NissirosV1, PascalFrancis, Checkpoint, bibRecord, 000034

Geochemical evidence for mixing of magmatic fluids with seawater, Nisyros hydrothermal system, Greece

Identifieur interne : 000034 ( PascalFrancis/Checkpoint ); précédent : 000033; suivant : 000035

Geochemical evidence for mixing of magmatic fluids with seawater, Nisyros hydrothermal system, Greece

Auteurs : Tatjana Brombach [Italie] ; Stefano Caliro [Italie] ; Giovanni Chiodini [Italie] ; Jens Fiebig [Suisse] ; Johannes C. Hunziker [Suisse] ; Brunella Raco [Italie]

Source :

Bulletin of volcanology [ 0258-8900 ] ; 2003.

RBID : Pascal:05-0054344

Descripteurs français

Pascal (Inist)
- Grèce, Hydrochimie, Phase fluide, Circulation hydrothermale, Mixage, Composition, Argon, Gaz rare, Eau, Interprétation, Isotope stable, Séparation, Réservoir, Température, Cratère, Fumerolle, Iles Egée Grèce, O 18-O 16, C 13-C 12, D-H, S 34-S 32, Fluide magmatique, Ile Nisyros.
Wicri :
- geographic : Grèce.
- topic : Gaz rare, Eau, Interprétation.

English descriptors

KwdEn :
- C-13/C-12, D/H, Greece, Greek Aegean Islands, O-18/O-16, S-34/S-32, argon, composition, craters, fluid phase, fumaroles, hydrochemistry, hydrothermal circulation, interpretation, mixing, noble gases, reservoirs, separation, stable isotopes, temperature, water.

Abstract

The chemical and isotopic compositions (δD_H2O, δ¹⁸O_H2O, δ¹⁸O_CO2, δ¹³C_CO2, δ³⁴S, and He/N₂ and He/Ar ratios) of fumarolic gases from Nisyros, Greece, indicate that both arc-type magmatic water and local seawater feed the hydrothermal system. Isotopic composition of the deep fluid is estimated to be +4.9±0.5‰ for δ¹⁸O and -11±5‰ for δD corresponding to a magmatic water fraction of 0.7. Interpretation of the stable water isotopes was based on liquid-vapor separation conditions obtained through gas geothermometry. The H₂-Ar, H₂-N₂, and H₂-H₂O geothermometers suggest reservoir temperatures of 345±15 °C, in agreement with temperatures measured in deep geothermal wells, whereas a vapor/liquid separation temperature of 260±30 °C is indicated by gas equilibria in the H₂O-H₂-CO₂-CO-CH₄ system. The largest magmatic inputs seem to occur below the Stephanos-Polybotes Micros crater, whereas the marginal fumarolic areas of Phlegeton-Polybotes Megalos craters receive a smaller contribution of magmatic gases.

Affiliations:

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

to stream PascalFrancis, to step Corpus: 000030
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Links to Exploration step

