Inflation/deflation sequence on Nisyros Active Volcano (Greece) during 1995-2000 issued from SAR differential interferometry
Identifieur interne :
000007 ( PascalFrancis/Curation );
précédent :
000006;
suivant :
000008
Inflation/deflation sequence on Nisyros Active Volcano (Greece) during 1995-2000 issued from SAR differential interferometry
Auteurs : Olga Sykioti [
Grèce] ;
Charalabos Kontoes [
Grèce] ;
Panagiotis Elias [
Grèce] ;
Pierre Briole [
France] ;
Maria Sachpazi [
Grèce] ;
Dimitris Paradissis [
Grèce] ;
Ioannis Kotsis [
Grèce]
Source :
-
SPIE proceedings series [ 1017-2653 ] ; 2003.
RBID : Pascal:03-0482836
Descripteurs français
English descriptors
Abstract
Nisyros is a poorly known Quaternary volcano, south-east of the Aegean volcanic arc. It is characterized by periods of intense seismic activity and paucity in eruptive episodes, sometimes accompanied by hydrothermal explosions. The most recent unrest episode lasted from 1995 to 1998, without eruption. Radar interferometry has been applied in order to study the evolution of the deformation from 1995 to 2000. Observations show a continuous uplift of 140mm during 1995-1997. At mid 1998, the movement trend changes into a slower surface deflation till 2000. Maximum crust deformation is constantly observed at the north-west part of the island, where most earthquake epicenters are located and in agreement to three GPS campaigns conducted between mid 1997 and mid 1998. We solve for the best-fit Mogi point source and best-fit Okada rectangular dislocation of the observed deformation field. Mogi model indicates a source at 5km depth beneath the north-west edge of the island, with a maximum deformation amplitude at surface of 0.14± 0.02m and a total volume change of 26± 4 x 106m3, during 1995-1997. The Okada model indicates a dike solution 2km long, 2.2km wide, with a 4m opening and a 30° dip. The upper center is at 6.4km depth and the volume change, also during 1995-1997, is 17.6 x 106 m3. Each solution is discussed on the potential controlling mechanism resulting to the volcano's inflation/deflation sequence.
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| A08 | 01 | 1 | ENG | @1 Inflation/deflation sequence on Nisyros Active Volcano (Greece) during 1995-2000 issued from SAR differential interferometry |
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| A09 | 01 | 1 | ENG | @1 Remote sensing for environmental monitoring, GIS applications, and geology II : Agia Pelagia, 23-26 September 2002 |
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| A11 | 01 | 1 | | @1 SYKIOTI (Olga) |
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| A11 | 02 | 1 | | @1 KONTOES (Charalabos) |
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| A11 | 03 | 1 | | @1 ELIAS (Panagiotis) |
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| A11 | 04 | 1 | | @1 BRIOLE (Pierre) |
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| A11 | 05 | 1 | | @1 SACHPAZI (Maria) |
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| A11 | 06 | 1 | | @1 PARADISSIS (Dimitris) |
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| A11 | 07 | 1 | | @1 KOTSIS (Ioannis) |
|---|
| A12 | 01 | 1 | | @1 EHLERS (Manfred) @9 ed. |
|---|
| A14 | 01 | | | @1 Institute for Space Applications and Remote Sensing, National Observatory of Athens @3 GRC @Z 1 aut. @Z 2 aut. @Z 3 aut. |
|---|
| A14 | 02 | | | @1 UMR-CNRS 7580, Département de Sismologie, Institut de Physique du Globe de París (IPGP) @3 FRA @Z 4 aut. |
|---|
| A14 | 03 | | | @1 Institute for Geodynamics, National Observatory of Athens @3 GRC @Z 5 aut. |
|---|
| A14 | 04 | | | @1 National Technical University of Athens, Department of Surveying Engineering, Dionysos Satellite Observatory @3 GRC @Z 6 aut. @Z 7 aut. |
|---|
| A18 | 01 | 1 | | @1 International Society for Optical Engineering @2 Bellingham WA @3 USA @9 patr. |
|---|
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| A44 | | | | @0 0000 @1 © 2003 INIST-CNRS. All rights reserved. |
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| A45 | | | | @0 17 ref. |
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| A47 | 01 | 1 | | @0 03-0482836 |
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| A60 | | | | @1 P @2 C |
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| A61 | | | | @0 A |
