NissirosV1, PascalFrancis, Corpus, bibRecord, 000036

Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)

Identifieur interne : 000036 ( PascalFrancis/Corpus ); précédent : 000035; suivant : 000037

Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)

Auteurs : Giovanni Chiodini ; Tatjana Brombach ; Stefano Caliro ; Carlo Cardellini ; Luigi Marini ; Volker Dietrich

Source :

Geophysical research letters [ 0094-8276 ] ; 2002.

RBID : Pascal:03-0063631

Descripteurs français

Pascal (Inist)
- Iles Egée Grèce, Gaz, Volcanisme, Analyse chimique, Fumerolle, Dioxyde carbone, Gaz hydrogène sulfuré, Rapport chimique, Méthane, Activité hydrothermale, Hydrogène, Monoxyde carbone, Condition pression température, Risque volcanique, Eruption, Phénomène précurseur, Ile Nisyros, Gaz volcanique, Fluide magmatique, Système hydrothermal.

English descriptors

KwdEn :
- Greek Aegean Islands, P-T conditions, carbon dioxide, carbon monoxide, chemical analysis, chemical ratios, eruptions, fumaroles, gases, hydrogen, hydrogen sulfide gas, hydrothermal activity, methane, precursors, volcanic risk, volcanism.

Abstract

Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997-2001, following a strong seismic crisis. Increasing H₂S/CO₂ ratios and decreasing CH₄/CO₂ ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H₂ and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 0094-8276`
A02	`01`			`@0 GPRLAJ`
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A05				`@2 29`
A06				`@2 16`
A08	`01`	`1`	`ENG`	`@1 Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)`
A11	`01`	`1`		`@1 CHIODINI (Giovanni)`
A11	`02`	`1`		`@1 BROMBACH (Tatjana)`
A11	`03`	`1`		`@1 CALIRO (Stefano)`
A11	`04`	`1`		`@1 CARDELLINI (Carlo)`
A11	`05`	`1`		`@1 MARINI (Luigi)`
A11	`06`	`1`		`@1 DIETRICH (Volker)`
A14	`01`			`@1 Osservatorio Vesuviano INGV @2 Napoli @3 ITA @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut.`
A14	`02`			`@1 Dip.Te.Ris., University di Geneva @3 ITA @Z 5 aut.`
A14	`03`			`@1 Institute of Mineralogy and Petrography, ETH-Zürich @3 CHE @Z 6 aut.`
A20				`@2 6.1-5.4`
A21				`@1 2002`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 16687 @5 354000105605150060`
A44				`@0 0000 @1 © 2003 INIST-CNRS. All rights reserved.`
A45				`@0 17 ref.`
A47	`01`	`1`		`@0 03-0063631`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Geophysical research letters`
A66	`01`			`@0 USA`
C01	`01`		`ENG`	@0 Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997-2001, following a strong seismic crisis. Increasing H₂S/CO₂ ratios and decreasing CH₄/CO₂ ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H₂ and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.
C02	`01`	`2`		`@0 222A01`
C02	`02`	`2`		`@0 220B03`
C02	`03`	`X`		`@0 001E01F01`
C02	`04`	`X`		`@0 001E01B03`
C03	`01`	`2`	`FRE`	`@0 Iles Egée Grèce @2 NG @5 01`
C03	`01`	`2`	`ENG`	`@0 Greek Aegean Islands @2 NG @5 01`
C03	`01`	`2`	`SPA`	`@0 Islas Egeas Griegas @2 NG @5 01`
C03	`02`	`2`	`FRE`	`@0 Gaz @5 02`
C03	`02`	`2`	`ENG`	`@0 gases @5 02`
C03	`02`	`2`	`SPA`	`@0 Gas @5 02`
C03	`03`	`2`	`FRE`	`@0 Volcanisme @5 03`
C03	`03`	`2`	`ENG`	`@0 volcanism @5 03`
C03	`04`	`2`	`FRE`	`@0 Analyse chimique @5 04`
C03	`04`	`2`	`ENG`	`@0 chemical analysis @5 04`
C03	`04`	`2`	`SPA`	`@0 Análisis químico @5 04`
C03	`05`	`2`	`FRE`	`@0 Fumerolle @5 05`
C03	`05`	`2`	`ENG`	`@0 fumaroles @5 05`
C03	`05`	`2`	`SPA`	`@0 Fumarola @5 05`
C03	`06`	`2`	`FRE`	`@0 Dioxyde carbone @5 06`
C03	`06`	`2`	`ENG`	`@0 carbon dioxide @5 06`
C03	`07`	`2`	`FRE`	`@0 Gaz hydrogène sulfuré @5 07`
C03	`07`	`2`	`ENG`	`@0 hydrogen sulfide gas @5 07`
C03	`07`	`2`	`SPA`	`@0 Gas sulfhídrico @5 07`
C03	`08`	`2`	`FRE`	`@0 Rapport chimique @5 08`
C03	`08`	`2`	`ENG`	`@0 chemical ratios @5 08`
C03	`08`	`2`	`SPA`	`@0 Relación química @5 08`
C03	`09`	`2`	`FRE`	`@0 Méthane @5 09`
C03	`09`	`2`	`ENG`	`@0 methane @5 09`
C03	`09`	`2`	`SPA`	`@0 Metano @5 09`
C03	`10`	`2`	`FRE`	`@0 Activité hydrothermale @5 10`
C03	`10`	`2`	`ENG`	`@0 hydrothermal activity @5 10`
C03	`11`	`2`	`FRE`	`@0 Hydrogène @5 11`
C03	`11`	`2`	`ENG`	`@0 hydrogen @5 11`
C03	`11`	`2`	`SPA`	`@0 Hidrógeno @5 11`
C03	`12`	`2`	`FRE`	`@0 Monoxyde carbone @5 12`
C03	`12`	`2`	`ENG`	`@0 carbon monoxide @5 12`
C03	`13`	`2`	`FRE`	`@0 Condition pression température @5 13`
C03	`13`	`2`	`ENG`	`@0 P-T conditions @5 13`
C03	`13`	`2`	`SPA`	`@0 Condición PT @5 13`
C03	`14`	`2`	`FRE`	`@0 Risque volcanique @5 14`
C03	`14`	`2`	`ENG`	`@0 volcanic risk @5 14`
C03	`15`	`2`	`FRE`	`@0 Eruption @5 15`
C03	`15`	`2`	`ENG`	`@0 eruptions @5 15`
C03	`15`	`2`	`SPA`	`@0 Erupción @5 15`
C03	`16`	`2`	`FRE`	`@0 Phénomène précurseur @5 16`
C03	`16`	`2`	`ENG`	`@0 precursors @5 16`
C03	`16`	`2`	`SPA`	`@0 Fenómeno precursor @5 16`
C03	`17`	`2`	`FRE`	`@0 Ile Nisyros @4 INC @5 52`
C03	`18`	`2`	`FRE`	`@0 Gaz volcanique @4 INC @5 53`
C03	`19`	`2`	`FRE`	`@0 Fluide magmatique @4 INC @5 54`
C03	`20`	`2`	`FRE`	`@0 Système hydrothermal @4 INC @5 55`
C06				`@0 ILS`
C07	`01`	`2`	`FRE`	`@0 Grèce @2 NG`
C07	`01`	`2`	`ENG`	`@0 Greece @2 NG`
C07	`01`	`2`	`SPA`	`@0 Grecia @2 NG`
C07	`02`	`2`	`FRE`	`@0 Europe Sud @2 NG`
C07	`02`	`2`	`ENG`	`@0 Southern Europe @2 NG`
C07	`02`	`2`	`SPA`	`@0 Europa Sur @2 NG`
C07	`03`	`2`	`FRE`	`@0 Europe`
C07	`03`	`2`	`ENG`	`@0 Europe`
C07	`03`	`2`	`SPA`	`@0 Europa`
N21				`@1 034`
N82				`@1 PSI`

