Fluid geochemistry of Nisyros island, Dodecanese, Greece
Identifieur interne : 000052 ( PascalFrancis/Checkpoint ); précédent : 000051; suivant : 000053Fluid geochemistry of Nisyros island, Dodecanese, Greece
Auteurs : G. Chiodini [Italie] ; R. Cioni ; C. Leonis ; L. Marini ; B. RacoSource :
- Journal of volcanology and geothermal research [ 0377-0273 ] ; 1993.
Descripteurs français
- Pascal (Inist)
- Grèce, Iles Dodécanèse, Nappe eau, Température, Chlore, Vapeur eau, Fumerolle, Source thermale, Hydrochimie, Eruption, Explosion, Risque volcanique, Prévision, Système géothermique, Puits eau, Cratère, Départ gaz, Pression fluide, Salinité, Modèle, Enthalpie, Mélange, Eau souterraine, Eau mer, Circulation hydrothermale, Ile Nisyros.
- Wicri :
- geographic : Grèce.
- topic : Chlore, Eau souterraine.
English descriptors
- KwdEn :
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
Affiliations:
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Pascal:93-0461021Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Fluid geochemistry of Nisyros island, Dodecanese, Greece</title><author><name sortKey="Chiodini, G" sort="Chiodini, G" uniqKey="Chiodini G" first="G." last="Chiodini">G. Chiodini</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Univ. Perugia, dip. sci. terra</s1><s2>06100 Perugia</s2><s3>ITA</s3><sZ>1 aut.</sZ></inist:fA14><country>Italie</country><wicri:noRegion>06100 Perugia</wicri:noRegion></affiliation></author><author><name sortKey="Cioni, R" sort="Cioni, R" uniqKey="Cioni R" first="R." last="Cioni">R. Cioni</name></author><author><name sortKey="Leonis, C" sort="Leonis, C" uniqKey="Leonis C" first="C." last="Leonis">C. Leonis</name></author><author><name sortKey="Marini, L" sort="Marini, L" uniqKey="Marini L" first="L." last="Marini">L. Marini</name></author><author><name sortKey="Raco, B" sort="Raco, B" uniqKey="Raco B" first="B." last="Raco">B. Raco</name></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">93-0461021</idno><date when="1993">1993</date><idno type="stanalyst">PASCAL 93-0461021 INIST</idno><idno type="RBID">Pascal:93-0461021</idno><idno type="wicri:Area/PascalFrancis/Corpus">000056</idno><idno type="wicri:Area/PascalFrancis/Curation">000068</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000052</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">000052</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Fluid geochemistry of Nisyros island, Dodecanese, Greece</title><author><name sortKey="Chiodini, G" sort="Chiodini, G" uniqKey="Chiodini G" first="G." last="Chiodini">G. Chiodini</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Univ. Perugia, dip. sci. terra</s1><s2>06100 Perugia</s2><s3>ITA</s3><sZ>1 aut.</sZ></inist:fA14><country>Italie</country><wicri:noRegion>06100 Perugia</wicri:noRegion></affiliation></author><author><name sortKey="Cioni, R" sort="Cioni, R" uniqKey="Cioni R" first="R." last="Cioni">R. Cioni</name></author><author><name sortKey="Leonis, C" sort="Leonis, C" uniqKey="Leonis C" first="C." last="Leonis">C. Leonis</name></author><author><name sortKey="Marini, L" sort="Marini, L" uniqKey="Marini L" first="L." last="Marini">L. Marini</name></author><author><name sortKey="Raco, B" sort="Raco, B" uniqKey="Raco B" first="B." last="Raco">B. Raco</name></author></analytic><series><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno><imprint><date when="1993">1993</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><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></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Grèce</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Chlore</term><term>Eau souterraine</term></keywords></textClass></profileDesc></teiHeader><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></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0377-0273</s0></fA01><fA02 i1="01"><s0>JVGRDQ</s0></fA02><fA03 i2="1"><s0>J. volcanol. geotherm. res.</s0></fA03><fA05><s2>56</s2></fA05><fA06><s2>1-2</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Fluid geochemistry of Nisyros island, Dodecanese, Greece</s1></fA08><fA11 i1="01" i2="1"><s1>CHIODINI (G.)</s1></fA11><fA11 i1="02" i2="1"><s1>CIONI (R.)</s1></fA11><fA11 i1="03" i2="1"><s1>LEONIS (C.)</s1></fA11><fA11 i1="04" i2="1"><s1>MARINI (L.)</s1></fA11><fA11 i1="05" i2="1"><s1>RACO (B.)</s1></fA11><fA14 i1="01"><s1>Univ. Perugia, dip. sci. terra</s1><s2>06100 Perugia</s2><s3>ITA</s3><sZ>1 aut.</sZ></fA14><fA20><s1>95-112</s1><s7>3</s7></fA20><fA21><s1>1993</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>17236</s2><s5>354000033650130050</s5></fA43><fA44><s0>0000</s0></fA44><fA45><s0>42 ref.</s0></fA45><fA47 i1="01" i2="1"><s0>93-0461021</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i2="1"><s0>Journal of volcanology and geothermal research</s0></fA64><fA66 i1="01"><s0>NLD</s0></fA66><fC01 i1="01" l="ENG"><s0>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</s0></fC01><fC02 i1="01" i2="2"><s0>222A01</s0></fC02><fC02 i1="02" i2="2"><s0>220B02</s0></fC02><fC02 i1="03" i2="2"><s0>226B02</s0></fC02><fC02 i1="04" i2="X"><s0>001E01F01</s0></fC02><fC02 i1="05" i2="X"><s0>001E01B02</s0></fC02><fC02 i1="06" i2="X"><s0>001E01O02</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Grèce</s0><s2>NG</s2></fC03><fC03 i1="01" i2="2" l="ENG"><s0>Greece</s0><s2>NG</s2></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Grecia</s0><s2>NG</s2></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Iles Dodécanèse</s0></fC03><fC03 i1="02" i2="2" l="ENG"><s0>Dodecanese</s0></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Islas Dodecanese</s0></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Nappe eau</s0></fC03><fC03 i1="03" i2="2" l="ENG"><s0>aquifers</s0></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Capa agua</s0></fC03><fC03 i1="04" 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sortKey="Cioni, R" sort="Cioni, R" uniqKey="Cioni R" first="R." last="Cioni">R. Cioni</name><name sortKey="Leonis, C" sort="Leonis, C" uniqKey="Leonis C" first="C." last="Leonis">C. Leonis</name><name sortKey="Marini, L" sort="Marini, L" uniqKey="Marini L" first="L." last="Marini">L. Marini</name><name sortKey="Raco, B" sort="Raco, B" uniqKey="Raco B" first="B." last="Raco">B. Raco</name></noCountry><country name="Italie"><noRegion><name sortKey="Chiodini, G" sort="Chiodini, G" uniqKey="Chiodini G" first="G." last="Chiodini">G. Chiodini</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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