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| A64 | 01 | 1 | | @0 SPIE proceedings series |
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| C01 | 01 | | ENG | @0 Nisyros is a poorly known Quaternary volcano, south-east of the Aegean volcanic arc. It is characterized by periods of intense seismic activity and paucity in eruptive episodes, sometimes accompanied by hydrothermal explosions. The most recent unrest episode lasted from 1995 to 1998, without eruption. Radar interferometry has been applied in order to study the evolution of the deformation from 1995 to 2000. Observations show a continuous uplift of 140mm during 1995-1997. At mid 1998, the movement trend changes into a slower surface deflation till 2000. Maximum crust deformation is constantly observed at the north-west part of the island, where most earthquake epicenters are located and in agreement to three GPS campaigns conducted between mid 1997 and mid 1998. We solve for the best-fit Mogi point source and best-fit Okada rectangular dislocation of the observed deformation field. Mogi model indicates a source at 5km depth beneath the north-west edge of the island, with a maximum deformation amplitude at surface of 0.14± 0.02m and a total volume change of 26± 4 x 106m3, during 1995-1997. The Okada model indicates a dike solution 2km long, 2.2km wide, with a 4m opening and a 30° dip. The upper center is at 6.4km depth and the volume change, also during 1995-1997, is 17.6 x 106 m3. Each solution is discussed on the potential controlling mechanism resulting to the volcano's inflation/deflation sequence. |
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| C02 | 01 | 3 | | @0 001B00G60L |
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| C02 | 02 | X | | @0 001E02G |
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| C03 | 01 | 3 | FRE | @0 Modélisation @5 01 |
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| C03 | 01 | 3 | ENG | @0 Modelling @5 01 |
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| C03 | 02 | 3 | FRE | @0 Télédétection @5 02 |
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| C03 | 02 | 3 | ENG | @0 Remote sensing @5 02 |
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| C03 | 03 | 3 | FRE | @0 Volcanisme @5 03 |
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| C03 | 03 | 3 | ENG | @0 Volcanism @5 03 |
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| C03 | 04 | 3 | FRE | @0 Radar ouverture synthétique @5 04 |
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| C03 | 04 | 3 | ENG | @0 Synthetic-aperture radar @5 04 |
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| C03 | 05 | 3 | FRE | @0 Grèce @2 NG @5 05 |
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| C03 | 05 | 3 | ENG | @0 Greece @2 NG @5 05 |
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| C03 | 06 | 3 | FRE | @0 Imagerie radar @5 06 |
|---|
| C03 | 06 | 3 | ENG | @0 Radar imaging @5 06 |
|---|
| C03 | 07 | 3 | FRE | @0 Analyse donnée @5 07 |
|---|
| C03 | 07 | 3 | ENG | @0 Data analysis @5 07 |
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| C03 | 08 | X | FRE | @0 Observation interférométrique @5 08 |
|---|
| C03 | 08 | X | ENG | @0 Interferometric observation @5 08 |
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| C03 | 08 | X | SPA | @0 Observación interferométrica @5 08 |
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| C03 | 09 | 3 | FRE | @0 Volcan actif Nisyros @4 INC @5 82 |
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| N21 | | | | @1 328 |
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| N82 | | | | @1 PSI |
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| pR |
| A30 | 01 | 1 | ENG | @1 Remote sensing for environmental monitoring, GIS applications, and geology. Conference @2 2 @3 Agia Pelagia GRC @4 2002-09-23 |
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Le document en format XML
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<sZ>1 aut.</sZ>
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<sZ>3 aut.</sZ>
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</affiliation><author><name sortKey="Elias, Panagiotis" sort="Elias, Panagiotis" uniqKey="Elias P" first="Panagiotis" last="Elias">Panagiotis Elias</name>
