Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics
Identifieur interne : 000061 ( PascalFrancis/Corpus ); précédent : 000060; suivant : 000062Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics
Auteurs : K. S. Seymour ; D. VlassopoulosSource :
- Journal of volcanology and geothermal research [ 0377-0273 ] ; 1992.
Descripteurs français
- Pascal (Inist)
- Magma, Mélange, Analyse élément trace, Arc volcanique, Quaternaire, Andésite, Rhyodacite, Composition calcoalcaline, Analyse chimique, Cristallisation fractionnée, Fractionnement chimique, Ponce, Phénocristal, Chambre magmatique, Magma basique, Association minérale, Mer Egée, Pillow lava, Pyroclastique, Terre rare, Donnée microsonde électronique, Volcan Nisyros.
English descriptors
- KwdEn :
- Aegean Sea, Quaternary, andesites, calc-alkalic composition, chemical composition, chemical fractionation, electron probe data, fractional crystallization, mafic magmas, magma chambers, magmas, melange, mineral assemblages, phenocrysts, pillow lava, pumice, pyroclastics, rare earths, rhyodacites, trace elements, volcanic arcs.
Abstract
Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite, Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60-66 wt.% SiO2
Notice en format standard (ISO 2709)
Pour connaître la documentation sur le format Inist Standard.
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Format Inist (serveur)
| NO : | PASCAL 93-0028457 INIST |
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| ET : | Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics |
| AU : | SEYMOUR (K. S.); VLASSOPOULOS (D.) |
| AF : | Concordia univ., geology dep./Montreal PQ H4B 1R6/Canada |
| DT : | Publication en série; Niveau analytique |
| SO : | Journal of volcanology and geothermal research; ISSN 0377-0273; Coden JVGRDQ; Pays-Bas; Da. 1992; Vol. 50; No. 3; Pp. 273-299; Bibl. 1 p.1/2 |
| LA : | Anglais |
| EA : | Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite, Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60-66 wt.% SiO2 |
| CC : | 222A01; 001E01F01 |
| FD : | Magma; Mélange; Analyse élément trace; Arc volcanique; Quaternaire; Andésite; Rhyodacite; Composition calcoalcaline; Analyse chimique; Cristallisation fractionnée; Fractionnement chimique; Ponce; Phénocristal; Chambre magmatique; Magma basique; Association minérale; Mer Egée; Pillow lava; Pyroclastique; Terre rare; Donnée microsonde électronique; Volcan Nisyros |
| FG : | Roche volcanique; Roche ignée; Mer Méditerranée Est; Mer Méditerranée |
| ED : | magmas; melange; trace elements; volcanic arcs; Quaternary; andesites; rhyodacites; calc-alkalic composition; chemical composition; fractional crystallization; chemical fractionation; pumice; phenocrysts; magma chambers; mafic magmas; mineral assemblages; Aegean Sea; pillow lava; pyroclastics; rare earths; electron probe data |
| EG : | volcanic rocks; igneous rocks; East Mediterranean; Mediterranean Sea |
| SD : | Magma; Mezcla; Análisis elementos traza; Cuaternario; Andesita; Riodacita; Composición calcoalcalina; Análisis químico; Cristalización fraccionada; Fraccionamiento químico; Piedra pómez; Fenocristal; Cámara magmática; Magma básico; Asociación mineral; Mar Egeo; Pillow lava; Piroclástico; Tierras raras; Dato sonda electrónica |
| LO : | INIST-17236.354000028033600040 |
| ID : | 93-0028457 |
Links to Exploration step
Pascal:93-0028457Le document en format XML
