Water-rock interaction in the magmatic-hydrothermal system of Nisyros Island (Greece)
Identifieur interne : 000026 ( PascalFrancis/Curation ); précédent : 000025; suivant : 000027Water-rock interaction in the magmatic-hydrothermal system of Nisyros Island (Greece)
Auteurs : Michele Ambrosio [Italie] ; Marco Doveri [Italie] ; Maria Teresa Fagioli [Italie] ; Luigi Marini [Italie] ; Claudia Principe [Italie] ; Brunella Raco [Italie]Source :
- Journal of volcanology and geothermal research [ 0377-0273 ] ; 2010.
Descripteurs français
- Pascal (Inist)
- Wicri :
- geographic : Grèce.
- topic : Minéralogie.
English descriptors
- KwdEn :
Abstract
In this work, we investigated the water-rock interaction processes taking place in the hydrothermal reservoir of Nisyros through both: (1) a review of the hydrothermal mineralogy encountered in the deep geothermal borehole Nisyros-2; and (2) a comparison of the analytically-derived redox potentials and acidities of fumarolic-related liquids, with those controlled by redox buffers and pH buffers, involving hydrothermal mineral phases. The propylitic zone met in the deep geothermal borehole Nisyros-2, from 950 to 1547 m (total depth), is characterised by abundant, well crystallised epidote, adularia, albite, quartz, pyrite, chlorite, and sericite-muscovite, accompanied by less abundant anhydrite, stilpnomelane, wairakite, garnet, tremolite and pyroxene. These hydrothermal minerals were produced in a comparatively wide temperature range, from 230 to 300 °C, approximately. Hydrothermal assemblages are well developed from 950 to 1360 m, whereas they are less developed below this depth, probably due to low permeability. Based on the RH values calculated for fumarolic gases and for the deep geothermal fluids of Nisyros-1 and Nisyros-2 wells, redox equilibrium with the (FeO)/(FeO1.5) rock buffer appears to be closely attained throughout the hydrothermal reservoir of Nisyros. This conclusion may be easily reconciled with the nearly ubiquitous occurrence of anhydrite and pyrite, since RH values controlled by coexistence of anhydrite and pyrite can be achieved by gas separation. The pH of the liquids feeding the fumarolic vents of Stephanos and Polybote Micros craters was computed, by means of the EQ3 code, based on the Cl-δD relationship which is constrained by the seawater-magmatic water mixing occurring at depth in the hydrothermal-magmatic system of Nisyros.
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Moruzzi 1</s1><s2>56124 Pisa</s2><s3>ITA</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ><sZ>5 aut.</sZ><sZ>6 aut.</sZ></inist:fA14><country>Italie</country></affiliation></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="2010">2010</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>Greece</term><term>acidity</term><term>adularia</term><term>albite</term><term>anhydrite</term><term>boreholes</term><term>buffers</term><term>chlorite</term><term>depth</term><term>epidote</term><term>garnet</term><term>islands</term><term>mineralogy</term><term>muscovite</term><term>pH</term><term>permeability</term><term>pyrite</term><term>pyroxene</term><term>quartz</term><term>reservoirs</term><term>sericite</term><term>stilpnomelane</term><term>temperature</term><term>tremolite</term><term>wairakite</term><term>water-rock interaction</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Interaction eau roche</term><term>Ile</term><term>Réservoir</term><term>Minéralogie</term><term>Puits