High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications
The classical marine Patagoniense succession at Lago Argentino, southwestern Patagonia (Argentina), known as Estancia 25 de Mayo Formation, was dated by radiometric U-Pb on zircon grains from pyroclastic rocks and 87Sr/ 86Sr ratio on calcitic oyster shells. U-Pb data yielded an age of 19.14 Ma for t...
Autores principales: | , |
---|---|
Publicado: |
2012
|
Materias: | |
Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v38_n_p110_Cuitino http://hdl.handle.net/20.500.12110/paper_08959811_v38_n_p110_Cuitino |
Aporte de: |
id |
paper:paper_08959811_v38_n_p110_Cuitino |
---|---|
record_format |
dspace |
spelling |
paper:paper_08959811_v38_n_p110_Cuitino2023-06-08T15:48:38Z High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications Cuitiño, José Ignacio Scasso, Roberto Adrian Argentina Austral basin Geochronology Miocene Patagonia Sr stratigraphy Transgression U-Pb ages chemostratigraphy chronostratigraphy geochronology isotopic analysis Miocene resolution strontium isotope transgression uranium-lead dating Patagonia Ostreidae The classical marine Patagoniense succession at Lago Argentino, southwestern Patagonia (Argentina), known as Estancia 25 de Mayo Formation, was dated by radiometric U-Pb on zircon grains from pyroclastic rocks and 87Sr/ 86Sr ratio on calcitic oyster shells. U-Pb data yielded an age of 19.14 Ma for the lower portion of the Patagoniense succession and 18.85 Ma for the lowermost part of the overlying Santa Cruz Formation. 87Sr/ 86Sr data yielded ages ranging from 20.05 Ma at the lower part and 19.1 Ma for the upper portion of the Estancia 25 de Mayo Formation, in good agreement with respect to the U-Pb results. Our results constrain the age of these beds entirely into the early Miocene Burdigalian stage, and locally into the Superpatagoniense stage. Correlation with other Patagoniense units in Santa Cruz, especially in the westernmost parts of the Austral Basin, reveals the existence of a shallow and extended sea, and lack of correlation with global sea-level highstands suggests a local Andean tectonic overprint as the cause of the sea level rise. © 2012 Elsevier Ltd. Fil:Cuitiño, J.I. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Scasso, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2012 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v38_n_p110_Cuitino http://hdl.handle.net/20.500.12110/paper_08959811_v38_n_p110_Cuitino |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Argentina Austral basin Geochronology Miocene Patagonia Sr stratigraphy Transgression U-Pb ages chemostratigraphy chronostratigraphy geochronology isotopic analysis Miocene resolution strontium isotope transgression uranium-lead dating Patagonia Ostreidae |
spellingShingle |
Argentina Austral basin Geochronology Miocene Patagonia Sr stratigraphy Transgression U-Pb ages chemostratigraphy chronostratigraphy geochronology isotopic analysis Miocene resolution strontium isotope transgression uranium-lead dating Patagonia Ostreidae Cuitiño, José Ignacio Scasso, Roberto Adrian High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications |
topic_facet |
Argentina Austral basin Geochronology Miocene Patagonia Sr stratigraphy Transgression U-Pb ages chemostratigraphy chronostratigraphy geochronology isotopic analysis Miocene resolution strontium isotope transgression uranium-lead dating Patagonia Ostreidae |
description |
The classical marine Patagoniense succession at Lago Argentino, southwestern Patagonia (Argentina), known as Estancia 25 de Mayo Formation, was dated by radiometric U-Pb on zircon grains from pyroclastic rocks and 87Sr/ 86Sr ratio on calcitic oyster shells. U-Pb data yielded an age of 19.14 Ma for the lower portion of the Patagoniense succession and 18.85 Ma for the lowermost part of the overlying Santa Cruz Formation. 87Sr/ 86Sr data yielded ages ranging from 20.05 Ma at the lower part and 19.1 Ma for the upper portion of the Estancia 25 de Mayo Formation, in good agreement with respect to the U-Pb results. Our results constrain the age of these beds entirely into the early Miocene Burdigalian stage, and locally into the Superpatagoniense stage. Correlation with other Patagoniense units in Santa Cruz, especially in the westernmost parts of the Austral Basin, reveals the existence of a shallow and extended sea, and lack of correlation with global sea-level highstands suggests a local Andean tectonic overprint as the cause of the sea level rise. © 2012 Elsevier Ltd. |
author |
Cuitiño, José Ignacio Scasso, Roberto Adrian |
author_facet |
Cuitiño, José Ignacio Scasso, Roberto Adrian |
author_sort |
Cuitiño, José Ignacio |
title |
High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications |
title_short |
High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications |
title_full |
High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications |
title_fullStr |
High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications |
title_full_unstemmed |
High resolution isotopic ages for the early Miocene "Patagoniense" transgression in Southwest Patagonia: Stratigraphic implications |
title_sort |
high resolution isotopic ages for the early miocene "patagoniense" transgression in southwest patagonia: stratigraphic implications |
publishDate |
2012 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v38_n_p110_Cuitino http://hdl.handle.net/20.500.12110/paper_08959811_v38_n_p110_Cuitino |
work_keys_str_mv |
AT cuitinojoseignacio highresolutionisotopicagesfortheearlymiocenepatagoniensetransgressioninsouthwestpatagoniastratigraphicimplications AT scassorobertoadrian highresolutionisotopicagesfortheearlymiocenepatagoniensetransgressioninsouthwestpatagoniastratigraphicimplications |
_version_ |
1768543853901512704 |