NissirosV1, PascalFrancis, Corpus, bibRecord, 000038

Seismological and SAR signature of unrest at Nisyros caldera, Greece

Identifieur interne : 000038 ( PascalFrancis/Corpus ); précédent : 000037; suivant : 000039

Seismological and SAR signature of unrest at Nisyros caldera, Greece

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

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.

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.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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C01	`01`		`ENG`	@0 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.
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Format Inist (serveur)

NO :	PASCAL 02-0464838 INIST
ET :	Seismological and SAR signature of unrest at Nisyros caldera, Greece
AU :	SACHPAZI (M.); KONTOES (Ch.); VOULGARIS (N.); LAIGLE (M.); VOUGIOUKALAKIS (G.); SIKIOTI (Olga); STAVRAKAKIS (G.); BASKOUTAS (J.); KALOGERAS (J.); LEPINE (J. Cl.)
AF :	National Observatory of Athens, Lofos Nymfon/Athens/Grèce (1 aut., 2 aut., 6 aut., 7 aut., 8 aut., 9 aut.); Department of Geology and Geothermy, Panepistimioupoli/Athens/Grèce (3 aut.); Laboratoire de Sismologie, Experimentale, Institut de Physique du Globe, 4 place Jussieu/75252 Paris/France (4 aut., 10 aut.); Institute of Geological and Mineral Exploration, Mesogion 70/Athens/Grèce (5 aut.)
DT :	Publication en série; Papier de recherche; Niveau analytique
SO :	Journal of volcanology and geothermal research; ISSN 0377-0273; Coden JVGRDQ; Pays-Bas; Da. 2002; Vol. 116; No. 1-2; Pp. 19-33; Bibl. 1 p.1/4
LA :	Anglais
EA :	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.
CC :	222A01; 225B03; 001E01F01; 001E01M03
FD :	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
FG :	Grèce; Europe Sud; Europe; Cénozoïque; Phanérozoïque
ED :	Hellenides; Greek Aegean Islands; seismology; volcanic arcs; Space remote sensing; synthetic aperture radar; calderas; Quaternary; activity; explosions; behavior; volcanoes; seismicity; interferometry; deformation; magma chambers; possibilities; intrusions; hypocenter; migration; magmas; transport
EG :	Greece; Southern Europe; Europe; Cenozoic; Phanerozoic
SD :	Islas Egeas Griegas; Teledetección espacial; Caldera; Cuaternario; Actividad; Explosión; Volcán; Sismicidad; Interferometría; Cámara magmática; Perspectiva; Intrusión; Hipocentro; Migración; Magma; Transporte
LO :	INIST-17236.354000104353950020
ID :	02-0464838