forage</term><term>Acidité</term><term>Tampon</term><term>PH</term><term>Profondeur</term><term>Epidote</term><term>Adulaire</term><term>Albite</term><term>Quartz</term><term>Pyrite</term><term>Chlorite</term><term>Séricite</term><term>Muscovite</term><term>Anhydrite</term><term>Stilpnomélane</term><term>Wairakite</term><term>Grenat</term><term>Tremolite</term><term>Pyroxène</term><term>Température</term><term>Perméabilité</term><term>Grèce</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Grèce</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Minéralogie</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">In this work, we investigated the water-rock interaction processes taking place in the hydrothermal reservoir of Nisyros through both: (1) a review of the hydrothermal mineralogy encountered in the deep geothermal borehole Nisyros-2; and (2) a comparison of the analytically-derived redox potentials and acidities of fumarolic-related liquids, with those controlled by redox buffers and pH buffers, involving hydrothermal mineral phases. The propylitic zone met in the deep geothermal borehole Nisyros-2, from 950 to 1547 m (total depth), is characterised by abundant, well crystallised epidote, adularia, albite, quartz, pyrite, chlorite, and sericite-muscovite, accompanied by less abundant anhydrite, stilpnomelane, wairakite, garnet, tremolite and pyroxene. These hydrothermal minerals were produced in a comparatively wide temperature range, from 230 to 300 °C, approximately. Hydrothermal assemblages are well developed from 950 to 1360 m, whereas they are less developed below this depth, probably due to low permeability. Based on the R<sub>H</sub> values calculated for fumarolic gases and for the deep geothermal fluids of Nisyros-1 and Nisyros-2 wells, redox equilibrium with the (FeO)/(FeO<sub>1.5</sub>) rock buffer appears to be closely attained throughout the hydrothermal reservoir of Nisyros. This conclusion may be easily reconciled with the nearly ubiquitous occurrence of anhydrite and pyrite, since R<sub>H</sub> values controlled by coexistence of anhydrite and pyrite can be achieved by gas separation. The pH of the liquids feeding the fumarolic vents of Stephanos and Polybote Micros craters was computed, by means of the EQ3 code, based on the Cl-δD relationship which is constrained by the seawater-magmatic water mixing occurring at depth in the hydrothermal-magmatic system of Nisyros.</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>192</s2></fA05><fA06><s2>1-2</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Water-rock interaction in the magmatic-hydrothermal system of Nisyros Island (Greece)</s1></fA08><fA11 i1="01" i2="1"><s1>AMBROSIO (Michele)</s1></fA11><fA11 i1="02" i2="1"><s1>DOVERI (Marco)</s1></fA11><fA11 i1="03" i2="1"><s1>FAGIOLI (Maria Teresa)</s1></fA11><fA11 i1="04" i2="1"><s1>MARINI (Luigi)</s1></fA11><fA11 i1="05" i2="1"><s1>PRINCIPE (Claudia)</s1></fA11><fA11 i1="06" i2="1"><s1>RACO (Brunella)</s1></fA11><fA14 i1="01"><s1>AF Geoscience and Technology Consulting, via Toniolo 222</s1><s2>Campo (PI), 56010</s2><s3>ITA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></fA14><fA14 i1="02"><s1>Institute of Geosciences and Georesources, CNR, Area della Ricerca, Via G. 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All rights reserved.