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Sulfur degassing at Erta Ale (Ethiopia) and Masaya (Nicaragua) volcanoes: Implications for degassing processes and oxygen fugacities of basaltic systems

Identifieur interne : 004951 ( Main/Exploration ); précédent : 004950; suivant : 004952

Sulfur degassing at Erta Ale (Ethiopia) and Masaya (Nicaragua) volcanoes: Implications for degassing processes and oxygen fugacities of basaltic systems

Auteurs : J. M. De Moor [États-Unis, Costa Rica] ; T. P. Fischer [États-Unis] ; Z. D. Sharp [États-Unis] ; P. L. King [États-Unis, Australie] ; M. Wilke [Allemagne] ; R. E. Botcharnikov [Allemagne] ; E. Cottrell [États-Unis] ; M. Zelenski [Russie] ; B. Marty [France] ; K. Klimm [Allemagne] ; C. Rivard [France] ; D. Ayalew [Éthiopie] ; C. Ramirez [Costa Rica] ; K. A. Kelley [États-Unis]

Source :

RBID : ISTEX:9FB53E111518B5C14E4AB18FEA88DA6B0CF711CF

Descripteurs français

English descriptors

Abstract

We investigate the relationship between sulfur and oxygen fugacity at Erta Ale and Masaya volcanoes. Oxygen fugacity was assessed utilizing Fe3+/∑Fe and major element compositions measured in olivine‐hosted melt inclusions and matrix glasses. Erta Ale melts have Fe3+/∑Fe of 0.15–0.16, reflecting fO2 of ΔQFM 0.0 ± 0.3, which is indistinguishable from fO2 calculated from CO2/CO ratios in high‐temperature gases. Masaya is more oxidized at ΔQFM +1.7 ± 0.4, typical of arc settings. Sulfur isotope compositions of gases and scoria at Erta Ale (δ34Sgas − 0.5‰; δ34Sscoria + 0.9‰) and Masaya (δ34Sgas + 4.8‰; δ34Sscoria + 7.4‰) reflect distinct sulfur sources, as well as isotopic fractionation during degassing (equilibrium and kinetic fractionation effects). Sulfur speciation in melts plays an important role in isotope fractionation during degassing and S6+/∑S is <0.07 in Erta Ale melt inclusions compared to >0.67 in Masaya melt inclusions. No change is observed in Fe3+/∑Fe or S6+/∑S with extent of S degassing at Erta Ale, indicating negligible effect on fO2, and further suggesting that H2S is the dominant gas species exsolved from the S2−‐rich melt (i.e., no redistribution of electrons). High SO2/H2S observed in Erta Ale gas emissions is due to gas re‐equilibration at low pressure and fixed fO2. Sulfur budget considerations indicate that the majority of S injected into the systems is emitted as gas, which is therefore representative of the magmatic S isotope composition. The composition of the Masaya gas plume (+4.8‰) cannot be explained by fractionation effects but rather reflects recycling of high δ34S oxidized sulfur through the subduction zone.

