Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina
Early Miocene shallow marine deposits in the region of Lago Posadas-Meseta Belgrano (Argentina) represent part of the “Patagoniense” transgression, an Atlantic marine incursion that flooded large part of Patagonia, including the Austral (foreland) Basin (southern Patagonia). These deposits, referred...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v42_n3_p364_Cuitino http://hdl.handle.net/20.500.12110/paper_07187092_v42_n3_p364_Cuitino |
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paper:paper_07187092_v42_n3_p364_Cuitino2023-06-08T15:43:18Z Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina Patagonia Patagoniense Sedimentology Sr-stratigraphy Transgression deposition marine sediment Miocene sedimentation sedimentology sequence stratigraphy topography transgression Argentina Austral Basin Patagonia Ostreidae Early Miocene shallow marine deposits in the region of Lago Posadas-Meseta Belgrano (Argentina) represent part of the “Patagoniense” transgression, an Atlantic marine incursion that flooded large part of Patagonia, including the Austral (foreland) Basin (southern Patagonia). These deposits, referred as El Chacay (Argentina) or Guadal (Chile) formations, and the transition to the overlying Santa Cruz Formation were divided into six facies: subtidal sand-bars, shallow marine sandy deposits, muddy shelf deposits, estuarine complex deposits, fluvial channels and fluvial floodplains. These are arranged in a general transgressive-regressive cycle, subdivided into two stratigraphic sequences, separated by a major erosional surface.87Sr/86Sr ages from shell carbonate in eight oysters yielded an age range of 20.3 to 18.1 Ma for these “Patagoniense” deposits. Correlation with other dated “Patagoniense” sections in southern Patagonia, like those at Lago Argentino or Comodoro Rivadavia, indicates that they belong to a single transgression that flooded several Patagonian basins approximately at the same time. Eustasy, flexural subsidence created by tectonic loading in the adjacent fold-and-thrust belt, and basin floor paleo-topography controlled the duration of the depositional event and the sedimentation style of these shallow marine deposits. © 2015, Servicio Nacional de Geologia y Mineria. All rights reserved. 2015 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v42_n3_p364_Cuitino http://hdl.handle.net/20.500.12110/paper_07187092_v42_n3_p364_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 |
Patagonia Patagoniense Sedimentology Sr-stratigraphy Transgression deposition marine sediment Miocene sedimentation sedimentology sequence stratigraphy topography transgression Argentina Austral Basin Patagonia Ostreidae |
spellingShingle |
Patagonia Patagoniense Sedimentology Sr-stratigraphy Transgression deposition marine sediment Miocene sedimentation sedimentology sequence stratigraphy topography transgression Argentina Austral Basin Patagonia Ostreidae Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina |
topic_facet |
Patagonia Patagoniense Sedimentology Sr-stratigraphy Transgression deposition marine sediment Miocene sedimentation sedimentology sequence stratigraphy topography transgression Argentina Austral Basin Patagonia Ostreidae |
description |
Early Miocene shallow marine deposits in the region of Lago Posadas-Meseta Belgrano (Argentina) represent part of the “Patagoniense” transgression, an Atlantic marine incursion that flooded large part of Patagonia, including the Austral (foreland) Basin (southern Patagonia). These deposits, referred as El Chacay (Argentina) or Guadal (Chile) formations, and the transition to the overlying Santa Cruz Formation were divided into six facies: subtidal sand-bars, shallow marine sandy deposits, muddy shelf deposits, estuarine complex deposits, fluvial channels and fluvial floodplains. These are arranged in a general transgressive-regressive cycle, subdivided into two stratigraphic sequences, separated by a major erosional surface.87Sr/86Sr ages from shell carbonate in eight oysters yielded an age range of 20.3 to 18.1 Ma for these “Patagoniense” deposits. Correlation with other dated “Patagoniense” sections in southern Patagonia, like those at Lago Argentino or Comodoro Rivadavia, indicates that they belong to a single transgression that flooded several Patagonian basins approximately at the same time. Eustasy, flexural subsidence created by tectonic loading in the adjacent fold-and-thrust belt, and basin floor paleo-topography controlled the duration of the depositional event and the sedimentation style of these shallow marine deposits. © 2015, Servicio Nacional de Geologia y Mineria. All rights reserved. |
title |
Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina |
title_short |
Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina |
title_full |
Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina |
title_fullStr |
Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina |
title_full_unstemmed |
Sr-stratigraphy and sedimentary evolution of early Miocene marine foreland deposits in the northern Austral (Magallanes) basin, Argentina |
title_sort |
sr-stratigraphy and sedimentary evolution of early miocene marine foreland deposits in the northern austral (magallanes) basin, argentina |
publishDate |
2015 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v42_n3_p364_Cuitino http://hdl.handle.net/20.500.12110/paper_07187092_v42_n3_p364_Cuitino |
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1768545147814936576 |