Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey
ABSTRACT Lago Yehuin, a WNW-ESE elongated basin located in the outer fold-and-thrust belt of the Fuegian Andes, occupies a compartmented structural depression originated along a segment of the left-lateral Lago Deseado fault system. This paper describes the first geophysical survey performed within...
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oai:scielo:S0718-710620180003003182018-11-05Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical surveyLozano,Jorge G.Tassone,AlejandroLodolo,EmanueleMenichetti,MarcoCerredo,María E.Bran,Donaldo M.Esteban,FedericoOrmazabal,Juan P.Baradello,LucaVilas,Juan F. Lago Yehuin Fuegian Andes Single-channel seismic profiles Strike-slip tectonics ABSTRACT Lago Yehuin, a WNW-ESE elongated basin located in the outer fold-and-thrust belt of the Fuegian Andes, occupies a compartmented structural depression originated along a segment of the left-lateral Lago Deseado fault system. This paper describes the first geophysical survey performed within the lake. New acquired high-resolution single-channel seismic data, integrated with geological information in the surroundings of the Lago Yehuin, allowed to: (i) produce a complete bathymetric map of the lake, (ii) reconstruct the basement surface of the lake, and (iii) analyze the geometry, distribution, and thickness of the sedimentary infill. Two sub-basins were recognized within Lago Yehuin: A western sub-basin, 7.5 km long, with a maximum depth of 118 m; an eastern sub-basin, 7.2 km long with a maximum depth of 80 m. Both sub-basins are limited by a set of normal faults which overprint NE-verging thrusts. Three seismostratigraphic units have been identified in the seismic records: (1) a lower unit with wedged geometry interpreted as a mass flow deposits; (2) a thick (up to 120 m) intermediate unit of glacio-lacustrine nature and irregularly distributed in the Yehuin basin; (3) a thin (generally <10 m) upper lacustrine unit which drapes the entire basin. Lago Yehuin is considered a Neogene basin generated by strike-slip tectonics that was later affected by glacial and glacio-lacustrine deposition. Interpreted submerged ridge moraines within Lago Yehuin are correlated with onland moraine arcs built by the complete recessional paths of Fuego and Ewan ice lobes. A significant structural control is proposed not only for the formation of Lago Yehuin, but also for the general paths of the northern arms of the Fagnano palaeo-glacier.info:eu-repo/semantics/openAccessServicio Nacional de Geología y Minería (SERNAGEOMIN)Andean geology v.45 n.3 20182018-01-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062018000300318en10.5027/andgeov45n3-3085 |
institution |
Scielo Chile |
collection |
Scielo Chile |
language |
English |
topic |
Lago Yehuin Fuegian Andes Single-channel seismic profiles Strike-slip tectonics |
spellingShingle |
Lago Yehuin Fuegian Andes Single-channel seismic profiles Strike-slip tectonics Lozano,Jorge G. Tassone,Alejandro Lodolo,Emanuele Menichetti,Marco Cerredo,María E. Bran,Donaldo M. Esteban,Federico Ormazabal,Juan P. Baradello,Luca Vilas,Juan F. Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey |
description |
ABSTRACT Lago Yehuin, a WNW-ESE elongated basin located in the outer fold-and-thrust belt of the Fuegian Andes, occupies a compartmented structural depression originated along a segment of the left-lateral Lago Deseado fault system. This paper describes the first geophysical survey performed within the lake. New acquired high-resolution single-channel seismic data, integrated with geological information in the surroundings of the Lago Yehuin, allowed to: (i) produce a complete bathymetric map of the lake, (ii) reconstruct the basement surface of the lake, and (iii) analyze the geometry, distribution, and thickness of the sedimentary infill. Two sub-basins were recognized within Lago Yehuin: A western sub-basin, 7.5 km long, with a maximum depth of 118 m; an eastern sub-basin, 7.2 km long with a maximum depth of 80 m. Both sub-basins are limited by a set of normal faults which overprint NE-verging thrusts. Three seismostratigraphic units have been identified in the seismic records: (1) a lower unit with wedged geometry interpreted as a mass flow deposits; (2) a thick (up to 120 m) intermediate unit of glacio-lacustrine nature and irregularly distributed in the Yehuin basin; (3) a thin (generally <10 m) upper lacustrine unit which drapes the entire basin. Lago Yehuin is considered a Neogene basin generated by strike-slip tectonics that was later affected by glacial and glacio-lacustrine deposition. Interpreted submerged ridge moraines within Lago Yehuin are correlated with onland moraine arcs built by the complete recessional paths of Fuego and Ewan ice lobes. A significant structural control is proposed not only for the formation of Lago Yehuin, but also for the general paths of the northern arms of the Fagnano palaeo-glacier. |
author |
Lozano,Jorge G. Tassone,Alejandro Lodolo,Emanuele Menichetti,Marco Cerredo,María E. Bran,Donaldo M. Esteban,Federico Ormazabal,Juan P. Baradello,Luca Vilas,Juan F. |
author_facet |
Lozano,Jorge G. Tassone,Alejandro Lodolo,Emanuele Menichetti,Marco Cerredo,María E. Bran,Donaldo M. Esteban,Federico Ormazabal,Juan P. Baradello,Luca Vilas,Juan F. |
author_sort |
Lozano,Jorge G. |
title |
Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey |
title_short |
Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey |
title_full |
Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey |
title_fullStr |
Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey |
title_full_unstemmed |
Origin and evolution of lago Yehuin (Tierra del Fuego, Argentina): Results from a geophysical survey |
title_sort |
origin and evolution of lago yehuin (tierra del fuego, argentina): results from a geophysical survey |
publisher |
Servicio Nacional de Geología y Minería (SERNAGEOMIN) |
publishDate |
2018 |
url |
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062018000300318 |
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