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Cenozoic tectonostratigraphic evolution and architecture of the Central Andes in northern Chile based on the Aquine region, Western Cordillera (19°-19º30’ S)

Abstract: ABSTRACT. Crustal thickening by horizontal shortening and associated deformation have been broadly considered as prime mechanisms for mountain building in the Central Andes of western South America. However, timing and structural style of Andean orogeny in no

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Arenigian tholeiitic basalts in the Famatina Ordovician basin, northwestern Argentina: emplacement conditions and their tectonic significance

Abstract: ABSTRACT. This study is focused on the analysis of volcanic deposits that crop out at the middle portion of the Las Planchadas range, northern part of the Famatina System in Argentina. These volcanic rocks are records of an Ordovician effusive basaltic volcan

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Geochemistry of Permian to Triassic igneous rocks from northern Chile (28º-30º15’S): Implications on the dynamics of the proto-Andean margin

Abstract: Permian to Triassic igneous rocks cropping out in the Coastal and Frontal cordilleras in northern Chile between 28º00’S and 30º15’S have long been interpreted to represent products of magmatism related to an extensional tectonic setting, either as the result

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Outlining the thermal posdepositional evolution of the Ordovician successions of northwestern Argentina by clay mineral analysis, chlorite geothermometry and Kübler index

Abstract: ABSTRACT. The thermal post-depositional evolution of metapelitic and metavolcanic rocks of the upper Cambrian- Ordovician succession in the Central Andes of northwestern Argentina, was estimated through X ray diffraction of clay mineral analysis, Kübler Index

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Hallazgo del primer seep fósil en la costa emergida de Chile central (33°56’ S). Caracterización e implicancias

Resumen: RESUMEN. Se describen las características determinativas del primer seep de hidrocarburo fósil, identificado en la costa emergida de Chile central, preservado en la playa de la localidad de Navidad. El paleoseep de Navidad (PSN) corresponde a una acumulación

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