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Pascal:02-0464838

Le document en format XML

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<author><name sortKey="Sikioti, Olga" sort="Sikioti, Olga" uniqKey="Sikioti O" first="Olga" last="Sikioti">Olga Sikioti</name>
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<sZ>9 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Stavrakakis, G" sort="Stavrakakis, G" uniqKey="Stavrakakis G" first="G." last="Stavrakakis">G. Stavrakakis</name>
<affiliation><inist:fA14 i1="01"><s1>National Observatory of Athens, Lofos Nymfon</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
<sZ>9 aut.</sZ>
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</affiliation>
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<author><name sortKey="Baskoutas, J" sort="Baskoutas, J" uniqKey="Baskoutas J" first="J." last="Baskoutas">J. Baskoutas</name>
<affiliation><inist:fA14 i1="01"><s1>National Observatory of Athens, Lofos Nymfon</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
<sZ>9 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Kalogeras, J" sort="Kalogeras, J" uniqKey="Kalogeras J" first="J." last="Kalogeras">J. Kalogeras</name>
<affiliation><inist:fA14 i1="01"><s1>National Observatory of Athens, Lofos Nymfon</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
<sZ>9 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Lepine, J Cl" sort="Lepine, J Cl" uniqKey="Lepine J" first="J. Cl." last="Lepine">J. Cl. Lepine</name>
<affiliation><inist:fA14 i1="03"><s1>Laboratoire de Sismologie, Experimentale, Institut de Physique du Globe, 4 place Jussieu</s1>
<s2>75252 Paris</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
<sZ>10 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">Journal of volcanology and geothermal research</title>
<title level="j" type="abbreviated">J. volcanol. geotherm. res.</title>
<idno type="ISSN">0377-0273</idno>
<imprint><date when="2002">2002</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Journal of volcanology and geothermal research</title>
<title level="j" type="abbreviated">J. volcanol. geotherm. res.</title>
<idno type="ISSN">0377-0273</idno>
</seriesStmt>
</fileDesc>
<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>
<term>transport</term>
<term>volcanic arcs</term>
<term>volcanoes</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Hellénides</term>
<term>Iles Egée Grèce</term>
<term>Sismologie</term>
<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>
</keywords>
</textClass>
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</teiHeader>
<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>
</front>
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<fA05><s2>116</s2>
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<fA06><s2>1-2</s2>
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<fA08 i1="01" i2="1" l="ENG"><s1>Seismological and SAR signature of unrest at Nisyros caldera, Greece</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>SACHPAZI (M.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>KONTOES (Ch.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>VOULGARIS (N.)</s1>
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<fA11 i1="04" i2="1"><s1>LAIGLE (M.)</s1>
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<fA11 i1="05" i2="1"><s1>VOUGIOUKALAKIS (G.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>SIKIOTI (Olga)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>STAVRAKAKIS (G.)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>BASKOUTAS (J.)</s1>
</fA11>
<fA11 i1="09" i2="1"><s1>KALOGERAS (J.)</s1>
</fA11>
<fA11 i1="10" i2="1"><s1>LEPINE (J. Cl.)</s1>
</fA11>
<fA14 i1="01"><s1>National Observatory of Athens, Lofos Nymfon</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
<sZ>9 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Department of Geology and Geothermy, Panepistimioupoli</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Laboratoire de Sismologie, Experimentale, Institut de Physique du Globe, 4 place Jussieu</s1>
<s2>75252 Paris</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
<sZ>10 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Institute of Geological and Mineral Exploration, Mesogion 70</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA20><s1>19-33</s1>
<s7>1</s7>
</fA20>
<fA21><s1>2002</s1>
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</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>17236</s2>
<s5>354000104353950020</s5>
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<fA44><s0>0000</s0>
<s1>© 2002 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>1 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>02-0464838</s0>
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<fA60><s1>P</s1>
<s3>PR</s3>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of volcanology and geothermal research</s0>
</fA64>
<fA66 i1="01"><s0>NLD</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>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.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>222A01</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>225B03</s0>
</fC02>
<fC02 i1="03" i2="X"><s0>001E01F01</s0>
</fC02>
<fC02 i1="04" i2="X"><s0>001E01M03</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Hellénides</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>Hellenides</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Iles Egée Grèce</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>Greek Aegean Islands</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Islas Egeas Griegas</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Sismologie</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>seismology</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Arc volcanique</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>volcanic arcs</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Télédétection spatiale</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>Space remote sensing</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Teledetección espacial</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Radar antenne synthétique</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>synthetic aperture radar</s0>
<s5>06</s5>
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<fC03 i1="07" i2="2" l="FRE"><s0>Caldeira</s0>
<s5>07</s5>
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<fC03 i1="07" i2="2" l="ENG"><s0>calderas</s0>
<s5>07</s5>
