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...

Full description

Bibliographic Details
Language:unknown
Published: 1997
Subjects:
Online Access:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v108_n3_p19_Aparicio
https://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
id ftunibueairesbd:paper:paper_03660176_v108_n3_p19_Aparicio
record_format openpolar
spelling ftunibueairesbd:paper:paper_03660176_v108_n3_p19_Aparicio 2023-05-15T14:15:30+02:00 El volcanismo de isla decepcion (Peninsula Antartica) 1997 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v108_n3_p19_Aparicio https://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v108_n3_p19_Aparicio http://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio Antartic Cale-alkaline volcanism Subduction 1997 ftunibueairesbd https://doi.org/20.500.12110/paper_03660176_v108_n3_p19_Aparicio 2023-02-16T01:59:41Z 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. Other/Unknown Material antartic* Deception Island Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Decepcion ENVELOPE(-60.700,-60.700,-62.983,-62.983) Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950)
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
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.
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)
publishDate 1997
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v108_n3_p19_Aparicio
https://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
long_lat ENVELOPE(-60.700,-60.700,-62.983,-62.983)
ENVELOPE(-60.633,-60.633,-62.950,-62.950)
geographic Decepcion
Deception Island
geographic_facet Decepcion
Deception Island
genre antartic*
Deception Island
genre_facet antartic*
Deception Island
op_relation https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v108_n3_p19_Aparicio
http://hdl.handle.net/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
op_doi https://doi.org/20.500.12110/paper_03660176_v108_n3_p19_Aparicio
_version_ 1766287868779560960