Geochemical evidence for mixing of magmatic fluids with seawater, Nisyros hydrothermal system, Greece
Identifieur interne : 000187 ( Main/Exploration ); précédent : 000186; suivant : 000188Geochemical 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.
Descripteurs français
- Pascal (Inist)
- Wicri :
- geographic : Grèce.
- topic : Gaz rare, Eau, Interprétation.
English descriptors
- KwdEn :
Abstract
The chemical and isotopic compositions (δDH2O, δ18OH2O, δ18OCO2, δ13CCO2, 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:
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Le document en format XML
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<series><title level="j" type="main">Bulletin of volcanology</title>
<title level="j" type="abbreviated">Bull. volcanol.</title>
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<seriesStmt><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>
<term>Fluide magmatique</term>
<term>Ile Nisyros</term>
</keywords>
<keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Grèce</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Gaz rare</term>
<term>Eau</term>
<term>Interprétation</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>
</TEI>
<affiliations><list><country><li>Italie</li>
<li>Suisse</li>
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<li>Toscane</li>
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<settlement><li>Lausanne</li>
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</settlement>
<orgName><li>Université de Lausanne</li>
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<tree><country name="Italie"><noRegion><name sortKey="Brombach, Tatjana" sort="Brombach, Tatjana" uniqKey="Brombach T" first="Tatjana" last="Brombach">Tatjana Brombach</name>
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<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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