Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina)
In this paper, evidence of paleoearthquake-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System in the Isla Grande de Tierra del Fuego, southern Argentina, has been identified. Well-preserved soft-sediment deformation structures were found in a Holocene se...
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ftconicet:oai:ri.conicet.gov.ar:11336/55625 2023-10-09T21:47:20+02:00 Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) Onorato, María Romina Perucca, Laura Patricia A. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Lopez, Carlos Ramiro application/pdf http://hdl.handle.net/11336/55625 eng eng Elsevier Science info:eu-repo/semantics/altIdentifier/doi/10.1016/j.sedgeo.2016.04.010 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0037073816300392 http://hdl.handle.net/11336/55625 Onorato, María Romina; Perucca, Laura Patricia A.; Coronato, Andrea Maria Josefa; Rabassa, Jorge Oscar; Lopez, Carlos Ramiro; Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina); Elsevier Science; Sedimentary Geology; 344; 10-2016; 135-144 0037-0738 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ FAGNANO LAKE MAGALLANES–FAGNANO FAULT SYSTEM PALEOEARTHQUAKE SOFT-SEDIMENT DEFORMATION STRUCTURES UDAETA POND https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.sedgeo.2016.04.010 2023-09-24T18:52:10Z In this paper, evidence of paleoearthquake-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System in the Isla Grande de Tierra del Fuego, southern Argentina, has been identified. Well-preserved soft-sediment deformation structures were found in a Holocene sequence of the Udaeta pond. These structures were analyzed in terms of their geometrical characteristics, deformation mechanism, driving force system and possible trigger agent. They were also grouped in different morphological types: sand dykes, convolute lamination, load structures and faulted soft-sediment deformation features. Udaeta, a small pond in Argentina Tierra del Fuego, is considered a Quaternary pull-apart basin related to the Magallanes–Fagnano Fault System. The recognition of these seismically-induced features is an essential tool for paleoseismic studies. Since the three main urban centers in the Tierra del Fuego province of Argentina (Ushuaia, Río Grande and Tolhuin) have undergone an explosive growth in recent years, the results of this study will hopefully contribute to future analyses of the seismic risk of the region. Fil: Onorato, María Romina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Recursos Naturales y Ambiente. Departamento de Biología; Argentina Fil: Perucca, Laura Patricia A. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto de Geología "Dr. Emiliano Aparicio". Gabinete de Neotectónica y Geomorfología; Argentina Fil: Coronato, Andrea Maria Josefa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Recursos ... Article in Journal/Newspaper Antártida Tierra del Fuego CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Austral San Juan Argentina Magallanes ENVELOPE(-62.933,-62.933,-64.883,-64.883) Ushuaia ENVELOPE(-40.000,-40.000,-82.167,-82.167) isla Grande ENVELOPE(140.025,140.025,-66.664,-66.664) Gabinete ENVELOPE(-63.448,-63.448,-66.574,-66.574) Sedimentary Geology 344 135 144 |
institution |
Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
FAGNANO LAKE MAGALLANES–FAGNANO FAULT SYSTEM PALEOEARTHQUAKE SOFT-SEDIMENT DEFORMATION STRUCTURES UDAETA POND https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
spellingShingle |
FAGNANO LAKE MAGALLANES–FAGNANO FAULT SYSTEM PALEOEARTHQUAKE SOFT-SEDIMENT DEFORMATION STRUCTURES UDAETA POND https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Onorato, María Romina Perucca, Laura Patricia A. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Lopez, Carlos Ramiro Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) |
topic_facet |
FAGNANO LAKE MAGALLANES–FAGNANO FAULT SYSTEM PALEOEARTHQUAKE SOFT-SEDIMENT DEFORMATION STRUCTURES UDAETA POND https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
In this paper, evidence of paleoearthquake-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System in the Isla Grande de Tierra del Fuego, southern Argentina, has been identified. Well-preserved soft-sediment deformation structures were found in a Holocene sequence of the Udaeta pond. These structures were analyzed in terms of their geometrical characteristics, deformation mechanism, driving force system and possible trigger agent. They were also grouped in different morphological types: sand dykes, convolute lamination, load structures and faulted soft-sediment deformation features. Udaeta, a small pond in Argentina Tierra del Fuego, is considered a Quaternary pull-apart basin related to the Magallanes–Fagnano Fault System. The recognition of these seismically-induced features is an essential tool for paleoseismic studies. Since the three main urban centers in the Tierra del Fuego province of Argentina (Ushuaia, Río Grande and Tolhuin) have undergone an explosive growth in recent years, the results of this study will hopefully contribute to future analyses of the seismic risk of the region. Fil: Onorato, María Romina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Recursos Naturales y Ambiente. Departamento de Biología; Argentina Fil: Perucca, Laura Patricia A. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto de Geología "Dr. Emiliano Aparicio". Gabinete de Neotectónica y Geomorfología; Argentina Fil: Coronato, Andrea Maria Josefa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Recursos ... |
format |
Article in Journal/Newspaper |
author |
Onorato, María Romina Perucca, Laura Patricia A. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Lopez, Carlos Ramiro |
author_facet |
Onorato, María Romina Perucca, Laura Patricia A. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Lopez, Carlos Ramiro |
author_sort |
Onorato, María Romina |
title |
Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) |
title_short |
Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) |
title_full |
Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) |
title_fullStr |
Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) |
title_full_unstemmed |
Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina) |
title_sort |
seismically-induced soft-sediment deformation structures associated with the magallanes–fagnano fault system (isla grande de tierra del fuego, argentina) |
publisher |
Elsevier Science |
url |
http://hdl.handle.net/11336/55625 |
long_lat |
ENVELOPE(-62.933,-62.933,-64.883,-64.883) ENVELOPE(-40.000,-40.000,-82.167,-82.167) ENVELOPE(140.025,140.025,-66.664,-66.664) ENVELOPE(-63.448,-63.448,-66.574,-66.574) |
geographic |
Austral San Juan Argentina Magallanes Ushuaia isla Grande Gabinete |
geographic_facet |
Austral San Juan Argentina Magallanes Ushuaia isla Grande Gabinete |
genre |
Antártida Tierra del Fuego |
genre_facet |
Antártida Tierra del Fuego |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.sedgeo.2016.04.010 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0037073816300392 http://hdl.handle.net/11336/55625 Onorato, María Romina; Perucca, Laura Patricia A.; Coronato, Andrea Maria Josefa; Rabassa, Jorge Oscar; Lopez, Carlos Ramiro; Seismically-induced soft-sediment deformation structures associated with the Magallanes–Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina); Elsevier Science; Sedimentary Geology; 344; 10-2016; 135-144 0037-0738 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1016/j.sedgeo.2016.04.010 |
container_title |
Sedimentary Geology |
container_volume |
344 |
container_start_page |
135 |
op_container_end_page |
144 |
_version_ |
1779310403893854208 |