Ground deformation of Nisyros Volcano (Greece) for the period 1995-2002 : Results from DInSAR and DGPS observations
Identifieur interne : 000029 ( PascalFrancis/Checkpoint ); précédent : 000028; suivant : 000030Ground deformation of Nisyros Volcano (Greece) for the period 1995-2002 : Results from DInSAR and DGPS observations
Auteurs : E. Lagios [Grèce] ; V. Sakkas [Grèce] ; Is. Parcharidis [Grèce] ; V. Dietrich [Suisse]Source :
- Bulletin of volcanology [ 0258-8900 ] ; 2005.
Descripteurs français
- Pascal (Inist)
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- geographic : Grèce.
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Abstract
Differential GPS (DGPS) and Differential Interferometric Synthetic Aperture Radar (DInSAR) analyses were applied to the Kos-Yali-Nisyros Volcanic Field (SE Hellenic Volcanic Arc) to quantify the ground deformation of Nisyros Volcano. After intense seismic activity in 1996, a GPS network was installed in June 1997 and re-occupied annually up to 2002. A general uplift ranging from 14 to 140 mm was determined at all stations of the network. The corresponding horizontal displacements ranged from 13 to 53 mm. The displacement vectors indicate that the island is undergoing extension towards the East, West and South. A two-source "Mogi" model combined with assumed motion along the Mandraki Fault was constructed to fit the observed deformation. The best-fit model assumes sources at a depth of 5500 m NW of the centre of the island and at 6500 m offshore ESE of Yali Island. DInSAR analysis using four pairs of images taken between May 1995 and September 2000 suggests that deformation was occurring during 1995 before the start of the seismic crisis. An amplitude of at least 56 mm along the slant range appeared for the period 1996 through 1999. This deformation is consistent with the two-source model invoked in DGPS modelling. Surface evidence of ground deformation is expressed in the contemporaneous reactivation of the Mandraki Fault. In addition, a 600 m long N-S trending irregular rupture in the caldera floor was formed between 2001 and 2002. This rupture is interpreted as the release of surface stress in the consolidated epiclastic and hydrothermal sediments of the caldera floor.
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<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Ground deformation of Nisyros Volcano (Greece) for the period 1995-2002 : Results from DInSAR and DGPS observations</title><author><name sortKey="Lagios, E" sort="Lagios, E" uniqKey="Lagios E" first="E." last="Lagios">E. Lagios</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>157 84 Athens</wicri:noRegion></affiliation></author><author><name sortKey="Sakkas, V" sort="Sakkas, V" uniqKey="Sakkas V" first="V." last="Sakkas">V. Sakkas</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>157 84 Athens</wicri:noRegion></affiliation></author><author><name sortKey="Parcharidis, Is" sort="Parcharidis, Is" uniqKey="Parcharidis I" first="Is." last="Parcharidis">Is. Parcharidis</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>157 84 Athens</wicri:noRegion></affiliation></author><author><name sortKey="Dietrich, V" sort="Dietrich, V" uniqKey="Dietrich V" first="V." last="Dietrich">V. Dietrich</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Swiss Federal Institute of Technology, Institute of Mineralogy and Petrography, ETH-Zentrum</s1><s2>8092 Zurich</s2><s3>CHE</s3><sZ>4 aut.</sZ></inist:fA14><country>Suisse</country><wicri:noRegion>8092 Zurich</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">06-0130830</idno><date when="2005">2005</date><idno type="stanalyst">PASCAL 06-0130830 INIST</idno><idno type="RBID">Pascal:06-0130830</idno><idno type="wicri:Area/PascalFrancis/Corpus">000024</idno><idno type="wicri:Area/PascalFrancis/Curation">000016</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000029</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">000029</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Ground deformation of Nisyros Volcano (Greece) for the period 1995-2002 : Results from DInSAR and DGPS observations</title><author><name sortKey="Lagios, E" sort="Lagios, E" uniqKey="Lagios E" first="E." last="Lagios">E. Lagios</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>157 84 Athens</wicri:noRegion></affiliation></author><author><name sortKey="Sakkas, V" sort="Sakkas, V" uniqKey="Sakkas V" first="V." last="Sakkas">V. Sakkas</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>157 84 Athens</wicri:noRegion></affiliation></author><author><name sortKey="Parcharidis, Is" sort="Parcharidis, Is" uniqKey="Parcharidis I" first="Is." last="Parcharidis">Is. Parcharidis</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>157 84 Athens</wicri:noRegion></affiliation></author><author><name sortKey="Dietrich, V" sort="Dietrich, V" uniqKey="Dietrich V" first="V." last="Dietrich">V. Dietrich</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Swiss Federal Institute of Technology, Institute of Mineralogy and Petrography, ETH-Zentrum</s1><s2>8092 Zurich</s2><s3>CHE</s3><sZ>4 aut.</sZ></inist:fA14><country>Suisse</country><wicri:noRegion>8092 Zurich</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Bulletin of volcanology</title><title level="j" type="abbreviated">Bull. volcanol.</title><idno type="ISSN">0258-8900</idno><imprint><date when="2005">2005</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Bulletin of volcanology</title><title level="j" type="abbreviated">Bull. volcanol.