</s1></fA44><fA45><s0>1 p.3/4</s0></fA45><fA47 i1="01" i2="1"><s0>10-0282852</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Journal of volcanology and geothermal research</s0></fA64><fA66 i1="01"><s0>GBR</s0></fA66><fC01 i1="01" l="ENG"><s0>In this work, we investigated the water-rock interaction processes taking place in the hydrothermal reservoir of Nisyros through both: (1) a review of the hydrothermal mineralogy encountered in the deep geothermal borehole Nisyros-2; and (2) a comparison of the analytically-derived redox potentials and acidities of fumarolic-related liquids, with those controlled by redox buffers and pH buffers, involving hydrothermal mineral phases. The propylitic zone met in the deep geothermal borehole Nisyros-2, from 950 to 1547 m (total depth), is characterised by abundant, well crystallised epidote, adularia, albite, quartz, pyrite, chlorite, and sericite-muscovite, accompanied by less abundant anhydrite, stilpnomelane, wairakite, garnet, tremolite and pyroxene. These hydrothermal minerals were produced in a comparatively wide temperature range, from 230 to 300 °C, approximately. Hydrothermal assemblages are well developed from 950 to 1360 m, whereas they are less developed below this depth, probably due to low permeability. Based on the R<sub>H</sub> values calculated for fumarolic gases and for the deep geothermal fluids of Nisyros-1 and Nisyros-2 wells, redox equilibrium with the (FeO)/(FeO<sub>1.5</sub>) rock buffer appears to be closely attained throughout the hydrothermal reservoir of Nisyros. This conclusion may be easily reconciled with the nearly ubiquitous occurrence of anhydrite and pyrite, since R<sub>H</sub> values controlled by coexistence of anhydrite and pyrite can be achieved by gas separation. The pH of the liquids feeding the fumarolic vents of Stephanos and Polybote Micros craters was computed, by means of the EQ3 code, based on the Cl-δD relationship which is constrained by the seawater-magmatic water mixing occurring at depth in the hydrothermal-magmatic system of Nisyros.</s0></fC01><fC02 i1="01" i2="2"><s0>001E01F01</s0></fC02><fC02 i1="02" i2="2"><s0>222A01</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Interaction eau roche</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>water-rock interaction</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Ile</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>islands</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Isla</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Réservoir</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>reservoirs</s0><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Minéralogie</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>mineralogy</s0><s5>04</s5></fC03><fC03 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l="ENG"><s0>epidote</s0><s2>NZ</s2><s5>10</s5></fC03><fC03 i1="10" i2="2" l="SPA"><s0>Epidota</s0><s2>NZ</s2><s5>10</s5></fC03><fC03 i1="11" i2="2" l="FRE"><s0>Adulaire</s0><s2>NZ</s2><s5>11</s5></fC03><fC03 i1="11" i2="2" l="ENG"><s0>adularia</s0><s2>NZ</s2><s5>11</s5></fC03><fC03 i1="11" i2="2" l="SPA"><s0>Adularia</s0><s2>NZ</s2><s5>11</s5></fC03><fC03 i1="12" i2="2" l="FRE"><s0>Albite</s0><s2>NZ</s2><s5>12</s5></fC03><fC03 i1="12" i2="2" l="ENG"><s0>albite</s0><s2>NZ</s2><s5>12</s5></fC03><fC03 i1="12" i2="2" l="SPA"><s0>Albita</s0><s2>NZ</s2><s5>12</s5></fC03><fC03 i1="13" i2="2" l="FRE"><s0>Quartz</s0><s2>NZ</s2><s5>13</s5></fC03><fC03 i1="13" i2="2" l="ENG"><s0>quartz</s0><s2>NZ</s2><s5>13</s5></fC03><fC03 