El volcanismo de isla decepcion (Peninsula Antartica)

The Deception island volcanism is constitued by tholeitic-calc alkaline rocks High Al 2O 2 contents and low TiO 2 and K 2O are features of these volcanic rocks. The composition change from basalts, basaltic andesites, andesites to dacrtes. These characteristics permit to associate this volcanism to...

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Bibliographic Details
Main Authors: Aparicio, A., Risso, C., Viramonte, J.G., Menegatti, M., Petrinovic, I.
Format: Journal/Newspaper
Language:unknown
Subjects:
Antartic
Cale-alkaline volcanism
Subduction
antartic*
Deception Island
Online Access:https://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
id ftunibueairesbd:todo:paper_03660176_v108_n3_p19_Aparicio
record_format openpolar
spelling ftunibueairesbd:todo:paper_03660176_v108_n3_p19_Aparicio 2023-10-29T02:32:39+01:00 El volcanismo de isla decepcion (Peninsula Antartica) Aparicio, A. Risso, C. Viramonte, J.G. Menegatti, M. Petrinovic, I. https://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio unknown http://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Antartic Cale-alkaline volcanism Subduction JOUR ftunibueairesbd https://doi.org/20.500.12110/paper_03660176_v108_n3_p19_Aparicio 2023-10-05T02:03:59Z The Deception island volcanism is constitued by tholeitic-calc alkaline rocks High Al 2O 2 contents and low TiO 2 and K 2O are features of these volcanic rocks. The composition change from basalts, basaltic andesites, andesites to dacrtes. These characteristics permit to associate this volcanism to the subduction process between the Drake and Shetland plates. The subduction process continues at the present time. Journal/Newspaper antartic* Deception Island 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 Antartic
Cale-alkaline volcanism
Subduction
spellingShingle Antartic
Cale-alkaline volcanism
Subduction
Aparicio, A.
Risso, C.
Viramonte, J.G.
Menegatti, M.
Petrinovic, I.
El volcanismo de isla decepcion (Peninsula Antartica)
topic_facet Antartic
Cale-alkaline volcanism
Subduction
description The Deception island volcanism is constitued by tholeitic-calc alkaline rocks High Al 2O 2 contents and low TiO 2 and K 2O are features of these volcanic rocks. The composition change from basalts, basaltic andesites, andesites to dacrtes. These characteristics permit to associate this volcanism to the subduction process between the Drake and Shetland plates. The subduction process continues at the present time.
format Journal/Newspaper
author Aparicio, A.
Risso, C.
Viramonte, J.G.
Menegatti, M.
Petrinovic, I.
author_facet Aparicio, A.
Risso, C.
Viramonte, J.G.
Menegatti, M.
Petrinovic, I.
author_sort Aparicio, A.
title El volcanismo de isla decepcion (Peninsula Antartica)
title_short El volcanismo de isla decepcion (Peninsula Antartica)
title_full El volcanismo de isla decepcion (Peninsula Antartica)
title_fullStr El volcanismo de isla decepcion (Peninsula Antartica)
title_full_unstemmed El volcanismo de isla decepcion (Peninsula Antartica)
title_sort el volcanismo de isla decepcion (peninsula antartica)
url https://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
genre antartic*
Deception Island
genre_facet antartic*
Deception Island
op_relation http://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar
op_doi https://doi.org/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
_version_ 1781054451660881920

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