Url:
DOI: 10.1002/ggge.20255


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Le document en format XML

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<term>Acta</term>
<term>Ag2s</term>
<term>Analytical precision</term>
<term>Basalt</term>
<term>Basaltic</term>
<term>Basaltic systems</term>
<term>Basaltic volcanoes</term>
<term>Basaltic volcanoes figure</term>
<term>Basaltic volcanoes table</term>
<term>Baso4</term>
<term>Behrens</term>
<term>Bizouard</term>
<term>Botcharnikov</term>
<term>Bubbler</term>
<term>Caldera</term>
<term>Central american</term>
<term>Chantilly</term>
<term>Chem</term>
<term>Conceptual model</term>
<term>Conduit</term>
<term>Convective</term>
<term>Convective degassing</term>
<term>Cosmochim</term>
<term>Costa rica</term>
<term>Cottrell</term>
<term>Crust</term>
<term>Crustal</term>
<term>Degassing</term>
<term>Degassing fractionation</term>
<term>Degassing processes</term>
<term>Dqfm</term>
<term>Earth planet</term>
<term>Equilibrium degassing</term>
<term>Equilibrium degassing fractionation</term>
<term>Erta</term>
<term>Eruption</term>
<term>Ethiopia</term>
<term>Fischer</term>
<term>Fractionation</term>
<term>Fractionation effects</term>
<term>Fugacity</term>
<term>Fumarolic</term>
<term>Fumarolic gases</term>
<term>Geochem</term>
<term>Geochim</term>
<term>Geol</term>
<term>Geophys</term>
<term>Geosyst</term>
<term>Geotherm</term>
<term>Gerlach</term>
<term>Giggenbach</term>
<term>Guern</term>
<term>Heavy isotope</term>
<term>Hydrothermal</term>
<term>Inclusion</term>
<term>Isotope</term>
<term>Isotope composition</term>
<term>Isotope compositions</term>
<term>Isotope fractionation</term>
<term>Isotopic</term>
<term>Isotopic equilibrium</term>
<term>Isotopic fractionation</term>
<term>Isotopically</term>
<term>Jugo</term>
<term>Kbar</term>
<term>Kelley</term>
<term>Kinetic effect</term>
<term>Kinetic fractionation</term>
<term>Klimm</term>
<term>Lava</term>
<term>Lava lake</term>
<term>Lett</term>
<term>Magma</term>
<term>Magma degassing rate</term>
<term>Magmatic</term>
<term>Magmatic gases</term>
<term>Magmatic system</term>
<term>Major element compositions</term>
<term>Mandeville</term>
<term>Marini</term>
<term>Masaya</term>
<term>Masaya caldera</term>
<term>Masaya volcano</term>
<term>Mass balance</term>
<term>Mather</term>
<term>Matrix</term>
<term>Matrix glass</term>
<term>Matrix glasses</term>
<term>Metrich</term>
<term>Mineral phases</term>
<term>Mole fraction</term>
<term>Momotombo</term>
<term>Moor</term>
<term>Morb</term>
<term>Nadeau</term>
<term>Nicaragua</term>
<term>Olivine</term>
<term>Open vent volcanoes</term>
<term>Oppenheimer</term>
<term>Oxidation state</term>
<term>Oxidized</term>
<term>Oxidized sulfur</term>
<term>Oxygen fugacities</term>
<term>Oxygen fugacity</term>
<term>Petrol</term>
<term>Plume</term>
<term>Plume gases</term>
<term>Redox</term>
<term>Sakai</term>
<term>Sawyer</term>
<term>Scaillet</term>
<term>Scoria</term>
<term>Scoria samples</term>
<term>Seawater sulfate</term>
<term>Silicate</term>
<term>Solubility</term>
<term>Speciation</term>
<term>Stix</term>
<term>Subducted sulfate</term>
<term>Subduction</term>
<term>Subduction zones</term>
<term>Sulfate</term>
<term>Sulfate aerosol</term>
<term>Sulfate aerosols</term>
<term>Sulfur</term>
<term>Sulfur content</term>
<term>Sulfur degassing</term>
<term>Sulfur dioxide</term>
<term>Sulfur isotope compositions</term>
<term>Sulfur speciation</term>
<term>Technical processes</term>
<term>Uids</term>
<term>Undegassed</term>
<term>Uxes</term>
<term>Volcanic</term>
<term>Volcanic gases</term>
<term>Volcano</term>
<term>Volcanol</term>
<term>Wilke</term>
<term>Xanes</term>
</keywords>
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<term>Acta</term>
<term>Ag2s</term>
<term>Analytical precision</term>
<term>Basalt</term>
<term>Basaltic</term>
<term>Basaltic systems</term>
<term>Basaltic volcanoes</term>
<term>Basaltic volcanoes figure</term>
<term>Basaltic volcanoes table</term>
<term>Baso4</term>
<term>Behrens</term>
<term>Bizouard</term>
<term>Botcharnikov</term>
<term>Bubbler</term>
