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Neotectonic transpressive zones in the Precordillera sur, central Andes of Argentina: a structural and geophysical investigation
(E Schweizerbartsche Verlags, 2009-07)
On the flat-slab segment of the Central Andes of Argentina, the southern portion (31°30' - 33° SL) of the Precordillera is characterized by a singular Late Cenozoic tectonic style related to the tectonic inversion of ...
Fajas oblicuas de deformación neotectónica en Precordillera y Cordillera Frontal (31° 30´ - 33° 30´ LS): controles paleotectónicosOblique belts of neotectonic deformation in Precordillera and Frontal Cordillera (31 30´ - 33 30´ ls): Paleotectonic control
(Asociación Geológica Argentina, 2006-12)
The Southern Precordillera and Cerrilladas Pedemontanas of Mendoza, Argentina, are two major morphotectonic units in the eastern side of the Central Andes at 31º30' - 33º30' South latitude. There, two regional NW striking ...
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 ...
Las mineralizaciones de la zona de Carrizal, Precordillera Occidental, ArgentinaOre deposits from Carrizal area, Western Precordillera, Argentina
(Instituto Geológico y Minero, 2017-11)
El área de Carrizal se ubica en el sur de la Sierra de Volcán, Precordillera Occidental de la provincia de San Juan, Argentina. Allí se desarrolla una importante zona de alteración en rocas sedimentarias de edad carbonífera ...
La deformación tardíocenozoica en el interior del Bloque Barreal, margen suroeste de la Precordillera de San JuanThe Late-Cenozoic deformation at the interior of Barreal block, southwestern margin of Precordillera in San Juan province
(Asociación Geológica Argentina, 2004-12)
RESUMEN. Se presenta aquí información geológica orientada a evaluar el rol de la actividad tectónica cuaternaria en la construcción del bloque Barreal (31°15´ - 31 °50´ LS). Dicho bloque es una unidad morfotectónica de la ...
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 ...