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

Identifieur interne : 000187 ( Main/Exploration ); précédent : 000186; suivant : 000188

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 :

RBID : Pascal:05-0054344

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English descriptors

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.


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Le document en format XML

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<term>Greek Aegean Islands</term>
<term>O-18/O-16</term>
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<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>
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<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>
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</country>
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<name sortKey="Hunziker, Johannes C" sort="Hunziker, Johannes C" uniqKey="Hunziker J" first="Johannes C." last="Hunziker">Johannes C. Hunziker</name>
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