First radiometric age of Cretaceous deposits of the Central Precordillera
Ciénaga del Río Huaco Formation was deposited during the Cretaceous in the Precordillera Central (La Rioja and San Juan provinces). The unit forms part of a thick red-bed sequence including rocks of different ages (from Late Paleozoic to Tertiary) and problematic identification. In the La Troya rive...
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I28-R145-paper_00044822_v62_n3_p471_Tedesco_oai2024-08-16 Tedesco, A.M. Limarino, C.O. Ciccioli, P.L. 2007 Ciénaga del Río Huaco Formation was deposited during the Cretaceous in the Precordillera Central (La Rioja and San Juan provinces). The unit forms part of a thick red-bed sequence including rocks of different ages (from Late Paleozoic to Tertiary) and problematic identification. In the La Troya river area, the red bed sequence is composed of the Panacán (Permian), Santo Domingo (Late Triassic- Early Jurassic), Ciénaga del Río Huaco (Cretaceous) and Puesto La Flecha Formations (Oligocene- Early Nfiocene). In the past, all these formations were included in the same stratigrapbic unit and only in recent years the different formations could be separated mainly based on their fossil contain. In the case of Ciénaga del Rio Huaco Formation, the finding of microfossils (palynomorphs and ostracods) allowed to infer a Late Cretaceous age for these rocks. However, a radiometric age of 108,1 ± 4,4 Ma presented in this paper, clearly suggest that the unit was deposited at the end of the Early Cretaceous. This age is the first Cretaceous absolute age in the Precordillera Central and enhances the time constraints of of the Cretaceous Basin. Fil:Tedesco, A.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Limarino, C.O. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Ciccioli, P.L. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. application/pdf http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p471_Tedesco info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Rev. Asoc. Geol. Argent. 2007;62(3):471-474 Ciénaga Huaco La Rioja Mesozoic Cretaceous formation mechanism geochronology palynomorph radiometric method red bed sediment thickness sedimentary sequence Argentina La Rioja [Argentina] Precordillera San Juan [Argentina] South America Ostracoda First radiometric age of Cretaceous deposits of the Central Precordillera info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v62_n3_p471_Tedesco_oai |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-145 |
collection |
Repositorio Digital de la Universidad de Buenos Aires (UBA) |
topic |
Ciénaga Huaco La Rioja Mesozoic Cretaceous formation mechanism geochronology palynomorph radiometric method red bed sediment thickness sedimentary sequence Argentina La Rioja [Argentina] Precordillera San Juan [Argentina] South America Ostracoda |
spellingShingle |
Ciénaga Huaco La Rioja Mesozoic Cretaceous formation mechanism geochronology palynomorph radiometric method red bed sediment thickness sedimentary sequence Argentina La Rioja [Argentina] Precordillera San Juan [Argentina] South America Ostracoda Tedesco, A.M. Limarino, C.O. Ciccioli, P.L. First radiometric age of Cretaceous deposits of the Central Precordillera |
topic_facet |
Ciénaga Huaco La Rioja Mesozoic Cretaceous formation mechanism geochronology palynomorph radiometric method red bed sediment thickness sedimentary sequence Argentina La Rioja [Argentina] Precordillera San Juan [Argentina] South America Ostracoda |
description |
Ciénaga del Río Huaco Formation was deposited during the Cretaceous in the Precordillera Central (La Rioja and San Juan provinces). The unit forms part of a thick red-bed sequence including rocks of different ages (from Late Paleozoic to Tertiary) and problematic identification. In the La Troya river area, the red bed sequence is composed of the Panacán (Permian), Santo Domingo (Late Triassic- Early Jurassic), Ciénaga del Río Huaco (Cretaceous) and Puesto La Flecha Formations (Oligocene- Early Nfiocene). In the past, all these formations were included in the same stratigrapbic unit and only in recent years the different formations could be separated mainly based on their fossil contain. In the case of Ciénaga del Rio Huaco Formation, the finding of microfossils (palynomorphs and ostracods) allowed to infer a Late Cretaceous age for these rocks. However, a radiometric age of 108,1 ± 4,4 Ma presented in this paper, clearly suggest that the unit was deposited at the end of the Early Cretaceous. This age is the first Cretaceous absolute age in the Precordillera Central and enhances the time constraints of of the Cretaceous Basin. |
format |
Artículo Artículo publishedVersion |
author |
Tedesco, A.M. Limarino, C.O. Ciccioli, P.L. |
author_facet |
Tedesco, A.M. Limarino, C.O. Ciccioli, P.L. |
author_sort |
Tedesco, A.M. |
title |
First radiometric age of Cretaceous deposits of the Central Precordillera |
title_short |
First radiometric age of Cretaceous deposits of the Central Precordillera |
title_full |
First radiometric age of Cretaceous deposits of the Central Precordillera |
title_fullStr |
First radiometric age of Cretaceous deposits of the Central Precordillera |
title_full_unstemmed |
First radiometric age of Cretaceous deposits of the Central Precordillera |
title_sort |
first radiometric age of cretaceous deposits of the central precordillera |
publishDate |
2007 |
url |
http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p471_Tedesco https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v62_n3_p471_Tedesco_oai |
work_keys_str_mv |
AT tedescoam firstradiometricageofcretaceousdepositsofthecentralprecordillera AT limarinoco firstradiometricageofcretaceousdepositsofthecentralprecordillera AT cicciolipl firstradiometricageofcretaceousdepositsofthecentralprecordillera |
_version_ |
1809356763425669120 |