of the Cretaceous post-rift sedimentary interval in the Punta del Este Basin (offshore Uruguay) and its implications for deep-water reservoirs
M Sequeira, E Morales, B Conti - Petroleum Geoscience, 2024 - lyellcollection.org
The formation of the Punta del Este Basin is associated with the fragmentation of West
Gondwana and consequently the opening of the South Atlantic Ocean during the Early …
Gondwana and consequently the opening of the South Atlantic Ocean during the Early …
World-class amethyst-agate geodes from Los Catalanes, Northern Uruguay: genetic implications from fluid inclusions and stable isotopes
F Arduin-Rode, G Sosa, A van den Kerkhof… - Mineralium …, 2024 - Springer
The amethyst and agate geodes from the Los Catalanes Gemmological District in Uruguay
represent one of the main deposits of its kind worldwide. The geometry of the deposit is …
represent one of the main deposits of its kind worldwide. The geometry of the deposit is …
Contrasting thermal histories in the Dom Feliciano Belt triggered by magmatism related to the Paraná-Etendeka LIP and fracture zone proximity
E do Amaral Santos, AR Jelinek, D Stockli… - Tectonophysics, 2023 - Elsevier
The present-day southern Brazilian continental margin rests on top of the Dom Feliciano Belt
(DFB) and adjacent cratons. This belt formed through the collision of the Rio de La Plata …
(DFB) and adjacent cratons. This belt formed through the collision of the Rio de La Plata …
The Sierra de Aguirre Formation, Uruguay: Post-collisional Ediacaran volcanism in the southernmost Dom Feliciano Belt
Abstract The Sierra de Aguirre Fm. in southern Uruguay constitutes one of several post-
collisional basins of the Dom Feliciano Belt, preserving an important volcanic record …
collisional basins of the Dom Feliciano Belt, preserving an important volcanic record …
Mantle contribution to Late Paleozoic glaciations of SW Gondwana
Abstract During the Mississippian to Pennsylvanian, mountain-building processes, changes
from marine to continental sedimentary paleoenvironments, and the formation of mountain …
from marine to continental sedimentary paleoenvironments, and the formation of mountain …
Thermal history along the Araçuaí Orogen and São Francisco Craton border, eastern Brazilian continental margin, based on low-temperature thermochronologic data
E do Amaral Santos, AR Jelinek, JP Machado… - Tectonophysics, 2022 - Elsevier
Passive margins form in response to rifting affecting a continental area. Rifting evolution is
dependent on structural and rheological inheritance, generally controlling differential …
dependent on structural and rheological inheritance, generally controlling differential …
Geomorphic expression of shear zones in Southern Brazilian and Uruguayan Shields
M Cardoso Jr, AS da Silveira, MR de Vargas… - Geomorphology, 2021 - Elsevier
Earth's surface is a result of complex tectonic and erosional processes shaping landscapes
and producing transient signs of different evolutionary stages. These transient signs are …
and producing transient signs of different evolutionary stages. These transient signs are …