<term>Caldera</term>
<term>Central american</term>
<term>Chantilly</term>
<term>Chem</term>
<term>Conceptual model</term>
<term>Conduit</term>
<term>Convective</term>
<term>Convective degassing</term>
<term>Cosmochim</term>
<term>Costa rica</term>
<term>Cottrell</term>
<term>Crust</term>
<term>Crustal</term>
<term>Degassing</term>
<term>Degassing fractionation</term>
<term>Degassing processes</term>
<term>Dqfm</term>
<term>Earth planet</term>
<term>Equilibrium degassing</term>
<term>Equilibrium degassing fractionation</term>
<term>Erta</term>
<term>Eruption</term>
<term>Ethiopia</term>
<term>Fischer</term>
<term>Fractionation</term>
<term>Fractionation effects</term>
<term>Fugacity</term>
<term>Fumarolic</term>
<term>Fumarolic gases</term>
<term>Geochem</term>
<term>Geochim</term>
<term>Geol</term>
<term>Geophys</term>
<term>Geosyst</term>
<term>Geotherm</term>
<term>Gerlach</term>
<term>Giggenbach</term>
<term>Guern</term>
<term>Heavy isotope</term>
<term>Hydrothermal</term>
<term>Inclusion</term>
<term>Isotope</term>
<term>Isotope composition</term>
<term>Isotope compositions</term>
<term>Isotope fractionation</term>
<term>Isotopic</term>
<term>Isotopic equilibrium</term>
<term>Isotopic fractionation</term>
<term>Isotopically</term>
<term>Jugo</term>
<term>Kbar</term>
<term>Kelley</term>
<term>Kinetic effect</term>
<term>Kinetic fractionation</term>
<term>Klimm</term>
<term>Lava</term>
<term>Lava lake</term>
<term>Lett</term>
<term>Magma</term>
<term>Magma degassing rate</term>
<term>Magmatic</term>
<term>Magmatic gases</term>
<term>Magmatic system</term>
<term>Major element compositions</term>
<term>Mandeville</term>
<term>Marini</term>
<term>Masaya</term>
<term>Masaya caldera</term>
<term>Masaya volcano</term>
<term>Mass balance</term>
<term>Mather</term>
<term>Matrix</term>
<term>Matrix glass</term>
<term>Matrix glasses</term>
<term>Metrich</term>
<term>Mineral phases</term>
<term>Mole fraction</term>
<term>Momotombo</term>
<term>Moor</term>
<term>Morb</term>
<term>Nadeau</term>
<term>Nicaragua</term>
<term>Olivine</term>
<term>Open vent volcanoes</term>
<term>Oppenheimer</term>
<term>Oxidation state</term>
<term>Oxidized</term>
<term>Oxidized sulfur</term>
<term>Oxygen fugacities</term>
<term>Oxygen fugacity</term>
<term>Petrol</term>
<term>Plume</term>
<term>Plume gases</term>
<term>Redox</term>
<term>Sakai</term>
<term>Sawyer</term>
<term>Scaillet</term>
<term>Scoria</term>
<term>Scoria samples</term>
<term>Seawater sulfate</term>
<term>Silicate</term>
<term>Solubility</term>
<term>Speciation</term>
<term>Stix</term>
<term>Subducted sulfate</term>
<term>Subduction</term>
<term>Subduction zones</term>
<term>Sulfate</term>
<term>Sulfate aerosol</term>
<term>Sulfate aerosols</term>
<term>Sulfur</term>
<term>Sulfur content</term>
<term>Sulfur degassing</term>
<term>Sulfur dioxide</term>
<term>Sulfur isotope compositions</term>
<term>Sulfur speciation</term>
<term>Technical processes</term>
<term>Uids</term>
<term>Undegassed</term>
<term>Uxes</term>
<term>Volcanic</term>
<term>Volcanic gases</term>
<term>Volcano</term>
<term>Volcanol</term>
<term>Wilke</term>
<term>Xanes</term>
</keywords>
<keywords scheme="Wicri" type="geographic" xml:lang="fr">
<term>Éthiopie</term>
<term>Nicaragua</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr">
<term>Essence</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front>
<div type="abstract">We investigate the relationship between sulfur and oxygen fugacity at Erta Ale and Masaya volcanoes. Oxygen fugacity was assessed utilizing Fe3+/∑Fe and major element compositions measured in olivine‐hosted melt inclusions and matrix glasses. Erta Ale melts have Fe3+/∑Fe of 0.15–0.16, reflecting fO2 of ΔQFM 0.0 ± 0.3, which is indistinguishable from fO2 calculated from CO2/CO ratios in high‐temperature gases. Masaya is more oxidized at ΔQFM +1.7 ± 0.4, typical of arc settings. Sulfur isotope compositions of gases and scoria at Erta Ale (δ34Sgas − 0.5‰; δ34Sscoria + 0.9‰) and Masaya (δ34Sgas + 4.8‰; δ34Sscoria + 7.4‰) reflect distinct sulfur sources, as well as isotopic fractionation