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<fC03 i1="07" i2="2" l="SPA"><s0>Caldera</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Quaternaire</s0>
<s2>NX</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>Quaternary</s0>
<s2>NX</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Cuaternario</s0>
<s2>NX</s2>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Activité</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>activity</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Actividad</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Explosion</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>explosions</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Explosión</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Comportement</s0>
<s5>13</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>behavior</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Volcan</s0>
<s5>14</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>volcanoes</s0>
<s5>14</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Volcán</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Sismicité</s0>
<s5>15</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>seismicity</s0>
<s5>15</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Sismicidad</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Interférométrie</s0>
<s5>16</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>interferometry</s0>
<s5>16</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Interferometría</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Déformation</s0>
<s5>19</s5>
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<fC03 i1="15" i2="2" l="ENG"><s0>deformation</s0>
<s5>19</s5>
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<fC03 i1="16" i2="2" l="FRE"><s0>Chambre magmatique</s0>
<s5>22</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>magma chambers</s0>
<s5>22</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Cámara magmática</s0>
<s5>22</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Perspective</s0>
<s5>24</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>possibilities</s0>
<s5>24</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Perspectiva</s0>
<s5>24</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Intrusion</s0>
<s5>25</s5>
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<fC03 i1="18" i2="2" l="ENG"><s0>intrusions</s0>
<s5>25</s5>
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<fC03 i1="18" i2="2" l="SPA"><s0>Intrusión</s0>
<s5>25</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>ERS-2</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Ile Nisyros</s0>
<s4>INC</s4>
<s5>55</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Hypocentre</s0>
<s5>61</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>hypocenter</s0>
<s5>61</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Hipocentro</s0>
<s5>61</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Migration</s0>
<s5>62</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>migration</s0>
<s5>62</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Migración</s0>
<s5>62</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Magma</s0>
<s5>63</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>magmas</s0>
<s5>63</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>Magma</s0>
<s5>63</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Transport</s0>
<s5>64</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>transport</s0>
<s5>64</s5>
</fC03>
<fC03 i1="24" i2="2" l="SPA"><s0>Transporte</s0>
<s5>64</s5>
</fC03>
<fC06><s0>ILS</s0>
<s0>TA</s0>
</fC06>
<fC07 i1="01" i2="2" l="FRE"><s0>Grèce</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Greece</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Grecia</s0>
<s2>NG</s2>
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<fC07 i1="02" i2="2" l="FRE"><s0>Europe Sud</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Southern Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Europa Sur</s0>
<s2>NG</s2>
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<fC07 i1="03" i2="2" l="FRE"><s0>Europe</s0>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Europe</s0>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Europa</s0>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Phanérozoïque</s0>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Phanerozoic</s0>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Fanerozoico</s0>
</fC07>
<fN21><s1>273</s1>
</fN21>
<fN82><s1>PSI</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 02-0464838 INIST</NO>
<ET>Seismological and SAR signature of unrest at Nisyros caldera, Greece</ET>
<AU>SACHPAZI (M.); KONTOES (Ch.); VOULGARIS (N.); LAIGLE (M.); VOUGIOUKALAKIS (G.); SIKIOTI (Olga); STAVRAKAKIS (G.); BASKOUTAS (J.); KALOGERAS (J.); LEPINE (J. Cl.)</AU>
<AF>National Observatory of Athens, Lofos Nymfon/Athens/Grèce (1 aut., 2 aut., 6 aut., 7 aut., 8 aut., 9 aut.); Department of Geology and Geothermy, Panepistimioupoli/Athens/Grèce (3 aut.); Laboratoire de Sismologie, Experimentale, Institut de Physique du Globe, 4 place Jussieu/75252 Paris/France (4 aut., 10 aut.); Institute of Geological and Mineral Exploration, Mesogion 70/Athens/Grèce (5 aut.)</AF>
<DT>Publication en série; Papier de recherche; Niveau analytique</DT>
<SO>Journal of volcanology and geothermal research; ISSN 0377-0273; Coden JVGRDQ; Pays-Bas; Da. 2002; Vol. 116; No. 1-2; Pp. 19-33; Bibl. 1 p.1/4</SO>
<LA>Anglais</LA>
<EA>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.</EA>
<CC>222A01; 225B03; 001E01F01; 001E01M03</CC>
<FD>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</FD>
<FG>Grèce; Europe Sud; Europe; Cénozoïque; Phanérozoïque</FG>
<ED>Hellenides; Greek Aegean Islands; seismology; volcanic arcs; Space remote sensing; synthetic aperture radar; calderas; Quaternary; activity; explosions; behavior; volcanoes; seismicity; interferometry; deformation; magma chambers; possibilities; intrusions; hypocenter; migration; magmas; transport</ED>
<EG>Greece; Southern Europe; Europe; Cenozoic; Phanerozoic</EG>
<SD>Islas Egeas Griegas; Teledetección espacial; Caldera; Cuaternario; Actividad; Explosión; Volcán; Sismicidad; Interferometría; Cámara magmática; Perspectiva; Intrusión; Hipocentro; Migración; Magma; Transporte</SD>
<LO>INIST-17236.354000104353950020</LO>
<ID>02-0464838</ID>
</server>
</inist>
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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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