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Miocene to Recent collapse calderas of the southern and central volcanic zones of the Andes and their tectonic constraints
(Springer, 2021-01-30)
Central (18–28° S) and Southern (33–46° S) Andean Volcanic Zones (CVZ and SVZ, respectively) have several Miocene to Recent collapse calderas. We compare their characteristics based on published data to identify how the ...
Tectono-depositional correlation between the Brazilian continental margin and the Rio Grande RiseCorrelação tectono-deposicional entre a margem continental brasileira e a Elevação do Rio Grande
(Universidade de São Paulo, Instituto de Geociências, 2020)
Tectono-sequence stratigraphy and U–Pb zircon ages of the Rincón Blanco Depocenter, northern Cuyo Rift, Argentina
(Elsevier Science, 2012-03)
Extensional processes that followed the Gondwanan Orogeny rise to the development of a series of rift basins along the continental margin over older accreted Eopaleozoic terranes. Stratigraphic, structural, paleontological, ...
New insights of the tectonic and sedimentary evolution of the Rio Grande Rise, South Atlantic Ocean
(2019-12-01)
Oceanic plateaus, such as the Rio Grande Rise (RGR), comprise crucial pieces of information about the opening of the South Atlantic Ocean and the evolution of associated lithospheric plate margins. A detailed seismostratigraphic ...
PETROLOGY AND TECTONO-MAGMATIC ENVIRONMENT OF THE VOLCANIC ROCKS OF SOUTH MARZAN ABAD, CENTRAL ALBORZ MOUNTAINPETROLOGY AND TECTONO-MAGMATIC ENVIRONMENT OF THE VOLCANIC ROCKS OF SOUTH MARZAN ABAD, CENTRAL ALBORZ MOUNTAIN
(Universidade Federal de Mato Grosso - UFMT Araguaia, 2020)
Dilatation and shearing in tectono-volcanic systems from poro-elasto-plastic models set in the Southern Andes Volcanic Zone context, inferences on geofluid flow
(2022)
Geothermal fields near volcanic complexes and active crustal-scale fault zones require an understanding of the mechanical interactions that control variations in pore fluid pressure at a crustal scale. Crustal faults can ...
The syn-rift of the Neuquén Basin (Precuyano and Lower Cuyano Cycle): Review of structure, volcanism, tectono-stratigraphy and depositional scenarios
(Springer, 2020)
The Neuquén Basin is constituted by a system of NW-SE rift clusters formed during the Late Triassic–Early Jurassic at the western margin of Gondwana. The rifting is the result of an extensional tectonic regime triggered ...