i1="13" i2="2" l="SPA"><s0>Cuarzo</s0><s2>NZ</s2><s5>13</s5></fC03><fC03 i1="14" i2="2" l="FRE"><s0>Pyrite</s0><s2>NZ</s2><s5>14</s5></fC03><fC03 i1="14" i2="2" l="ENG"><s0>pyrite</s0><s2>NZ</s2><s5>14</s5></fC03><fC03 i1="14" i2="2" l="SPA"><s0>Pirita</s0><s2>NZ</s2><s5>14</s5></fC03><fC03 i1="15" i2="2" l="FRE"><s0>Chlorite</s0><s2>NZ</s2><s5>15</s5></fC03><fC03 i1="15" i2="2" l="ENG"><s0>chlorite</s0><s2>NZ</s2><s5>15</s5></fC03><fC03 i1="15" i2="2" l="SPA"><s0>Clorito</s0><s2>NZ</s2><s5>15</s5></fC03><fC03 i1="16" i2="2" l="FRE"><s0>Séricite</s0><s2>NZ</s2><s5>16</s5></fC03><fC03 i1="16" i2="2" l="ENG"><s0>sericite</s0><s2>NZ</s2><s5>16</s5></fC03><fC03 i1="17" i2="2" l="FRE"><s0>Muscovite</s0><s2>NZ</s2><s5>17</s5></fC03><fC03 i1="17" i2="2" l="ENG"><s0>muscovite</s0><s2>NZ</s2><s5>17</s5></fC03><fC03 i1="17" i2="2" l="SPA"><s0>Muscovita</s0><s2>NZ</s2><s5>17</s5></fC03><fC03 i1="18" i2="2" l="FRE"><s0>Anhydrite</s0><s2>NZ</s2><s5>18</s5></fC03><fC03 i1="18" i2="2" l="ENG"><s0>anhydrite</s0><s2>NZ</s2><s5>18</s5></fC03><fC03 i1="18" i2="2" l="SPA"><s0>Anhidrita</s0><s2>NZ</s2><s5>18</s5></fC03><fC03 i1="19" i2="2" l="FRE"><s0>Stilpnomélane</s0><s2>NZ</s2><s5>19</s5></fC03><fC03 i1="19" i2="2" l="ENG"><s0>stilpnomelane</s0><s2>NZ</s2><s5>19</s5></fC03><fC03 i1="19" i2="2" l="SPA"><s0>Estilpnomelana</s0><s2>NZ</s2><s5>19</s5></fC03><fC03 i1="20" i2="2" l="FRE"><s0>Wairakite</s0><s2>NZ</s2><s5>20</s5></fC03><fC03 i1="20" i2="2" l="ENG"><s0>wairakite</s0><s2>NZ</s2><s5>20</s5></fC03><fC03 i1="20" i2="2" l="SPA"><s0>Wairakita</s0><s2>NZ</s2><s5>20</s5></fC03><fC03 i1="21" i2="2" l="FRE"><s0>Grenat</s0><s2>NZ</s2><s5>21</s5></fC03><fC03 i1="21" i2="2" l="ENG"><s0>garnet</s0><s2>NZ</s2><s5>21</s5></fC03><fC03 i1="21" i2="2" l="SPA"><s0>Granate</s0><s2>NZ</s2><s5>21</s5></fC03><fC03 i1="22" i2="2" l="FRE"><s0>Tremolite</s0><s2>NZ</s2><s5>22</s5></fC03><fC03 i1="22" i2="2" l="ENG"><s0>tremolite</s0><s2>NZ</s2><s5>22</s5></fC03><fC03 i1="22" i2="2" l="SPA"><s0>Tremolita</s0><s2>NZ</s2><s5>22</s5></fC03><fC03 i1="23" i2="2" l="FRE"><s0>Pyroxène</s0><s2>NZ</s2><s5>23</s5></fC03><fC03 i1="23" i2="2" l="ENG"><s0>pyroxene</s0><s2>NZ</s2><s5>23</s5></fC03><fC03 i1="23" i2="2" l="SPA"><s0>Piroxeno</s0><s2>NZ</s2><s5>23</s5></fC03><fC03 i1="24" i2="2" l="FRE"><s0>Température</s0><s5>24</s5></fC03><fC03 i1="24" i2="2" l="ENG"><s0>temperature</s0><s5>24</s5></fC03><fC03 i1="24" i2="2" l="SPA"><s0>Temperatura</s0><s5>24</s5></fC03><fC03 i1="25" i2="2" l="FRE"><s0>Perméabilité</s0><s5>25</s5></fC03><fC03 i1="25" i2="2" l="ENG"><s0>permeability</s0><s5>25</s5></fC03><fC03 i1="25" i2="2" l="SPA"><s0>Permeabilidad</s0><s5>25</s5></fC03><fC03 i1="26" i2="2" l="FRE"><s0>Grèce</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="26" i2="2" l="ENG"><s0>Greece</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="26" i2="2" l="SPA"><s0>Grecia</s0><s2>NG</s2><s5>61</s5></fC03><fC07 i1="01" i2="2" l="FRE"><s0>Sorosilicate</s0><s2>NZ</s2></fC07><fC07 i1="01" i2="2" l="ENG"><s0>sorosilicates</s0><s2>NZ</s2></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Silicate</s0><s2>NZ</s2></fC07><fC07 i1="02" i2="2" l="ENG"><s0>silicates</s0><s2>NZ</s2></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Silicato</s0><s2>NZ</s2></fC07><fC07 i1="03" i2="2" l="FRE"><s0>Feldspath K</s0><s2>NZ</s2></fC07><fC07 i1="03" i2="2" l="ENG"><s0>K-feldspar</s0><s2>NZ</s2></fC07><fC07 i1="03" i2="2" l="SPA"><s0>Feldespato K</s0><s2>NZ</s2></fC07><fC07 