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<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
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</affiliation><author><name sortKey="Briole, Pierre" sort="Briole, Pierre" uniqKey="Briole P" first="Pierre" last="Briole">Pierre Briole</name>
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<s3>FRA</s3>
<sZ>4 aut.</sZ>
</inist:fA14><country>France</country>
</affiliation><author><name sortKey="Sachpazi, Maria" sort="Sachpazi, Maria" uniqKey="Sachpazi M" first="Maria" last="Sachpazi">Maria Sachpazi</name>
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<sZ>7 aut.</sZ>
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<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14><country>Grèce</country>
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</imprint><seriesStmt><title level="j" type="main">SPIE proceedings series</title>
<idno type="ISSN">1017-2653</idno>
</seriesStmt><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Data analysis</term>
<term>Greece</term>
<term>Interferometric observation</term>
<term>Modelling</term>
<term>Radar imaging</term>
<term>Remote sensing</term>
<term>Synthetic-aperture radar</term>
<term>Volcanism</term>
</keywords><keywords scheme="Pascal" xml:lang="fr"><term>Modélisation</term>
<term>Télédétection</term>
<term>Volcanisme</term>
<term>Radar ouverture synthétique</term>
<term>Grèce</term>
<term>Imagerie radar</term>
<term>Analyse donnée</term>
<term>Observation interférométrique</term>
<term>Volcan actif Nisyros</term>
</keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Grèce</term>
</keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Télédétection</term>
</keywords><front><div type="abstract" xml:lang="en">Nisyros is a poorly known Quaternary volcano, south-east of the Aegean volcanic arc. It is characterized by periods of intense seismic activity and paucity in eruptive episodes, sometimes accompanied by hydrothermal explosions. The most recent unrest episode lasted from 1995 to 1998, without eruption. Radar interferometry has been applied in order to study the evolution of the deformation from 1995 to 2000. Observations show a continuous uplift of 140mm during 1995-1997. At mid 1998, the movement trend changes into a slower surface deflation till 2000. Maximum crust deformation is constantly observed at the north-west part of the island, where most earthquake epicenters are located and in agreement to three GPS campaigns conducted between mid 1997 and mid 1998. We solve for the best-fit Mogi point source and best-fit Okada rectangular dislocation of the observed deformation field. Mogi model indicates a source at 5km depth beneath the north-west edge of the island, with a maximum deformation amplitude at surface of 0.14± 0.02m and a total volume change of 26± 4 x 10<sup>6</sup>
m<sup>3</sup>
, during 1995-1997. The Okada model indicates a dike solution 2km long, 2.2km wide, with a 4m opening and a 30° dip. The upper center is at 6.4km depth and the volume change, also during 1995-1997, is 17.6 x 10<sup>6</sup>
m<sup>3</sup>
. Each solution is discussed on the potential controlling mechanism resulting to the volcano's inflation/deflation sequence.</div><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1017-2653</s0>
</fA01><fA05><s2>4886</s2>
</fA05><fA08 i1="01" i2="1" l="ENG"><s1>Inflation/deflation sequence on Nisyros Active Volcano (Greece) during 1995-2000 issued from SAR differential interferometry</s1>
</fA08><fA09 i1="01" i2="1" l="ENG"><s1>Remote sensing for environmental monitoring, GIS applications, and geology II : Agia Pelagia, 23-26 September 2002</s1>
</fA09><fA11 i1="01" i2="1"><s1>SYKIOTI (Olga)</s1>
</fA11><fA11 i1="02" i2="1"><s1>KONTOES (Charalabos)</s1>
</fA11><fA11 i1="03" i2="1"><s1>ELIAS (Panagiotis)</s1>
</fA11><fA11 i1="04" i2="1"><s1>BRIOLE (Pierre)</s1>
</fA11><fA11 i1="05" i2="1"><s1>SACHPAZI (Maria)</s1>
</fA11><fA11 i1="06" i2="1"><s1>PARADISSIS (Dimitris)</s1>
</fA11><fA11 i1="07" i2="1"><s1>KOTSIS (Ioannis)</s1>
</fA11><fA12 i1="01" i2="1"><s1>EHLERS (Manfred)</s1>
<s9>ed.</s9>
</fA12><fA14 i1="01"><s1>Institute for Space Applications and Remote Sensing, National Observatory of Athens</s1>