Format Inist (serveur)

NO :	PASCAL 03-0063631 INIST
ET :	Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)
AU :	CHIODINI (Giovanni); BROMBACH (Tatjana); CALIRO (Stefano); CARDELLINI (Carlo); MARINI (Luigi); DIETRICH (Volker)
AF :	Osservatorio Vesuviano INGV/Napoli/Italie (1 aut., 2 aut., 3 aut., 4 aut.); Dip.Te.Ris., University di Geneva/Italie (5 aut.); Institute of Mineralogy and Petrography, ETH-Zürich/Suisse (6 aut.)
DT :	Publication en série; Niveau analytique
SO :	Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 2002; Vol. 29; No. 16; 6.1-5.4; Bibl. 17 ref.
LA :	Anglais
EA :	Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997-2001, following a strong seismic crisis. Increasing H₂S/CO₂ ratios and decreasing CH₄/CO₂ ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H₂ and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.
CC :	222A01; 220B03; 001E01F01; 001E01B03
FD :	Iles Egée Grèce; Gaz; Volcanisme; Analyse chimique; Fumerolle; Dioxyde carbone; Gaz hydrogène sulfuré; Rapport chimique; Méthane; Activité hydrothermale; Hydrogène; Monoxyde carbone; Condition pression température; Risque volcanique; Eruption; Phénomène précurseur; Ile Nisyros; Gaz volcanique; Fluide magmatique; Système hydrothermal
FG :	Grèce; Europe Sud; Europe
ED :	Greek Aegean Islands; gases; volcanism; chemical analysis; fumaroles; carbon dioxide; hydrogen sulfide gas; chemical ratios; methane; hydrothermal activity; hydrogen; carbon monoxide; P-T conditions; volcanic risk; eruptions; precursors
EG :	Greece; Southern Europe; Europe
SD :	Islas Egeas Griegas; Gas; Análisis químico; Fumarola; Gas sulfhídrico; Relación química; Metano; Hidrógeno; Condición PT; Erupción; Fenómeno precursor
LO :	INIST-16687.354000105605150060
ID :	03-0063631

