Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica

Deception Island is an active volcano with a large structural collapse that has been interpreted by several investigators as having been generated by different processes. The general stratigraphy and structural study of the volcano is presented, with special emphasis on the distribution and structur...

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Bibliographic Details
Main Authors: Baraldo, A., Rinaldi, C.A.
Format: Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
id ftunibueairesbd:todo:paper_08959811_v13_n8_p785_Baraldo
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spelling ftunibueairesbd:todo:paper_08959811_v13_n8_p785_Baraldo 2023-10-29T02:31:22+01:00 Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica Baraldo, A. Rinaldi, C.A. https://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo unknown http://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Antarctica Deception island Volcanic calderas Volcanoes caldera stratigraphy structural geology volcano South Shetland Islands JOUR ftunibueairesbd https://doi.org/20.500.12110/paper_08959811_v13_n8_p785_Baraldo 2023-10-05T01:49:14Z Deception Island is an active volcano with a large structural collapse that has been interpreted by several investigators as having been generated by different processes. The general stratigraphy and structural study of the volcano is presented, with special emphasis on the distribution and structural disposition of the different stratigraphic units. The rocks of Deception Island have traditionally been divided into pre- and post-caldera products. A subdivision of the pre-caldera deposits, called 'pre- and syn-caldera deposits,' has been observed in two main units. Bulk magnetic susceptibility analyses are used to support the field stratigraphy presented. The localization and distribution of dikes is used to assign the central collapse of the volcano to rifting induced by tensional tectonics occurring in the Bransfield Strait and the presence of transcurrent faults around the island. © 2000 Elsevier Science Ltd. All rights reserved. Fil:Baraldo, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Rinaldi, C.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Journal/Newspaper Antarc* Antarctica Bransfield Strait Deception Island South Shetland Islands Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
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 Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
South Shetland Islands
spellingShingle Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
South Shetland Islands
Baraldo, A.
Rinaldi, C.A.
Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
topic_facet Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
South Shetland Islands
description Deception Island is an active volcano with a large structural collapse that has been interpreted by several investigators as having been generated by different processes. The general stratigraphy and structural study of the volcano is presented, with special emphasis on the distribution and structural disposition of the different stratigraphic units. The rocks of Deception Island have traditionally been divided into pre- and post-caldera products. A subdivision of the pre-caldera deposits, called 'pre- and syn-caldera deposits,' has been observed in two main units. Bulk magnetic susceptibility analyses are used to support the field stratigraphy presented. The localization and distribution of dikes is used to assign the central collapse of the volcano to rifting induced by tensional tectonics occurring in the Bransfield Strait and the presence of transcurrent faults around the island. © 2000 Elsevier Science Ltd. All rights reserved. Fil:Baraldo, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Rinaldi, C.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
format Journal/Newspaper
author Baraldo, A.
Rinaldi, C.A.
author_facet Baraldo, A.
Rinaldi, C.A.
author_sort Baraldo, A.
title Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
title_short Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
title_full Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
title_fullStr Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
title_full_unstemmed Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
title_sort stratigraphy and structure of deception island, south shetland islands, antarctica
url https://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
genre Antarc*
Antarctica
Bransfield Strait
Deception Island
South Shetland Islands
genre_facet Antarc*
Antarctica
Bransfield Strait
Deception Island
South Shetland Islands
op_relation http://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar
op_doi https://doi.org/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
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