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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Detalles Bibliográficos
Autores principales: Baraldo, Andrés, Rinaldi, Carlos A.
Publicado: 2000
Materias:
Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
Deception Island
South Shetland Islands
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v13_n8_p785_Baraldo
http://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id paper:paper_08959811_v13_n8_p785_Baraldo
record_format dspace
spelling paper:paper_08959811_v13_n8_p785_Baraldo2023-06-08T15:48:09Z Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica Baraldo, Andrés Rinaldi, Carlos A. Antarctica Deception island Volcanic calderas Volcanoes caldera stratigraphy structural geology volcano Antarctica Deception Island South Shetland Islands 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. 2000 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v13_n8_p785_Baraldo http://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
Antarctica
Deception Island
South Shetland Islands
spellingShingle Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
Antarctica
Deception Island
South Shetland Islands
Baraldo, Andrés
Rinaldi, Carlos A.
Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
topic_facet Antarctica
Deception island
Volcanic calderas
Volcanoes
caldera
stratigraphy
structural geology
volcano
Antarctica
Deception Island
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.
author Baraldo, Andrés
Rinaldi, Carlos A.
author_facet Baraldo, Andrés
Rinaldi, Carlos A.
author_sort Baraldo, Andrés
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
publishDate 2000
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v13_n8_p785_Baraldo
http://hdl.handle.net/20.500.12110/paper_08959811_v13_n8_p785_Baraldo
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