on Deception Island (Antarctica)

Abstraet On the basis of the correlation between seismic tectonostratigraphic units, volcanism, and geochemical distribution patterns of sea-floor sediments on Deception Island (Antarctica), a regional tectonic extension is sug-gested to explain the sequence of volcanic and hydro-thermal events. The...

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Bibliographic Details
Main Authors: J. Rey, L. Somoza, J. Martinez-frias
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1993
Subjects:
Brandsfield Strait (Fig. 1). Tectonically
the DI is located
Deception Island
Antarc*
Antarctica
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.465.1278
http://tierra.rediris.es/publipapers/Deception_Geo_Marine.pdf
Description
Summary:Abstraet On the basis of the correlation between seismic tectonostratigraphic units, volcanism, and geochemical distribution patterns of sea-floor sediments on Deception Island (Antarctica), a regional tectonic extension is sug-gested to explain the sequence of volcanic and hydro-thermal events. The syncollapse caldera episode is com-posed of five tectonostratigraphic units separated by pro-gressively tilted and bent unconformities. Each unit shows a sequence of Quaternary volcanic ones and mound struc-tures that display high contents of Fe, Mn, and Zn. As-rich active fumaroles and hot-spring areas are associated with the postcollapse episode and linked to normal faulting and present volcanism.

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