NissirosV1, Main, Exploration, bibRecord, 000193

Seismological and SAR signature of unrest at Nisyros caldera, Greece

Identifieur interne : 000193 ( Main/Exploration ); précédent : 000192; suivant : 000194

Seismological and SAR signature of unrest at Nisyros caldera, Greece

Auteurs : M. Sachpazi [Grèce] ; Ch. Kontoes [Grèce] ; N. Voulgaris [Grèce] ; M. Laigle [France] ; G. Vougioukalakis [Grèce] ; Olga Sikioti [Grèce] ; G. Stavrakakis [Grèce] ; J. Baskoutas [Grèce] ; J. Kalogeras [Grèce] ; J. Cl. Lepine [France]

Source :

Journal of volcanology and geothermal research [ 0377-0273 ] ; 2002.

RBID : Pascal:02-0464838

Descripteurs français

Pascal (Inist)
- Hellénides, Iles Egée Grèce, Sismologie, Arc volcanique, Télédétection spatiale, Radar antenne synthétique, Caldeira, Quaternaire, Activité, Explosion, Comportement, Volcan, Sismicité, Interférométrie, Déformation, Chambre magmatique, Perspective, Intrusion, ERS-2, Ile Nisyros, Hypocentre, Migration, Magma, Transport.
Wicri :
- topic : Sismologie, Migration.

English descriptors

KwdEn :
- Greek Aegean Islands, Hellenides, Quaternary, Space remote sensing, activity, behavior, calderas, deformation, explosions, hypocenter, interferometry, intrusions, magma chambers, magmas, migration, possibilities, seismicity, seismology, synthetic aperture radar, transport, volcanic arcs, volcanoes.

Abstract

Nisyros island, a Quaternary volcanic center located at the SE of the Aegean Volcanic Arc, has been in the past characterized by periods of intense seismic activity accompanied sometimes by hydrothermal explosions, the last one being in 1887. The recent long lasting episode of unrest (1995-1998) in the area is the first instrumentally documented providing information on the behavior of the volcano. Evidence from seismicity and SAR interferometry suggests that the presently active part of the Kos-Nisyros volcano-tectonic complex is located at the NW coast of Nisyros island defining an area much smaller than the whole volcano-tectonic area. Seismicity patterns vary both temporally and spatially consistently with different rates of vertical ground deformation inferred from SAR interferometry. These observations help us to discuss the different elements controlling the behavior of the volcanic system such as: the existence, location and timing of magma chamber inflation, the occurrence of tensile failure at the boundaries of the chamber and the possibility of magmatic fluids being expelled to form a shallow magmatic intrusion, the seismic failure and migration of hypocenters indicating shallow magma transport.

Affiliations:

Links toward previous steps (curation, corpus...)

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Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Greek Aegean Islands</term>
<term>Hellenides</term>
<term>Quaternary</term>
<term>Space remote sensing</term>
<term>activity</term>
<term>behavior</term>
<term>calderas</term>
<term>deformation</term>
<term>explosions</term>
<term>hypocenter</term>
<term>interferometry</term>
<term>intrusions</term>
<term>magma chambers</term>
<term>magmas</term>
<term>migration</term>
<term>possibilities</term>
<term>seismicity</term>
<term>seismology</term>
<term>synthetic aperture radar</term>
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<term>volcanic arcs</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Hellénides</term>
<term>Iles Egée Grèce</term>
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<term>Arc volcanique</term>
<term>Télédétection spatiale</term>
<term>Radar antenne synthétique</term>
<term>Caldeira</term>
<term>Quaternaire</term>
<term>Activité</term>
<term>Explosion</term>
<term>Comportement</term>
<term>Volcan</term>
<term>Sismicité</term>
<term>Interférométrie</term>
<term>Déformation</term>
<term>Chambre magmatique</term>
<term>Perspective</term>
<term>Intrusion</term>
<term>ERS-2</term>
<term>Ile Nisyros</term>
<term>Hypocentre</term>
<term>Migration</term>
<term>Magma</term>
<term>Transport</term>
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<front><div type="abstract" xml:lang="en">Nisyros island, a Quaternary volcanic center located at the SE of the Aegean Volcanic Arc, has been in the past characterized by periods of intense seismic activity accompanied sometimes by hydrothermal explosions, the last one being in 1887. The recent long lasting episode of unrest (1995-1998) in the area is the first instrumentally documented providing information on the behavior of the volcano. Evidence from seismicity and SAR interferometry suggests that the presently active part of the Kos-Nisyros volcano-tectonic complex is located at the NW coast of Nisyros island defining an area much smaller than the whole volcano-tectonic area. Seismicity patterns vary both temporally and spatially consistently with different rates of vertical ground deformation inferred from SAR interferometry. These observations help us to discuss the different elements controlling the behavior of the volcanic system such as: the existence, location and timing of magma chamber inflation, the occurrence of tensile failure at the boundaries of the chamber and the possibility of magmatic fluids being expelled to form a shallow magmatic intrusion, the seismic failure and migration of hypocenters indicating shallow magma transport.</div>
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   |texte=   Seismological and SAR signature of unrest at Nisyros caldera, Greece
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Seismological and SAR signature of unrest at Nisyros caldera, Greece

Seismological and SAR signature of unrest at Nisyros caldera, Greece

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