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The Choiyoi volcanic province at 34°S-36°S (San Rafael, Mendoza, Argentina): Implications for the Late Palaeozoic evolution of the southwestern margin of Gondwana
(Elsevier Science, 2009-08)
The Choiyoi rhyolitic province of Chile and Argentina (23°S-42°S) was emplaced at the SW margin of Gondwana during the Permian. The San Rafael Massif (Mendoza, Argentina, 34°-36°S), is a key area to analyse the relative ...
Stratigraphy, structure and geodynamic evolution of the Paleozoic rocks in the Cordillera del Viento (37º S latitude, Andes of Neuquén, Argentina)
(Servicio Publicaciones, 2014-06-25)
The Pre-Andean Paleozoic substrate from the Cordillera del Viento anticline is a polyorogenic basement composed of two groups of preorogenic rocks with different stratigraphy and deformation. The oldest set consists of ...
Plume overriding triggers shallow subduction and orogeny in the southern Central Andes
(Elsevier Science, 2017-09)
Plate tectonic theory implies that mantle plumes may be eventually overridden by lithosphere during continental drift. These events have particular tectonomagmatic consequences for active margins and hence related orogenic ...
Palaeomagnetism of the Upper Carboniferous-Lower Permian transition from Paganzo basin, Argentina
(Wiley Blackwell Publishing, Inc, 2004-06)
A palaeomagnetic study of Upper Palaeozoic rocks was performed on Paganzo basin, central-western Argentina and its western extension, Río Blanco subbasin. The volcanic-volcaniclastic Rio del Peñón and marine sedimentary ...
Strain fabric analysis applied to hydrothermal ore deposits emplaced during changing geodynamical conditions (Infiernillo and Las Picazas, San Rafael Massif, Argentina)
(Elsevier Science, 2013-09)
Infiernillo and Las Picazas are two small hydrothermal ore deposits in the northern San Rafael Massif (Argentina). They are genetically linked to the Permian Choiyoi volcanic province which reflects the transition from a ...
Reactivation of Paleozoic structures during Cenozoic deformation in the Cordón del Plata and Southern Precordillera ranges (Mendoza, Argentina)
(Universidad Complutense de Madrid, 2014-06)
The tectonic style of the eastern morphostructural units of the Central Andes between 32°20´ and 33°20´S is strongly influenced by pre-Andean structures, especially those developed during the late Carboniferous-Early Permian ...
Reactivation of Late Paleozoic structures during the Cenozoic deformation in the Cordón del Plata range and Southern Precordillera (Mendoza, Argentina)
(Universidad Complutense de Madrid, 2014-04)
The tectonic style of the eastern morphostructural units of the Central Andes between 32°20´ and 33°20´S is strongly influenced by pre-Andean structures, especially those developed during the Early Permian San Rafael ...
Geological and geophysical evidences of the polyphase structural evolution of the Southern Precordillera (31°42′S-69°24′W), central-western Argentina
(Pergamon-Elsevier Science Ltd, 2018-11)
The evolution of the western margin of South America comprised different tectonic regimes responsible of the present geological composition and structure of the Central Andes. Remote sensing, geological and geophysical ...
Análisis tectonoestratigráfico del Grupo Puesto Viejo (San Rafael, Argentina): evolución de un rift continental triásicoTectonostratigraphic analysis of the Puesto Viejo Group (San Rafael, Argentina): evolution of a Triassic continental rift
(Asociación Argentina de Sedimentología, 2016-11)
La cuenca triásica que alberga al Grupo Puesto Viejo se localiza en el Bloque San Rafael, al oeste de las principales acumulaciones de esa edad del ámbito cuyano. Este depocentro elongado con geometría de graben limitado ...