Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina

This work is focused on the Pipanaco basin area, which straddles two provinces: Catamarca and La Rioja (Argentina), and is located within the Sierras Pampeanas mountain range. The region features a tectonic depression bound by inverse faults (except its southern border). Existing gravimetric and geo...

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Detalles Bibliográficos
Autores: Gimenez, Mario Ernesto, Gómez Ortíz, David, Martinez, Myriam Patricia, Introcaso, Antonio
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2014
País:Argentina
Institución:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:español
OAI Identifier:oai:ri.conicet.gov.ar:11336/4903
Acceso en línea:http://hdl.handle.net/11336/4903
Access Level:acceso abierto
Palabra clave:Cuenca de Pipanaco
Gravimetría
Modelo de Corteza
Cuenca de Antepaís Andino
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Descripción
Sumario:This work is focused on the Pipanaco basin area, which straddles two provinces: Catamarca and La Rioja (Argentina), and is located within the Sierras Pampeanas mountain range. The region features a tectonic depression bound by inverse faults (except its southern border). Existing gravimetric and geological information have been combined with new gravity data to model crustal features beneath the basin.Gravity anomaly maps were prepared using land gravity stations. Crustal-related anomalies were enhanced following a residualization process in order to identify density inhomogeneities located in the upper crust, which is the main focus of this study. Then, 2-D and 3-D density models of the upper crust were prepared from the residual Bouguer anomaly. The density of these models reveals that the sedimentary basin reaches a maximum depth of 3km of Neogene age sediments. Moreover, nonoutcropping, highdensity bodies were also identified, whose origin would go back to the evolutionary stage of the central Andes, and originated in a rifting process during the early Carboniferous.