Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina
- Autores
- Gimenez, Mario Ernesto; Gómez Ortíz, David; Martinez, Myriam Patricia; Introcaso, Antonio
- Año de publicación
- 2014
- Idioma
- español castellano
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- 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.
Fil: Gimenez, Mario Ernesto. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Fisicas y Naturales. Instituto Geofisico Sismologico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico San Juan. Centro de Investigaciones de la Geosfera y Biosfera; Argentina
Fil: Gómez Ortíz, David. Universidad Rey Juan Carlos; España
Fil: Martinez, Myriam Patricia. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Fisicas y Naturales. Instituto Geofisico Sismologico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico San Juan. Centro de Investigaciones de la Geosfera y Biosfera; Argentina
Fil: Introcaso, Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Rosario. Instituto de Física de Rosario (i); Argentina - Materia
-
Cuenca de Pipanaco
Gravimetría
Modelo de Corteza
Cuenca de Antepaís Andino - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/4903
Ver los metadatos del registro completo
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Caracterización geofísica de la cuenca de Pipanaco Catamarca - ArgentinaGimenez, Mario ErnestoGómez Ortíz, DavidMartinez, Myriam PatriciaIntrocaso, AntonioCuenca de PipanacoGravimetríaModelo de CortezaCuenca de Antepaís Andinohttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This 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.Fil: Gimenez, Mario Ernesto. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Fisicas y Naturales. Instituto Geofisico Sismologico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico San Juan. Centro de Investigaciones de la Geosfera y Biosfera; ArgentinaFil: Gómez Ortíz, David. Universidad Rey Juan Carlos; EspañaFil: Martinez, Myriam Patricia. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Fisicas y Naturales. Instituto Geofisico Sismologico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico San Juan. Centro de Investigaciones de la Geosfera y Biosfera; ArgentinaFil: Introcaso, Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Rosario. Instituto de Física de Rosario (i); ArgentinaEuropean Association of Geoscientists & Engineers2014-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/4903Gimenez, Mario Ernesto; Gómez Ortíz, David; Martinez, Myriam Patricia; Introcaso, Antonio; Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina; European Association of Geoscientists & Engineers; Geociencias Aplicadas Latinoamericanas; 1; 2; 5-2014; 1-72352-0418spainfo:eu-repo/semantics/altIdentifier/url/http://geolatin.eage.org/publication/publicationdetails/?publication=76973info:eu-repo/semantics/altIdentifier/doi/info:eu-repo/semantics/altIdentifier/doi/10.3997/2352-8281.20140001info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:51:22Zoai:ri.conicet.gov.ar:11336/4903instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:51:22.49CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| title |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| spellingShingle |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina Gimenez, Mario Ernesto Cuenca de Pipanaco Gravimetría Modelo de Corteza Cuenca de Antepaís Andino |
| title_short |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| title_full |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| title_fullStr |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| title_full_unstemmed |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| title_sort |
Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina |
| dc.creator.none.fl_str_mv |
Gimenez, Mario Ernesto Gómez Ortíz, David Martinez, Myriam Patricia Introcaso, Antonio |
| author |
Gimenez, Mario Ernesto |
| author_facet |
Gimenez, Mario Ernesto Gómez Ortíz, David Martinez, Myriam Patricia Introcaso, Antonio |
| author_role |
author |
| author2 |
Gómez Ortíz, David Martinez, Myriam Patricia Introcaso, Antonio |
| author2_role |
author author author |
| dc.subject.none.fl_str_mv |
Cuenca de Pipanaco Gravimetría Modelo de Corteza Cuenca de Antepaís Andino |
| topic |
Cuenca de Pipanaco Gravimetría Modelo de Corteza Cuenca de Antepaís Andino |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
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. Fil: Gimenez, Mario Ernesto. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Fisicas y Naturales. Instituto Geofisico Sismologico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico San Juan. Centro de Investigaciones de la Geosfera y Biosfera; Argentina Fil: Gómez Ortíz, David. Universidad Rey Juan Carlos; España Fil: Martinez, Myriam Patricia. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Fisicas y Naturales. Instituto Geofisico Sismologico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico San Juan. Centro de Investigaciones de la Geosfera y Biosfera; Argentina Fil: Introcaso, Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Rosario. Instituto de Física de Rosario (i); Argentina |
| description |
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. |
| publishDate |
2014 |
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2014-05 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/4903 Gimenez, Mario Ernesto; Gómez Ortíz, David; Martinez, Myriam Patricia; Introcaso, Antonio; Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina; European Association of Geoscientists & Engineers; Geociencias Aplicadas Latinoamericanas; 1; 2; 5-2014; 1-7 2352-0418 |
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http://hdl.handle.net/11336/4903 |
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Gimenez, Mario Ernesto; Gómez Ortíz, David; Martinez, Myriam Patricia; Introcaso, Antonio; Caracterización geofísica de la cuenca de Pipanaco Catamarca - Argentina; European Association of Geoscientists & Engineers; Geociencias Aplicadas Latinoamericanas; 1; 2; 5-2014; 1-7 2352-0418 |
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European Association of Geoscientists & Engineers |
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European Association of Geoscientists & Engineers |
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