Pascal:05-0054344

Le document en format XML

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<series><title level="j" type="main">Bulletin of volcanology</title>
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<term>D/H</term>
<term>Greece</term>
<term>Greek Aegean Islands</term>
<term>O-18/O-16</term>
<term>S-34/S-32</term>
<term>argon</term>
<term>composition</term>
<term>craters</term>
<term>fluid phase</term>
<term>fumaroles</term>
<term>hydrochemistry</term>
<term>hydrothermal circulation</term>
<term>interpretation</term>
<term>mixing</term>
<term>noble gases</term>
<term>reservoirs</term>
<term>separation</term>
<term>stable isotopes</term>
<term>temperature</term>
<term>water</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Grèce</term>
<term>Hydrochimie</term>
<term>Phase fluide</term>
<term>Circulation hydrothermale</term>
<term>Mixage</term>
<term>Composition</term>
<term>Argon</term>
<term>Gaz rare</term>
<term>Eau</term>
<term>Interprétation</term>
<term>Isotope stable</term>
<term>Séparation</term>
<term>Réservoir</term>
<term>Température</term>
<term>Cratère</term>
<term>Fumerolle</term>
<term>Iles Egée Grèce</term>
<term>O 18-O 16</term>
<term>C 13-C 12</term>
<term>D-H</term>
<term>S 34-S 32</term>
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<front><div type="abstract" xml:lang="en">The chemical and isotopic compositions (δD<sub>H2O</sub>
, δ<sup>18</sup>
O<sub>H2O</sub>
, δ<sup>18</sup>
O<sub>CO2</sub>
, δ<sup>13</sup>
C<sub>CO2</sub>
, δ<sup>34</sup>
S, and He/N<sub>2</sub>
 and He/Ar ratios) of fumarolic gases from Nisyros, Greece, indicate that both arc-type magmatic water and local seawater feed the hydrothermal system. Isotopic composition of the deep fluid is estimated to be +4.9±0.5‰ for δ<sup>18</sup>
O and -11±5‰ for δD corresponding to a magmatic water fraction of 0.7. Interpretation of the stable water isotopes was based on liquid-vapor separation conditions obtained through gas geothermometry. The H<sub>2</sub>
-Ar, H<sub>2</sub>
-N<sub>2</sub>
, and H<sub>2</sub>
-H<sub>2</sub>
O geothermometers suggest reservoir temperatures of 345±15 °C, in agreement with temperatures measured in deep geothermal wells, whereas a vapor/liquid separation temperature of 260±30 °C is indicated by gas equilibria in the H<sub>2</sub>
O-H<sub>2</sub>
-CO<sub>2</sub>
-CO-CH<sub>4</sub>
 system. The largest magmatic inputs seem to occur below the Stephanos-Polybotes Micros crater, whereas the marginal fumarolic areas of Phlegeton-Polybotes Megalos craters receive a smaller contribution of magmatic gases.</div>
</front>
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<fC01 i1="01" l="ENG"><s0>The chemical and isotopic compositions (δD<sub>H2O</sub>
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O geothermometers suggest reservoir temperatures of 345±15 °C, in agreement with temperatures measured in deep geothermal wells, whereas a vapor/liquid separation temperature of 260±30 °C is indicated by gas equilibria in the H<sub>2</sub>
O-H<sub>2</sub>
-CO<sub>2</sub>
-CO-CH<sub>4</sub>
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<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Interprétation</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>interpretation</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Interpretación</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Isotope stable</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>stable isotopes</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Isótopo estable</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Séparation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>separation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Separación</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Réservoir</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>reservoirs</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Température</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>temperature</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Temperatura</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Cratère</s0>
<s5>17</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>craters</s0>
<s5>17</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Cráter</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Fumerolle</s0>
<s5>18</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>fumaroles</s0>
<s5>18</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Fumarola</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Iles Egée Grèce</s0>
<s2>NG</s2>
<s5>20</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>Greek Aegean Islands</s0>
<s2>NG</s2>
<s5>20</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Islas Egeas Griegas</s0>
<s2>NG</s2>
<s5>20</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>O 18-O 16</s0>
<s5>21</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>O-18/O-16</s0>
<s5>21</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>O 18-O 16</s0>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>C 13-C 12</s0>
<s5>22</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>C-13/C-12</s0>
<s5>22</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>C 13-C 12</s0>
<s5>22</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>D-H</s0>
<s5>23</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>D/H</s0>
<s5>23</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>D H</s0>
<s5>23</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>S 34-S 32</s0>
<s5>24</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>S-34/S-32</s0>
<s5>24</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>S 34-S 32</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Fluide magmatique</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Ile Nisyros</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC06><s0>ILS</s0>
<s0>TAS</s0>
<s0>ANS</s0>
</fC06>
<fC07 i1="01" i2="2" l="FRE"><s0>Europe Sud</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Southern Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Europa Sur</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Europe</s0>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Europe</s0>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Europa</s0>
</fC07>
<fN21><s1>024</s1>
</fN21>
<fN44 i1="01"><s1>PSI</s1>
</fN44>
<fN82><s1>PSI</s1>
</fN82>
</pA>
</standard>
</inist>
<affiliations><list><country><li>Italie</li>
<li>Suisse</li>
</country>
<region><li>Canton de Vaud</li>
<li>Toscane</li>
</region>
<settlement><li>Lausanne</li>
<li>Pise</li>
</settlement>
<orgName><li>Université de Lausanne</li>
</orgName>
</list>
<tree><country name="Italie"><noRegion><name sortKey="Brombach, Tatjana" sort="Brombach, Tatjana" uniqKey="Brombach T" first="Tatjana" last="Brombach">Tatjana Brombach</name>
</noRegion>
<name sortKey="Caliro, Stefano" sort="Caliro, Stefano" uniqKey="Caliro S" first="Stefano" last="Caliro">Stefano Caliro</name>
<name sortKey="Chiodini, Giovanni" sort="Chiodini, Giovanni" uniqKey="Chiodini G" first="Giovanni" last="Chiodini">Giovanni Chiodini</name>
<name sortKey="Raco, Brunella" sort="Raco, Brunella" uniqKey="Raco B" first="Brunella" last="Raco">Brunella Raco</name>
</country>
<country name="Suisse"><region name="Canton de Vaud"><name sortKey="Fiebig, Jens" sort="Fiebig, Jens" uniqKey="Fiebig J" first="Jens" last="Fiebig">Jens Fiebig</name>
</region>
<name sortKey="Hunziker, Johannes C" sort="Hunziker, Johannes C" uniqKey="Hunziker J" first="Johannes C." last="Hunziker">Johannes C. Hunziker</name>
</country>
</tree>
</affiliations>
</record>

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Geochemical evidence for mixing of magmatic fluids with seawater, Nisyros hydrothermal system, Greece

Geochemical evidence for mixing of magmatic fluids with seawater, Nisyros hydrothermal system, Greece

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