Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina
- Autores
- Ávila, J. N.; Chemale Jr., F.; Kawashita, K.; Armstrong, R.; Cingolani, Carlos Alberto
- Año de publicación
- 2003
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- The Cuyo Basin rift is located in the northwestern Mendoza Province (NW-Argentina), as part of the Argentine Precordillera. It is a Triassic basin which has a very dynamic evolution controlled by climatic and tectonic events during the geological time. Such events influenced directly the basin inception, geometry and depositional evolution, Ieading to correlation between strata in different regions to be a very difficuit task. The Cacheuta sub-basin consists in one of the most important depocenters of the Cuyo Basin, especially due to its economic potential in hydrocarbon exploration (Chebli et al., 2001). The Cuyo Basin displays a general NW-SE trend, mostly controlled by pre-existing structures (Ramos, 1992) (Fig. 1). The eastern limit of this basin coincides with an important suture generated in the Silurian through the amalgamation of the Cuyania Terrane to the southwestern margin of Gondwana. On the other hand, the western border is a structure that represents the Devonian accretion zone of the Chilenia and Cuyania terranes (Ramos & Kay, 1991).
Facultad de Ciencias Naturales y Museo - Materia
-
Ciencias Naturales
Sm-Nd isotopes
U-Pb SHRJMP
Cuyo Basin
rift-basin
provenance - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/164212
Ver los metadatos del registro completo
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Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-ArgentinaÁvila, J. N.Chemale Jr., F.Kawashita, K.Armstrong, R.Cingolani, Carlos AlbertoCiencias NaturalesSm-Nd isotopesU-Pb SHRJMPCuyo Basinrift-basinprovenanceThe Cuyo Basin rift is located in the northwestern Mendoza Province (NW-Argentina), as part of the Argentine Precordillera. It is a Triassic basin which has a very dynamic evolution controlled by climatic and tectonic events during the geological time. Such events influenced directly the basin inception, geometry and depositional evolution, Ieading to correlation between strata in different regions to be a very difficuit task. The Cacheuta sub-basin consists in one of the most important depocenters of the Cuyo Basin, especially due to its economic potential in hydrocarbon exploration (Chebli et al., 2001). The Cuyo Basin displays a general NW-SE trend, mostly controlled by pre-existing structures (Ramos, 1992) (Fig. 1). The eastern limit of this basin coincides with an important suture generated in the Silurian through the amalgamation of the Cuyania Terrane to the southwestern margin of Gondwana. On the other hand, the western border is a structure that represents the Devonian accretion zone of the Chilenia and Cuyania terranes (Ramos & Kay, 1991).Facultad de Ciencias Naturales y Museo2003info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdf147-150http://sedici.unlp.edu.ar/handle/10915/164212enginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-03T11:15:26Zoai:sedici.unlp.edu.ar:10915/164212Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-03 11:15:26.523SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
title |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
spellingShingle |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina Ávila, J. N. Ciencias Naturales Sm-Nd isotopes U-Pb SHRJMP Cuyo Basin rift-basin provenance |
title_short |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
title_full |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
title_fullStr |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
title_full_unstemmed |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
title_sort |
Sm-Nd isotopic signature and U-Pb shrimp zircon dating of the Cacheuta sub-basin, Cuyo basin, NW-Argentina |
dc.creator.none.fl_str_mv |
Ávila, J. N. Chemale Jr., F. Kawashita, K. Armstrong, R. Cingolani, Carlos Alberto |
author |
Ávila, J. N. |
author_facet |
Ávila, J. N. Chemale Jr., F. Kawashita, K. Armstrong, R. Cingolani, Carlos Alberto |
author_role |
author |
author2 |
Chemale Jr., F. Kawashita, K. Armstrong, R. Cingolani, Carlos Alberto |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales Sm-Nd isotopes U-Pb SHRJMP Cuyo Basin rift-basin provenance |
topic |
Ciencias Naturales Sm-Nd isotopes U-Pb SHRJMP Cuyo Basin rift-basin provenance |
dc.description.none.fl_txt_mv |
The Cuyo Basin rift is located in the northwestern Mendoza Province (NW-Argentina), as part of the Argentine Precordillera. It is a Triassic basin which has a very dynamic evolution controlled by climatic and tectonic events during the geological time. Such events influenced directly the basin inception, geometry and depositional evolution, Ieading to correlation between strata in different regions to be a very difficuit task. The Cacheuta sub-basin consists in one of the most important depocenters of the Cuyo Basin, especially due to its economic potential in hydrocarbon exploration (Chebli et al., 2001). The Cuyo Basin displays a general NW-SE trend, mostly controlled by pre-existing structures (Ramos, 1992) (Fig. 1). The eastern limit of this basin coincides with an important suture generated in the Silurian through the amalgamation of the Cuyania Terrane to the southwestern margin of Gondwana. On the other hand, the western border is a structure that represents the Devonian accretion zone of the Chilenia and Cuyania terranes (Ramos & Kay, 1991). Facultad de Ciencias Naturales y Museo |
description |
The Cuyo Basin rift is located in the northwestern Mendoza Province (NW-Argentina), as part of the Argentine Precordillera. It is a Triassic basin which has a very dynamic evolution controlled by climatic and tectonic events during the geological time. Such events influenced directly the basin inception, geometry and depositional evolution, Ieading to correlation between strata in different regions to be a very difficuit task. The Cacheuta sub-basin consists in one of the most important depocenters of the Cuyo Basin, especially due to its economic potential in hydrocarbon exploration (Chebli et al., 2001). The Cuyo Basin displays a general NW-SE trend, mostly controlled by pre-existing structures (Ramos, 1992) (Fig. 1). The eastern limit of this basin coincides with an important suture generated in the Silurian through the amalgamation of the Cuyania Terrane to the southwestern margin of Gondwana. On the other hand, the western border is a structure that represents the Devonian accretion zone of the Chilenia and Cuyania terranes (Ramos & Kay, 1991). |
publishDate |
2003 |
dc.date.none.fl_str_mv |
2003 |
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eng |
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eng |
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