during degassing (equilibrium and kinetic fractionation effects). Sulfur speciation in melts plays an important role in isotope fractionation during degassing and S6+/∑S is <0.07 in Erta Ale melt inclusions compared to >0.67 in Masaya melt inclusions. No change is observed in Fe3+/∑Fe or S6+/∑S with extent of S degassing at Erta Ale, indicating negligible effect on fO2, and further suggesting that H2S is the dominant gas species exsolved from the S2−‐rich melt (i.e., no redistribution of electrons). High SO2/H2S observed in Erta Ale gas emissions is due to gas re‐equilibration at low pressure and fixed fO2. Sulfur budget considerations indicate that the majority of S injected into the systems is emitted as gas, which is therefore representative of the magmatic S isotope composition. The composition of the Masaya gas plume (+4.8‰) cannot be explained by fractionation effects but rather reflects recycling of high δ34S oxidized sulfur through the subduction zone.</div>
</front>
</TEI>
<affiliations>
<list>
<country>
<li>Allemagne</li>
<li>Australie</li>
<li>Costa Rica</li>
<li>France</li>
<li>Russie</li>
<li>États-Unis</li>
<li>Éthiopie</li>
</country>
<region>
<li>Auvergne-Rhône-Alpes</li>
<li>Basse-Saxe</li>
<li>Brandebourg</li>
<li>District de Darmstadt</li>
<li>District fédéral central</li>
<li>Hesse (Land)</li>
<li>Nouveau-Mexique</li>
<li>Rhône-Alpes</li>
</region>
<settlement>
<li>Francfort-sur-le-Main</li>
<li>Grenoble</li>
<li>Hanovre</li>
<li>Moscou</li>
<li>Potsdam</li>
</settlement>
<orgName>
<li>Université Johann Wolfgang Goethe de Francfort-sur-le-Main</li>
</orgName>
</list>
<tree>
<country name="États-Unis">
<region name="Nouveau-Mexique">
<name sortKey="De Moor, J M" sort="De Moor, J M" uniqKey="De Moor J" first="J. M." last="De Moor">J. M. De Moor</name>
</region>
<name sortKey="Cottrell, E" sort="Cottrell, E" uniqKey="Cottrell E" first="E." last="Cottrell">E. Cottrell</name>
<name sortKey="De Moor, J M" sort="De Moor, J M" uniqKey="De Moor J" first="J. M." last="De Moor">J. M. De Moor</name>
<name sortKey="Fischer, T P" sort="Fischer, T P" uniqKey="Fischer T" first="T. P." last="Fischer">T. P. Fischer</name>
<name sortKey="Kelley, K A" sort="Kelley, K A" uniqKey="Kelley K" first="K. A." last="Kelley">K. A. Kelley</name>
<name sortKey="King, P L" sort="King, P L" uniqKey="King P" first="P. L." last="King">P. L. King</name>
<name sortKey="Sharp, Z D" sort="Sharp, Z D" uniqKey="Sharp Z" first="Z. D." last="Sharp">Z. D. Sharp</name>
</country>
<country name="Costa Rica">
<noRegion>
<name sortKey="De Moor, J M" sort="De Moor, J M" uniqKey="De Moor J" first="J. M." last="De Moor">J. M. De Moor</name>
</noRegion>
<name sortKey="Ramirez, C" sort="Ramirez, C" uniqKey="Ramirez C" first="C." last="Ramirez">C. Ramirez</name>
</country>
<country name="Australie">
<noRegion>
<name sortKey="King, P L" sort="King, P L" uniqKey="King P" first="P. L." last="King">P. L. King</name>
</noRegion>
</country>
<country name="Allemagne">
<region name="Brandebourg">
<name sortKey="Wilke, M" sort="Wilke, M" uniqKey="Wilke M" first="M." last="Wilke">M. Wilke</name>
</region>
<name sortKey="Botcharnikov, R E" sort="Botcharnikov, R E" uniqKey="Botcharnikov R" first="R. E." last="Botcharnikov">R. E. Botcharnikov</name>
<name sortKey="Klimm, K" sort="Klimm, K" uniqKey="Klimm K" first="K." last="Klimm">K. Klimm</name>
</country>
<country name="Russie">
<region name="District fédéral central">
<name sortKey="Zelenski, M" sort="Zelenski, M" uniqKey="Zelenski M" first="M." last="Zelenski">M. Zelenski</name>
</region>
</country>
<country name="France">
<noRegion>
<name sortKey="Marty, B" sort="Marty, B" uniqKey="Marty B" first="B." last="Marty">B. Marty</name>
</noRegion>
<name sortKey="Rivard, C" sort="Rivard, C" uniqKey="Rivard C" first="C." last="Rivard">C. Rivard</name>
</country>
<country name="Éthiopie">
<noRegion>
<name sortKey="Ayalew, D" sort="Ayalew, D" uniqKey="Ayalew D" first="D." last="Ayalew">D. Ayalew</name>
</noRegion>
</country>
</tree>
</affiliations>
</record>

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