Results 1 to 10 of about 1,863,720 (234)

Waveform inversion and focal mechanisms of two weak earthquakes in Cordillera Principal (Argentina) between 35° and 35.5° S [PDF]

open access: yesJournal of South American Earth Sciences, 2016
Abstract Only few (six) focal mechanism, in CMT Catalog, have been so far known for intraplate shallow events in the Andean chain close to Chile–Argentina state border at latitudes ∼35° S. We add two more mechanisms, depths and moment magnitudes by carefully analyzing full waveforms of weak events recorded by broad-band stations of the Chile ...
Villegas Alvarez, Raquel Judith   +5 more
semanticscholar   +5 more sources

Deformación compresiva cuaternaria en la Cordillera Principal de Chile central (Cajón del Maipo, este de Santiago) [PDF]

open access: yesRevista geológica de Chile, 2008
RESUMEN:El estudio geologico y estructural detallado de sedimentos recientes en el valle del rio Maipo (Cajon del Maipo), al este de Santiago, muestra la existencia de una deformacion en compresion con fallas inversas y pliegues de arrastre contemporaneos.
Lavenu, Alain, Cembrano, José
openaire   +3 more sources

El Cenozoico del alto río Teno, Cordillera Principal, Chile central: estratigrafía, plutonismo y su relación con estructuras profundas [PDF]

open access: yesAndean geology, 2010
The Cenozoic of the upper Teno River, Cordillera Principal, Central Chile: stratigraphy, plutonism and their relation with deep structures. The Cenozoic geologic evolution of the central part of the Cordillera Principal at ~35°S, is intimately related to the geodynamic evolution of deep crustal structures, which during different stages con- trolled the
Piquer, José   +3 more
openaire   +4 more sources

Extensional stresses in the Colombian Eastern Cordillera fold-and-thrust belt (northern Andes): insights from 2D finite element modeling [PDF]

open access: yesGeologica Acta, 2009
Deformation and stress characteristics in the upper crust of the fold-and-thrust belt in the Colombian Eastern Cordillera were investigated by numerical analysis.
R. ISLAM, D. HAYASHI
doaj   +6 more sources

Nuevos antecedentes estratigráficos y geocronológicos para el Meso-Cenozoico de la Cordillera Principal de Chile entre 32° y 32°30’S: Implicancias estructurales y paleogeográficas [PDF]

open access: yesAndean Geology, 2014
New stratigraphical and geochronological constraints for the Mezo-Cenozoic deposits in the High Andes of central Chile between 32° and 32°30’S: Structural and palaeogeographic implications. Attempts to differentiate geological units of the Andean Principal Cordillera, between 31°30’S and 33°S, faced several problems until very recently.
Jara, Pamela, Charrier, Reynaldo
openaire   +4 more sources

Geomorphologic and Glacial Evolution of the Cachapoal and southern Maipo catchments in the Andean Principal Cordillera, Central Chile (34°-35º S)

open access: yesAndean Geology, 2019
We present here a reconstruction of the post late Miocene landscape evolution of the western slope of the Andean Cordillera Principal near 34°20’ S. We base our analysis on the available geological information, a morphological characterization of the landform assemblages in the Cachapoal and southern Maipo catchments, and the first 10Be exposure ages ...
Charrier, Reynaldo   +3 more
openaire   +5 more sources

Fission track thermochronology of Neogene plutons in the Principal Andean Cordillera of central Chile (33-35°S): Implications for tectonic evolution and porphyry Cu-Mo mineralization [PDF]

open access: yesAndean geology, 2009
Apatite fission track data for Miocene plutons of the western slope of the Principal Andean Cordillera in central Chile (33-35°S) define a distinct episode of enhanced crustal cooling through the temperature range of the apatite partial annealing zone (~125-60°C) from about 6 to 3 Ma.
Maksaev, Víctor   +3 more
semanticscholar   +5 more sources

Magnetic fabric of deformed Quaternary sediments: contributions to the understanding of the neotectonic activity in the surroundings of the Aburrá Valley, Central Cordillera, Colombia

open access: yesBoletín Geológico, 2022
The origin of the Aburrá Valley (AV) is proposed as a set of coalescent tectonic subbasins located along the northern  portion of the Central Cordillera of Colombia, the Northern  Andes of Colombia.
Santiago Noriega Londoño   +4 more
doaj   +2 more sources

Glacial geomorphology of the Marinelli and Pigafetta glaciers, Cordillera Darwin Icefield, southernmost Chile

open access: yesJournal of Maps, 2018
This paper presents a glacial geomorphological map relating to two rapidly receding glaciers in the Cordillera Darwin Icefield. The Marinelli marine-terminating glacier and Pigafetta freshwater-terminating glacier are selected to represent different ...
Eñaut Izagirre   +3 more
doaj   +2 more sources

Las eolianitas de la Formación Agua de la Piedra (Mioceno Tardío), Cordillera principal (Provincia de Mendoza, Argentina)

open access: yesLatin American Journal of Sedimentology and Basin Analysis, 2006
Se analiza la sedimentología y la arquitectura depositacional de las secuencias aflorantes en las localidades de La Jaula y Agua del Médano, Provincia de Mendoza con el objetivo de dar a conocer la presencia de médanos pedemontanas, pertenecientes a la ...
Ana M. Combina
doaj   +4 more sources

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