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Fluid geochemistry of Nisyros island, Dodecanese, Greece

Identifieur interne : 000397 ( Main/Merge ); précédent : 000396; suivant : 000398

Fluid geochemistry of Nisyros island, Dodecanese, Greece

Auteurs : G. Chiodini [Italie] ; R. Cioni ; C. Leonis ; L. Marini ; B. Raco

Source :

RBID : Pascal:93-0461021

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English descriptors

Abstract

Two distinct hydrothermal aquifers are present beneath the Lakki plain: (a) a deep aquifer, characterized by temperatures higher than 290°C and chloride-rich fluids; and (b) a shallow aquifer, with a chloride content close to that of sea water and temperatures in the range 170-255°C. The vapor phase boiled from the shallow aquifer feeds the fumarolic vents in the southern half of the Lakki plain and its liquid phase flows northeast and southwest, contributing to the thermal springs located along the northern and southern coasts of the island. This conceptual hydrogeochemical model of Nisyros Island can be used to reconstruct past hydrothermal eruptions and to estimate the risk of such events happening again in the future

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Pascal:93-0461021

Le document en format XML

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<title xml:lang="en" level="a">Fluid geochemistry of Nisyros island, Dodecanese, Greece</title>
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<name sortKey="Chiodini, G" sort="Chiodini, G" uniqKey="Chiodini G" first="G." last="Chiodini">G. Chiodini</name>
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<s1>Univ. Perugia, dip. sci. terra</s1>
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<country>Italie</country>
<wicri:noRegion>06100 Perugia</wicri:noRegion>
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<name sortKey="Cioni, R" sort="Cioni, R" uniqKey="Cioni R" first="R." last="Cioni">R. Cioni</name>
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<name sortKey="Leonis, C" sort="Leonis, C" uniqKey="Leonis C" first="C." last="Leonis">C. Leonis</name>
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<name sortKey="Marini, L" sort="Marini, L" uniqKey="Marini L" first="L." last="Marini">L. Marini</name>
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<name sortKey="Raco, B" sort="Raco, B" uniqKey="Raco B" first="B." last="Raco">B. Raco</name>
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<title xml:lang="en" level="a">Fluid geochemistry of Nisyros island, Dodecanese, Greece</title>
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<name sortKey="Cioni, R" sort="Cioni, R" uniqKey="Cioni R" first="R." last="Cioni">R. Cioni</name>
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<name sortKey="Leonis, C" sort="Leonis, C" uniqKey="Leonis C" first="C." last="Leonis">C. Leonis</name>
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<name sortKey="Marini, L" sort="Marini, L" uniqKey="Marini L" first="L." last="Marini">L. Marini</name>
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<series>
<title level="j" type="main">Journal of volcanology and geothermal research</title>
<title level="j" type="abbreviated">J. volcanol. geotherm. res.</title>
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<term>Dodecanese</term>
<term>Greece</term>
<term>aquifers</term>
<term>chlorine</term>
<term>craters</term>
<term>degassing</term>
<term>enthalpy</term>
<term>eruptions</term>
<term>explosions</term>
<term>fluid pressure</term>
<term>fumaroles</term>
<term>geothermal systems</term>
<term>ground water</term>
<term>hot springs</term>
<term>hydrochemistry</term>
<term>melange</term>
<term>models</term>
<term>prediction</term>
<term>salinity</term>
<term>sea water</term>
<term>temperature</term>
<term>volcanic hazards</term>
<term>water vapor</term>
<term>water wells</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Grèce</term>
<term>Iles Dodécanèse</term>
<term>Nappe eau</term>
<term>Température</term>
<term>Chlore</term>
<term>Vapeur eau</term>
<term>Fumerolle</term>
<term>Source thermale</term>
<term>Hydrochimie</term>
<term>Eruption</term>
<term>Explosion</term>
<term>Risque volcanique</term>
<term>Prévision</term>
<term>Système géothermique</term>
<term>Puits eau</term>
<term>Cratère</term>
<term>Départ gaz</term>
<term>Pression fluide</term>
<term>Salinité</term>
<term>Modèle</term>
<term>Enthalpie</term>
<term>Mélange</term>
<term>Eau souterraine</term>
<term>Eau mer</term>
<term>Circulation hydrothermale</term>
<term>Ile Nisyros</term>
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<term>Grèce</term>
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<term>Chlore</term>
<term>Eau souterraine</term>
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<front>
<div type="abstract" xml:lang="en">Two distinct hydrothermal aquifers are present beneath the Lakki plain: (a) a deep aquifer, characterized by temperatures higher than 290°C and chloride-rich fluids; and (b) a shallow aquifer, with a chloride content close to that of sea water and temperatures in the range 170-255°C. The vapor phase boiled from the shallow aquifer feeds the fumarolic vents in the southern half of the Lakki plain and its liquid phase flows northeast and southwest, contributing to the thermal springs located along the northern and southern coasts of the island. This conceptual hydrogeochemical model of Nisyros Island can be used to reconstruct past hydrothermal eruptions and to estimate the risk of such events happening again in the future</div>
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<name sortKey="Marini, L" sort="Marini, L" uniqKey="Marini L" first="L." last="Marini">L. Marini</name>
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