The recent seismo-volcanic activity at Deception

This paper reviews the recent seismic studies carried out at Deception Island, South Shetland Islands, Antarctica, which was monitoredby the Argentinean andSpanish Antarctic Programs since 1986. Several types of seismic network have been deployed temporarily during each Antarctic summer. These netwo...

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Main Authors: Jes!us M. Ib!an Ez, Javier Almendros, Enrique Carmona, Miguel Abril
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2002
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.5284
http://hera.ugr.es/doi/1498085X.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.379.5284 2023-05-15T13:36:48+02:00 The recent seismo-volcanic activity at Deception Jes!us M. Ib!an Ez Javier Almendros Enrique Carmona Miguel Abril The Pennsylvania State University CiteSeerX Archives 2002 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.5284 http://hera.ugr.es/doi/1498085X.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.5284 http://hera.ugr.es/doi/1498085X.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://hera.ugr.es/doi/1498085X.pdf text 2002 ftciteseerx 2016-09-18T00:16:23Z This paper reviews the recent seismic studies carried out at Deception Island, South Shetland Islands, Antarctica, which was monitoredby the Argentinean andSpanish Antarctic Programs since 1986. Several types of seismic network have been deployed temporarily during each Antarctic summer. These networks have consisted of a variety of instruments, including radio-telemetered stations, autonomous digital seismic stations, broadband seismometers, and seismic arrays. We have identified two main types of seismic signals generated by the volcano, namely pure seismovolcanic signals, such as volcanic tremor andlong-period(LP) events, andvolcano-tectonic (VT) earthquakes. Their temporal distributions are far from homogeneous. Volcanic tremors and LP events usually occur in seismic swarms lasting from a few hours to some days. The number of LP events in these swarms is highly variable, from a background level of less than 30/day to a peak activity of about 100 events/h. The occurrence of VT earthquakes is even more irregular. Most VT earthquakes at Deception Island have been recorded during two intense seismic crises, in 1992 and 1999, respectively. Some of these VT earthquakes were large enough to be felt by researchers working on the island. Analyses of both types of seismic events have allowed us to derive source locations, establish seismic source models, analyze seismic attenuation, calculate the energy andstress drop of the seismic sources, andrelate the occurrence of seismicity to the volcanic activity. Pure seismo-volcanic signals are modelled as the consequence of hydrothermal Text Antarc* Antarctic Antarctica Deception Island South Shetland Islands Unknown Antarctic Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950) South Shetland Islands
institution Open Polar
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description This paper reviews the recent seismic studies carried out at Deception Island, South Shetland Islands, Antarctica, which was monitoredby the Argentinean andSpanish Antarctic Programs since 1986. Several types of seismic network have been deployed temporarily during each Antarctic summer. These networks have consisted of a variety of instruments, including radio-telemetered stations, autonomous digital seismic stations, broadband seismometers, and seismic arrays. We have identified two main types of seismic signals generated by the volcano, namely pure seismovolcanic signals, such as volcanic tremor andlong-period(LP) events, andvolcano-tectonic (VT) earthquakes. Their temporal distributions are far from homogeneous. Volcanic tremors and LP events usually occur in seismic swarms lasting from a few hours to some days. The number of LP events in these swarms is highly variable, from a background level of less than 30/day to a peak activity of about 100 events/h. The occurrence of VT earthquakes is even more irregular. Most VT earthquakes at Deception Island have been recorded during two intense seismic crises, in 1992 and 1999, respectively. Some of these VT earthquakes were large enough to be felt by researchers working on the island. Analyses of both types of seismic events have allowed us to derive source locations, establish seismic source models, analyze seismic attenuation, calculate the energy andstress drop of the seismic sources, andrelate the occurrence of seismicity to the volcanic activity. Pure seismo-volcanic signals are modelled as the consequence of hydrothermal
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Jes!us M. Ib!an Ez
Javier Almendros
Enrique Carmona
Miguel Abril
spellingShingle Jes!us M. Ib!an Ez
Javier Almendros
Enrique Carmona
Miguel Abril
The recent seismo-volcanic activity at Deception
author_facet Jes!us M. Ib!an Ez
Javier Almendros
Enrique Carmona
Miguel Abril
author_sort Jes!us M. Ib!an Ez
title The recent seismo-volcanic activity at Deception
title_short The recent seismo-volcanic activity at Deception
title_full The recent seismo-volcanic activity at Deception
title_fullStr The recent seismo-volcanic activity at Deception
title_full_unstemmed The recent seismo-volcanic activity at Deception
title_sort recent seismo-volcanic activity at deception
publishDate 2002
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.379.5284
http://hera.ugr.es/doi/1498085X.pdf
long_lat ENVELOPE(-60.633,-60.633,-62.950,-62.950)
geographic Antarctic
Deception Island
South Shetland Islands
geographic_facet Antarctic
Deception Island
South Shetland Islands
genre Antarc*
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Antarctica
Deception Island
South Shetland Islands
genre_facet Antarc*
Antarctic
Antarctica
Deception Island
South Shetland Islands
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