<s3>GRC</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14><fA14 i1="02"><s1>UMR-CNRS 7580, Département de Sismologie, Institut de Physique du Globe de París (IPGP)</s1>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
</fA14><fA14 i1="03"><s1>Institute for Geodynamics, National Observatory of Athens</s1>
<s3>GRC</s3>
<sZ>5 aut.</sZ>
</fA14><fA14 i1="04"><s1>National Technical University of Athens, Department of Surveying Engineering, Dionysos Satellite Observatory</s1>
<s3>GRC</s3>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14><fA18 i1="01" i2="1"><s1>International Society for Optical Engineering</s1>
<s2>Bellingham WA</s2>
<s3>USA</s3>
<s9>patr.</s9>
</fA18><fA20><s1>315-321</s1>
</fA20><fA21><s1>2003</s1>
</fA21><fA23 i1="01"><s0>ENG</s0>
</fA23><fA26 i1="01"><s0>0-8194-4668-8</s0>
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<s2>21760</s2>
<s5>354000117379140330</s5>
</fA43><fA44><s0>0000</s0>
<s1>© 2003 INIST-CNRS. All rights reserved.</s1>
</fA44><fA45><s0>17 ref.</s0>
</fA45><fA47 i1="01" i2="1"><s0>03-0482836</s0>
</fA47><fA60><s1>P</s1>
<s2>C</s2>
</fA60><fA64 i1="01" i2="1"><s0>SPIE proceedings series</s0>
</fA64><fA66 i1="01"><s0>USA</s0>
</fA66><fC01 i1="01" l="ENG"><s0>Nisyros is a poorly known Quaternary volcano, south-east of the Aegean volcanic arc. It is characterized by periods of intense seismic activity and paucity in eruptive episodes, sometimes accompanied by hydrothermal explosions. The most recent unrest episode lasted from 1995 to 1998, without eruption. Radar interferometry has been applied in order to study the evolution of the deformation from 1995 to 2000. Observations show a continuous uplift of 140mm during 1995-1997. At mid 1998, the movement trend changes into a slower surface deflation till 2000. Maximum crust deformation is constantly observed at the north-west part of the island, where most earthquake epicenters are located and in agreement to three GPS campaigns conducted between mid 1997 and mid 1998. We solve for the best-fit Mogi point source and best-fit Okada rectangular dislocation of the observed deformation field. Mogi model indicates a source at 5km depth beneath the north-west edge of the island, with a maximum deformation amplitude at surface of 0.14± 0.02m and a total volume change of 26± 4 x 10<sup>6</sup>
m<sup>3</sup>
, during 1995-1997. The Okada model indicates a dike solution 2km long, 2.2km wide, with a 4m opening and a 30° dip. The upper center is at 6.4km depth and the volume change, also during 1995-1997, is 17.6 x 10<sup>6</sup>
m<sup>3</sup>
. Each solution is discussed on the potential controlling mechanism resulting to the volcano's inflation/deflation sequence.</s0><fC02 i1="01" i2="3"><s0>001B00G60L</s0>
</fC02><fC02 i1="02" i2="X"><s0>001E02G</s0>
</fC02><fC03 i1="01" i2="3" l="FRE"><s0>Modélisation</s0>
<s5>01</s5>
</fC03><fC03 i1="01" i2="3" l="ENG"><s0>Modelling</s0>
<s5>01</s5>
</fC03><fC03 i1="02" i2="3" l="FRE"><s0>Télédétection</s0>
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<s5>03</s5>
</fC03><fC03 i1="03" i2="3" l="ENG"><s0>Volcanism</s0>
<s5>03</s5>
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<s5>04</s5>
</fC03><fC03 i1="04" i2="3" l="ENG"><s0>Synthetic-aperture radar</s0>
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<s2>NG</s2>
<s5>05</s5>
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<s2>NG</s2>
<s5>05</s5>
</fC03><fC03 i1="06" i2="3" l="FRE"><s0>Imagerie radar</s0>
<s5>06</s5>
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<s5>06</s5>
</fC03><fC03 i1="07" i2="3" l="FRE"><s0>Analyse donnée</s0>
<s5>07</s5>
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<s5>07</s5>
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<s5>08</s5>
</fC03><fC03 i1="08" i2="X" l="SPA"><s0>Observación interferométrica</s0>
<s5>08</s5>
</fC03><fC03 i1="09" i2="3" l="FRE"><s0>Volcan actif Nisyros</s0>
<s4>INC</s4>
<s5>82</s5>
</fC03><fN21><s1>328</s1>
</fN21><fN82><s1>PSI</s1>
</fN82><pR><fA30 i1="01" i2="1" l="ENG"><s1>Remote sensing for environmental monitoring, GIS applications, and geology. Conference</s1>
<s2>2</s2>
<s3>Agia Pelagia GRC</s3>
<s4>2002-09-23</s4>
</fA30>
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|texte= Inflation/deflation sequence on Nisyros Active Volcano (Greece) during 1995-2000 issued from SAR differential interferometry
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