</title><idno type="ISSN">0258-8900</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Global Positioning System</term><term>Greece</term><term>Kos</term><term>amplitude</term><term>calderas</term><term>deformation</term><term>depth</term><term>displacements</term><term>extension</term><term>faults</term><term>imagery</term><term>interferometry</term><term>models</term><term>networks</term><term>offshore</term><term>reactivation</term><term>rupture</term><term>stress</term><term>synthetic aperture radar</term><term>uplifts</term><term>volcanic arcs</term><term>volcanic fields</term><term>volcanoes</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Déformation</term><term>Volcan</term><term>Système GPS</term><term>Radar antenne synthétique</term><term>Champ volcanique</term><term>Arc volcanique</term><term>Réseau</term><term>Surrection</term><term>Déplacement</term><term>Extension</term><term>Modèle</term><term>Faille</term><term>Profondeur</term><term>Off shore</term><term>Amplitude</term><term>Réactivation</term><term>Rupture</term><term>Caldeira</term><term>Contrainte</term><term>Interférométrie</term><term>Imagerie</term><term>Grèce</term><term>Ile Cos</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Grèce</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Differential GPS (DGPS) and Differential Interferometric Synthetic Aperture Radar (DInSAR) analyses were applied to the Kos-Yali-Nisyros Volcanic Field (SE Hellenic Volcanic Arc) to quantify the ground deformation of Nisyros Volcano. After intense seismic activity in 1996, a GPS network was installed in June 1997 and re-occupied annually up to 2002. A general uplift ranging from 14 to 140 mm was determined at all stations of the network. The corresponding horizontal displacements ranged from 13 to 53 mm. The displacement vectors indicate that the island is undergoing extension towards the East, West and South. A two-source "Mogi" model combined with assumed motion along the Mandraki Fault was constructed to fit the observed deformation. The best-fit model assumes sources at a depth of 5500 m NW of the centre of the island and at 6500 m offshore ESE of Yali Island. DInSAR analysis using four pairs of images taken between May 1995 and September 2000 suggests that deformation was occurring during 1995 before the start of the seismic crisis. An amplitude of at least 56 mm along the slant range appeared for the period 1996 through 1999. This deformation is consistent with the two-source model invoked in DGPS modelling. Surface evidence of ground deformation is expressed in the contemporaneous reactivation of the Mandraki Fault. In addition, a 600 m long N-S trending irregular rupture in the caldera floor was formed between 2001 and 2002. This rupture is interpreted as the release of surface stress in the consolidated epiclastic and hydrothermal sediments of the caldera floor.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0258-8900</s0></fA01><fA02 i1="01"><s0>BUVOEW</s0></fA02><fA03 i2="1"><s0>Bull. volcanol.</s0></fA03><fA05><s2>68</s2></fA05><fA06><s2>2</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Ground deformation of Nisyros Volcano (Greece) for the period 1995-2002 : Results from DInSAR and DGPS observations</s1></fA08><fA11 i1="01" i2="1"><s1>LAGIOS (E.)</s1></fA11><fA11 i1="02" i2="1"><s1>SAKKAS (V.)</s1></fA11><fA11 i1="03" i2="1"><s1>PARCHARIDIS (Is.)</s1></fA11><fA11 i1="04" i2="1"><s1>DIETRICH (V.)</s1></fA11><fA14 i1="01"><s1>Space Applications Research Unit in Geosciences, Laboratory of Geophysics, Department of Geophysics & Geothermics, National Kapodistrian University of Athens, Panepistimiopolis-Ilissia</s1><s2>157 84 Athens</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></fA14><fA14 i1="02"><s1>Swiss Federal Institute of Technology, Institute of Mineralogy and Petrography, ETH-Zentrum</s1><s2>8092 Zurich</s2><s3>CHE</s3><sZ>4 aut.</sZ></fA14><fA20><s1>201-214</s1></fA20><fA21><s1>2005</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>2715</s2><s5>354000135735980070</s5></fA43><fA44><s0>0000</s0><s1>© 2006 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>1 p.1/4</s0></fA45><fA47 i1="01" i2="1"><s0>06-0130830</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Bulletin of volcanology</s0></fA64><fA66 i1="01"><s0>DEU</s0></fA66><fC01 i1="01" l="ENG"><s0>Differential GPS (DGPS) and Differential Interferometric Synthetic Aperture Radar (DInSAR) analyses were applied to the Kos-Yali-Nisyros Volcanic Field (SE Hellenic Volcanic Arc) to quantify the ground deformation of Nisyros Volcano. After intense seismic activity in 1996, a GPS network was installed in June 1997 and re-occupied annually up to 2002. A general uplift ranging from 14 to 140 mm was determined at all stations of the network. The corresponding horizontal displacements ranged from 13 to 53 mm. The displacement vectors indicate that the island is undergoing extension towards the East, West and South. A two-source "Mogi" model combined with assumed motion along the Mandraki Fault was constructed to fit the observed deformation. The best-fit model assumes sources at a depth of 5500 m NW of the centre of the island and at 6500 m offshore ESE of Yali Island. DInSAR analysis using four pairs of images taken between May 1995 and September 2000 suggests that deformation was occurring during 1995 before the start of the seismic crisis. An amplitude of at least 56 mm along the slant range appeared for the period 1996 through 1999. This deformation is consistent with the two-source model invoked in DGPS modelling. Surface evidence of ground deformation is expressed in the contemporaneous reactivation of the Mandraki Fault. In addition, a 600 m long N-S trending irregular rupture in the caldera floor was formed between 2001 and 2002. This rupture is interpreted as the release of surface stress in the consolidated epiclastic and hydrothermal sediments of the caldera floor.</s0></fC01><fC02 i1="01" i2="2"><s0>222A01</s0></fC02><fC02 i1="02" i2="2"><s0>226B02</s0></fC02><fC02 i1="03" i2="2"><s0>001E01F01</s0></fC02><fC02 i1="04" i2="2"><s0>001E01O02</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Déformation</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>deformation</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Volcan</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>volcanoes</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Volcán</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Système GPS</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>Global Positioning System</s0><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Radar antenne synthétique</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>synthetic aperture radar</s0><s5>04</s5></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Champ 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