i1="04" i2="2" l="FRE"><s0>Feldspath alcalin</s0><s2>NZ</s2></fC07><fC07 i1="04" i2="2" l="ENG"><s0>alkali feldspar</s0><s2>NZ</s2></fC07><fC07 i1="04" i2="2" l="SPA"><s0>Feldespato alcalino</s0><s2>NZ</s2></fC07><fC07 i1="05" i2="2" l="FRE"><s0>Feldspath</s0><s2>NZ</s2></fC07><fC07 i1="05" i2="2" l="ENG"><s0>feldspar</s0><s2>NZ</s2></fC07><fC07 i1="05" i2="2" l="SPA"><s0>Feldespato</s0><s2>NZ</s2></fC07><fC07 i1="06" i2="2" l="FRE"><s0>Tectosilicate</s0><s2>NZ</s2></fC07><fC07 i1="06" i2="2" l="ENG"><s0>framework silicates</s0><s2>NZ</s2></fC07><fC07 i1="07" i2="2" l="FRE"><s0>Plagioclase</s0><s2>NZ</s2></fC07><fC07 i1="07" i2="2" l="ENG"><s0>plagioclase</s0><s2>NZ</s2></fC07><fC07 i1="07" i2="2" l="SPA"><s0>Plagioclasa</s0><s2>NZ</s2></fC07><fC07 i1="08" i2="2" l="FRE"><s0>Sulfure fer</s0><s2>NZ</s2></fC07><fC07 i1="08" i2="2" l="ENG"><s0>iron sulfides</s0><s2>NZ</s2></fC07><fC07 i1="08" i2="2" l="SPA"><s0>Sulfuro hierro</s0><s2>NZ</s2></fC07><fC07 i1="09" i2="2" l="FRE"><s0>Sulfure</s0><s2>NZ</s2></fC07><fC07 i1="09" i2="2" l="ENG"><s0>sulfides</s0><s2>NZ</s2></fC07><fC07 i1="09" i2="2" l="SPA"><s0>Sulfuro</s0><s2>NZ</s2></fC07><fC07 i1="10" i2="2" l="FRE"><s0>Phyllosilicate</s0><s2>NZ</s2></fC07><fC07 i1="10" i2="2" l="ENG"><s0>sheet silicates</s0><s2>NZ</s2></fC07><fC07 i1="10" i2="2" l="SPA"><s0>Filosilicato</s0><s2>NZ</s2></fC07><fC07 i1="11" i2="2" l="FRE"><s0>Mica</s0><s2>NZ</s2></fC07><fC07 i1="11" i2="2" l="ENG"><s0>mica</s0><s2>NZ</s2></fC07><fC07 i1="11" i2="2" l="SPA"><s0>Mica</s0><s2>NZ</s2></fC07><fC07 i1="12" i2="2" l="FRE"><s0>Sulfate</s0><s2>NZ</s2></fC07><fC07 i1="12" i2="2" l="ENG"><s0>sulfates</s0><s2>NZ</s2></fC07><fC07 i1="12" i2="2" l="SPA"><s0>Sulfato</s0><s2>NZ</s2></fC07><fC07 i1="13" i2="2" l="FRE"><s0>Zéolite</s0><s2>NZ</s2></fC07><fC07 i1="13" i2="2" l="ENG"><s0>zeolite</s0><s2>NZ</s2></fC07><fC07 i1="13" i2="2" l="SPA"><s0>Zeolita</s0><s2>NZ</s2></fC07><fC07 i1="14" i2="2" l="FRE"><s0>Nésosilicate</s0><s2>NZ</s2></fC07><fC07 i1="14" i2="2" l="ENG"><s0>nesosilicates</s0><s2>NZ</s2></fC07><fC07 i1="15" i2="2" l="FRE"><s0>Amphibole clino</s0><s2>NZ</s2></fC07><fC07 i1="15" i2="2" l="ENG"><s0>clinoamphibole</s0><s2>NZ</s2></fC07><fC07 i1="15" i2="2" l="SPA"><s0>Clinoanfíbol</s0><s2>NZ</s2></fC07><fC07 i1="16" i2="2" l="FRE"><s0>Amphibole</s0><s2>NZ</s2></fC07><fC07 i1="16" i2="2" l="ENG"><s0>amphibole</s0><s2>NZ</s2></fC07><fC07 i1="16" i2="2" l="SPA"><s0>Anfíbol</s0><s2>NZ</s2></fC07><fC07 i1="17" i2="2" l="FRE"><s0>Inosilicate</s0><s2>NZ</s2></fC07><fC07 i1="17" i2="2" l="ENG"><s0>chain silicates</s0><s2>NZ</s2></fC07><fC07 i1="18" i2="2" l="FRE"><s0>Europe Sud</s0><s2>NG</s2></fC07><fC07 i1="18" i2="2" l="ENG"><s0>Southern Europe</s0><s2>NG</s2></fC07><fC07 i1="18" i2="2" l="SPA"><s0>Europa Sur</s0><s2>NG</s2></fC07><fC07 i1="19" i2="2" l="FRE"><s0>Europe</s0><s2>564</s2></fC07><fC07 i1="19" i2="2" l="ENG"><s0>Europe</s0><s2>564</s2></fC07><fC07 i1="19" i2="2" l="SPA"><s0>Europa</s0><s2>564</s2></fC07><fN21><s1>181</s1></fN21><fN44 i1="01"><s1>OTO</s1></fN44><fN82><s1>OTO</s1></fN82></pA></standard></inist></record>Pour manipuler ce document sous Unix (Dilib)
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|wiki= Wicri/Terre
|area= NissirosV1
|flux= PascalFrancis
|étape= Curation
|type= RBID
|clé= Pascal:10-0282852
|texte= Water-rock interaction in the magmatic-hydrothermal system of Nisyros Island (Greece)
}}
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