Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate

The upper cliff of the Santa Cruz River was used to assess the proglacial environments of the Argentino Glacier outlet of Late Pleistocene age. These cliffs show glaciolacustrine, fluvioglacial and till deposits, where only the first one are deformed. Glacial landforms in the area and these structur...

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Main Authors: Goyanes, Gabriel Alejandro, Massabie, Armando Carlos
Language:unknown
Published: 2015
Subjects:
Online Access:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v57_n_p1_Goyanes
https://hdl.handle.net/20.500.12110/paper_08959811_v57_n_p1_Goyanes
id ftunibueairesbd:paper:paper_08959811_v57_n_p1_Goyanes
record_format openpolar
spelling ftunibueairesbd:paper:paper_08959811_v57_n_p1_Goyanes 2023-05-15T16:40:36+02:00 Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate Goyanes, Gabriel Alejandro Massabie, Armando Carlos 2015 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v57_n_p1_Goyanes https://hdl.handle.net/20.500.12110/paper_08959811_v57_n_p1_Goyanes unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v57_n_p1_Goyanes http://hdl.handle.net/20.500.12110/paper_08959811_v57_n_p1_Goyanes Argentina Glacial landforms Last Glaciation Push moraines Santa Cruz river Southern Patagonia drumlin glacial landform glaciotectonics ice sheet overturn Pleistocene push moraine thrust Patagonia Santa Cruz River [Santa Cruz] Santa Cruz [Argentina] 2015 ftunibueairesbd https://doi.org/20.500.12110/paper_08959811_v57_n_p1_Goyanes 2023-02-16T01:56:49Z The upper cliff of the Santa Cruz River was used to assess the proglacial environments of the Argentino Glacier outlet of Late Pleistocene age. These cliffs show glaciolacustrine, fluvioglacial and till deposits, where only the first one are deformed. Glacial landforms in the area and these structures suggest that the ice mass advanced, topographically controlled, towards the east from the Patagonian Ice Sheet pushing up the proglacial sediments.The spatial arrangement of thrusts and overturned folds, the drumlins-flutes moraine directions and the end moraines shape, allow inferring the dynamic and the Argentino glacier profile. Detailed analyses of the glaciotectonic structures indicate that these have two origins: load in the north with stress transfer to the southeast, and push from the west. Through the analysis of deformed sediments, their thickness and their sedimentary and structural features, three zones of deformations were recognized. Each of these zones was associated to glacial advances because of changes of the regional climate conditions. © 2014 Elsevier Ltd. Fil:Goyanes, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Massabie, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Other/Unknown Material Ice Sheet Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Argentina Argentino Patagonia
institution Open Polar
collection Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
op_collection_id ftunibueairesbd
language unknown
topic Argentina
Glacial landforms
Last Glaciation
Push moraines
Santa Cruz river
Southern Patagonia
drumlin
glacial landform
glaciotectonics
ice sheet
overturn
Pleistocene
push moraine
thrust
Patagonia
Santa Cruz River [Santa Cruz]
Santa Cruz [Argentina]
spellingShingle Argentina
Glacial landforms
Last Glaciation
Push moraines
Santa Cruz river
Southern Patagonia
drumlin
glacial landform
glaciotectonics
ice sheet
overturn
Pleistocene
push moraine
thrust
Patagonia
Santa Cruz River [Santa Cruz]
Santa Cruz [Argentina]
Goyanes, Gabriel Alejandro
Massabie, Armando Carlos
Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate
topic_facet Argentina
Glacial landforms
Last Glaciation
Push moraines
Santa Cruz river
Southern Patagonia
drumlin
glacial landform
glaciotectonics
ice sheet
overturn
Pleistocene
push moraine
thrust
Patagonia
Santa Cruz River [Santa Cruz]
Santa Cruz [Argentina]
description The upper cliff of the Santa Cruz River was used to assess the proglacial environments of the Argentino Glacier outlet of Late Pleistocene age. These cliffs show glaciolacustrine, fluvioglacial and till deposits, where only the first one are deformed. Glacial landforms in the area and these structures suggest that the ice mass advanced, topographically controlled, towards the east from the Patagonian Ice Sheet pushing up the proglacial sediments.The spatial arrangement of thrusts and overturned folds, the drumlins-flutes moraine directions and the end moraines shape, allow inferring the dynamic and the Argentino glacier profile. Detailed analyses of the glaciotectonic structures indicate that these have two origins: load in the north with stress transfer to the southeast, and push from the west. Through the analysis of deformed sediments, their thickness and their sedimentary and structural features, three zones of deformations were recognized. Each of these zones was associated to glacial advances because of changes of the regional climate conditions. © 2014 Elsevier Ltd. Fil:Goyanes, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Massabie, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
author Goyanes, Gabriel Alejandro
Massabie, Armando Carlos
author_facet Goyanes, Gabriel Alejandro
Massabie, Armando Carlos
author_sort Goyanes, Gabriel Alejandro
title Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate
title_short Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate
title_full Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate
title_fullStr Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate
title_full_unstemmed Push moraines in the upper valley of Santa Cruz river, southwest Argentina. Structural analysis and relationship with Late Pleistocene paleoclimate
title_sort push moraines in the upper valley of santa cruz river, southwest argentina. structural analysis and relationship with late pleistocene paleoclimate
publishDate 2015
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v57_n_p1_Goyanes
https://hdl.handle.net/20.500.12110/paper_08959811_v57_n_p1_Goyanes
geographic Argentina
Argentino
Patagonia
geographic_facet Argentina
Argentino
Patagonia
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v57_n_p1_Goyanes
http://hdl.handle.net/20.500.12110/paper_08959811_v57_n_p1_Goyanes
op_doi https://doi.org/20.500.12110/paper_08959811_v57_n_p1_Goyanes
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