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Groundwater resources and recharge processes in the western andean front of central Chile
(Elsevier, 2020)
In Central Chile, the increment of withdrawals together with drought conditions has exposed the poor understanding of the regional hydrogeological system. In this study, we addressed theWestern Andean Front hydrogeology ...
Groundwater resources and recharge processes in the Western Andean Front of Central Chile
(ELSEVIER, 2020)
In Central Chile, the increment of withdrawals together with drought conditions has exposed the poor understanding of the regional hydrogeological system. In this study, we addressed theWestern Andean Front hydrogeology ...
Holocene shortening rates of an Andean-front thrust, Southern Precordillera, Argentina
(Elsevier, 2015-09)
A significant part of the Quaternary shortening between the Chilean trench and the relative stable interior of the South American plate at the Pampean flat slab (27–33°S), has been accommodated at the eastern foothills of ...
Abanico east formation: petrology and geochemistry of volcanic rocks behind the cenozoic arc front in the andean cordillera, central chile (33 degrees 50 s)
(SERVICIO NACIONAL DE GEOLOGIA Y MINERIA, 2006)
Distribution of landslides along the Andean active orogenic front (Argentinean Precordillera 31–33° S)
(Elsevier Ltd, 2019)
As one of the main environmental effects of earthquakes, the distribution of landslides could reflect regional neotectonic activity. To that end, we carried out an inventory of landslides along the Precordillera range ...
Quaternary shortening at the orogenic front of the Central Andes of Argentina: the Las Peñas Thrust System
(Lyell Collection, 2014-06)
The NNW-trending Las Peñas Thrust System is one of the key structures along the Andean orogenic front between 32°15′ and 32°40′S in the Southern Precordillera of Argentina. This east-verging structure crops out over a ...
Andean evolution at the Guañacos and Chos Malal fold and thrust belts (36°30′-37°s)
(Pergamon-Elsevier Science Ltd, 2007-10)
The Andes between 36°30′ and 37°S represent a Cretaceous fold and thrust belt strongly reactivated in the late Miocene. Most of the features that absorbed Neogene shortening were already uplifted in the late Cretaceous, ...
Huge slope collapses flashing the andean active orogenic front (argentinean precordillera 31-33°s)
(Springer, 2017)
The study area is located along the Andean active orogenic front comprising the mostseismically active region of Argentina. Main Quaternary deformation is concentrated in thisWestern central part of the country associated ...
Groundwater resources of the Western Andean Front: insights from the Aconcagua Basin, Central Chile
(Universidad de Chile, 2020)
The misunderstanding of hydrogeological processes together with the oversimplification of aquifer conceptual models result in numerous inaccuracies in the management of groundwater resources. Despite that Chile is a ...
Crustal wedging triggering recent deformation in the Andean thrust front between 31°S and 33°S: Sierras Pampeanas-Precordillera interaction
(American Geophysical Union, 2007-03)
We document a new model of crustal structure of the Andean front in Argentina where numerous historic earthquakes destroyed the cities of Mendoza in 1861 (Ms = ∼7) and San Juan in 1944 (Mw = 7.0). The Cerro Salinas anticline ...