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Depositional setting of the southern arms of Lago Argentino (southern Patagonia)

Bibliographic Data

ID16839720
AuthorsJorge G Lozano (0000-0002-2626-4253, Consejo Nacional de Investigaciones Científicas y Técnicas, corresponding author), Federica Donda (0000-0002-1284-5866, National Institute of Oceanography and Applied Geophysics), Donaldo M Bran (0000-0002-7093-2183, Consejo Nacional de Investigaciones Científicas y Técnicas), Emanuele Lodolo (0000-0002-4706-2095, National Institute of Oceanography and Applied Geophysics), Luca Baradello (0000-0002-9796-4521, National Institute of Oceanography and Applied Geophysics), Rosario Romeo (0000-0001-5867-8998, National Institute of Oceanography and Applied Geophysics), Juan Francisco Vilas, Maurizio Grossi (National Institute of Oceanography and Applied Geophysics), Alejandro Tassone (Consejo Nacional de Investigaciones Científicas y Técnicas)
Year2020
Volume16
Issue2
Pages324-334
Publication date2020-12-09
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueJournal of Maps (JOURNAL)
Journal identifiersISSN: 1744-5647 • E-ISSN: 1744-5647
PublisherInforma UK Limited (PUBLISHER • GB)
DOI10.1080/17445647.2020.1746700
OpenAlexW3013887713
LanguageEN
Citations received3
References cited19

Lago Argentino hosts a series of calving glaciers originating from the Southern Patagonian Icefield, the largest temperate ice cap of the southern hemisphere. Brazo Rico and Brazo Sur are two basins located in the southern part of Lago Argentino, where a series of high-resolution seismic profiles have allowed reconstruction of its depositional setting and sedimentary architecture, and to produce the following maps: top of the acoustic basement, top of the glacial sequence, and thickness of the glacio-lacustrine deposits. Data reveal the role of basement highs in the complex dynamic behavior of the two main glaciers, Perito Moreno and Frías glaciers, which fluctuated along Brazo Rico and Brazo Sur since the end of the Last Glacial Maximum. Their advances and retreats are testified by the presence of several moraine fronts buried beneath a generally undisturbed, glacio-lacustrine and lacustrine sequence, which records the depositional history of the southern arms of Lago Argentino

Archaeology · Basement · Climatology · Geography · Geomorphology · Glacial period · Glacier · Ice field · Moraine · Paleocurrent · Sedimentary depositional environment · Sedimentary rock · Southern Hemisphere · Structural basin · Cryospheric studies and observations · Geological formations and processes · Geology and Paleoclimatology Research · Geology · Paleontology

  • Do ice-dam rupture events leave a distinctive signature in proglacial lake sediments?

    Open Access•Guido Brignone, Matias Romero et al.•Quaternary Research•2025

  • Stratigraphic signature of the Perito Moreno ice-dammings during the Little Ice Age (southern Patagonia, Argentina)

    Open Access•Mauro Caffau, Emanuele Lodolo et al.•The Holocene•2021

  • Seismic stratigraphy of the northern area of Punta Bandera (Lago Argentino, southern Patagonia)

    Open Access•Jorge G Lozano, Florencia B Restelli et al.•Quaternary International•2024

  • Documentary and tree-ring evidence for a long-term interval without ice impoundments from Glaciar Perito Moreno, Patagonia, Argentina

    Open Access•Claudia M Guerrido, Ricardo Villalba et al.•The Holocene•2014

Unique citing works3
Citations per year0.6
Citation span2021 - 2025 (5)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 2

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