Links to Exploration step

Pascal:03-0063631

Le document en format XML

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<author><name sortKey="Caliro, Stefano" sort="Caliro, Stefano" uniqKey="Caliro S" first="Stefano" last="Caliro">Stefano Caliro</name>
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<author><name sortKey="Cardellini, Carlo" sort="Cardellini, Carlo" uniqKey="Cardellini C" first="Carlo" last="Cardellini">Carlo Cardellini</name>
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<author><name sortKey="Dietrich, Volker" sort="Dietrich, Volker" uniqKey="Dietrich V" first="Volker" last="Dietrich">Volker Dietrich</name>
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<front><div type="abstract" xml:lang="en">Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997-2001, following a strong seismic crisis. Increasing H<sub>2</sub>
S/CO<sub>2</sub>
 ratios and decreasing CH<sub>4</sub>
/CO<sub>2</sub>
 ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H<sub>2</sub>
 and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.</div>
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<fA11 i1="01" i2="1"><s1>CHIODINI (Giovanni)</s1>
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<fA14 i1="02"><s1>Dip.Te.Ris., University di Geneva</s1>
<s3>ITA</s3>
<sZ>5 aut.</sZ>
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<fA14 i1="03"><s1>Institute of Mineralogy and Petrography, ETH-Zürich</s1>
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<fC01 i1="01" l="ENG"><s0>Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997-2001, following a strong seismic crisis. Increasing H<sub>2</sub>
S/CO<sub>2</sub>
 ratios and decreasing CH<sub>4</sub>
/CO<sub>2</sub>
 ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H<sub>2</sub>
 and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.</s0>
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</fC02>
<fC02 i1="03" i2="X"><s0>001E01F01</s0>
</fC02>
<fC02 i1="04" i2="X"><s0>001E01B03</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Iles Egée Grèce</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>Greek Aegean Islands</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Islas Egeas Griegas</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Gaz</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>gases</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Gas</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Volcanisme</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>volcanism</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Analyse chimique</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>chemical analysis</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Análisis químico</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Fumerolle</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>fumaroles</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Fumarola</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Dioxyde carbone</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>carbon dioxide</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Gaz hydrogène sulfuré</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>hydrogen sulfide gas</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Gas sulfhídrico</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Rapport chimique</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>chemical ratios</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Relación química</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Méthane</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>methane</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Metano</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Activité hydrothermale</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>hydrothermal activity</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Hydrogène</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>hydrogen</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Hidrógeno</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Monoxyde carbone</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>carbon monoxide</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Condition pression température</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>P-T conditions</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Condición PT</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Risque volcanique</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>volcanic risk</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Eruption</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>eruptions</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Erupción</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Phénomène précurseur</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>precursors</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Fenómeno precursor</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Ile Nisyros</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Gaz volcanique</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Fluide magmatique</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Système hydrothermal</s0>
<s4>INC</s4>
<s5>55</s5>
</fC03>
<fC06><s0>ILS</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>
</fC07>
<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>
</fC07>
<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>
<fN21><s1>034</s1>
</fN21>
<fN82><s1>PSI</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 03-0063631 INIST</NO>
<ET>Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)</ET>
<AU>CHIODINI (Giovanni); BROMBACH (Tatjana); CALIRO (Stefano); CARDELLINI (Carlo); MARINI (Luigi); DIETRICH (Volker)</AU>
<AF>Osservatorio Vesuviano INGV/Napoli/Italie (1 aut., 2 aut., 3 aut., 4 aut.); Dip.Te.Ris., University di Geneva/Italie (5 aut.); Institute of Mineralogy and Petrography, ETH-Zürich/Suisse (6 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 2002; Vol. 29; No. 16; 6.1-5.4; Bibl. 17 ref.</SO>
<LA>Anglais</LA>
<EA>Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997-2001, following a strong seismic crisis. Increasing H<sub>2</sub>
S/CO<sub>2</sub>
 ratios and decreasing CH<sub>4</sub>
/CO<sub>2</sub>
 ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H<sub>2</sub>
 and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.</EA>
<CC>222A01; 220B03; 001E01F01; 001E01B03</CC>
<FD>Iles Egée Grèce; Gaz; Volcanisme; Analyse chimique; Fumerolle; Dioxyde carbone; Gaz hydrogène sulfuré; Rapport chimique; Méthane; Activité hydrothermale; Hydrogène; Monoxyde carbone; Condition pression température; Risque volcanique; Eruption; Phénomène précurseur; Ile Nisyros; Gaz volcanique; Fluide magmatique; Système hydrothermal</FD>
<FG>Grèce; Europe Sud; Europe</FG>
<ED>Greek Aegean Islands; gases; volcanism; chemical analysis; fumaroles; carbon dioxide; hydrogen sulfide gas; chemical ratios; methane; hydrothermal activity; hydrogen; carbon monoxide; P-T conditions; volcanic risk; eruptions; precursors</ED>
<EG>Greece; Southern Europe; Europe</EG>
<SD>Islas Egeas Griegas; Gas; Análisis químico; Fumarola; Gas sulfhídrico; Relación química; Metano; Hidrógeno; Condición PT; Erupción; Fenómeno precursor</SD>
<LO>INIST-16687.354000105605150060</LO>
<ID>03-0063631</ID>
</server>
</inist>
</record>

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Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)

Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)

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