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Vlassopoulos</name></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">93-0028457</idno><date when="1992">1992</date><idno type="stanalyst">PASCAL 93-0028457 INIST</idno><idno type="RBID">Pascal:93-0028457</idno><idno type="wicri:Area/PascalFrancis/Corpus">000061</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</title><author><name sortKey="Seymour, K S" sort="Seymour, K S" uniqKey="Seymour K" first="K. S." last="Seymour">K. S. Seymour</name><affiliation><inist:fA14 i1="01"><s1>Concordia univ., geology dep.</s1><s2>Montreal PQ H4B 1R6</s2><s3>CAN</s3></inist:fA14></affiliation></author><author><name sortKey="Vlassopoulos, D" sort="Vlassopoulos, D" uniqKey="Vlassopoulos D" first="D." last="Vlassopoulos">D. Vlassopoulos</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="1992">1992</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>Aegean Sea</term><term>Quaternary</term><term>andesites</term><term>calc-alkalic composition</term><term>chemical composition</term><term>chemical fractionation</term><term>electron probe data</term><term>fractional crystallization</term><term>mafic magmas</term><term>magma chambers</term><term>magmas</term><term>melange</term><term>mineral assemblages</term><term>phenocrysts</term><term>pillow lava</term><term>pumice</term><term>pyroclastics</term><term>rare earths</term><term>rhyodacites</term><term>trace elements</term><term>volcanic arcs</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Magma</term><term>Mélange</term><term>Analyse élément trace</term><term>Arc volcanique</term><term>Quaternaire</term><term>Andésite</term><term>Rhyodacite</term><term>Composition calcoalcaline</term><term>Analyse chimique</term><term>Cristallisation fractionnée</term><term>Fractionnement chimique</term><term>Ponce</term><term>Phénocristal</term><term>Chambre magmatique</term><term>Magma basique</term><term>Association minérale</term><term>Mer Egée</term><term>Pillow lava</term><term>Pyroclastique</term><term>Terre rare</term><term>Donnée microsonde électronique</term><term>Volcan Nisyros</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite, Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60-66 wt.% SiO<sub>2</sub></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>50</s2></fA05><fA06><s2>3</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</s1></fA08><fA11 i1="01" i2="1"><s1>SEYMOUR (K. S.)</s1></fA11><fA11 i1="02" i2="1"><s1>VLASSOPOULOS (D.)</s1></fA11><fA14 i1="01"><s1>Concordia univ., geology dep.</s1><s2>Montreal PQ H4B 1R6</s2><s3>CAN</s3></fA14><fA20><s1>273-299</s1><s7>8</s7></fA20><fA21><s1>1992</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>17236</s2><s5>354000028033600040</s5></fA43><fA44><s0>0000</s0></fA44><fA45><s0>1 p.1/2</s0></fA45><fA47 i1="01" i2="1"><s0>93-0028457</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>Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite, Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60-66 wt.% SiO<sub>2</sub></s0></fC01><fC02 i1="01" i2="2"><s0>222A01</s0></fC02><fC02 i1="02" i2="X"><s0>001E01F01</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Magma</s0></fC03><fC03 i1="01" i2="2" l="ENG"><s0>magmas</s0></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Magma</s0></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Mélange</s0></fC03><fC03 i1="02" i2="2" l="ENG"><s0>melange</s0></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Mezcla</s0></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Analyse élément trace</s0></fC03><fC03 i1="03" i2="2" l="ENG"><s0>trace elements</s0></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Análisis elementos traza</s0></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Arc volcanique</s0></fC03><fC03 i1="04" i2="2" l="ENG"><s0>volcanic arcs</s0></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Quaternaire</s0></fC03><fC03 i1="05" i2="2" l="ENG"><s0>Quaternary</s0></fC03><fC03 i1="05" i2="2" l="SPA"><s0>Cuaternario</s0></fC03><fC03 i1="06" i2="2" l="FRE"><s0>Andésite</s0></fC03><fC03 i1="06" i2="2" l="ENG"><s0>andesites</s0></fC03><fC03 i1="06" i2="2" l="SPA"><s0>Andesita</s0></fC03><fC03 i1="07" i2="2" l="FRE"><s0>Rhyodacite</s0></fC03><fC03 i1="07" i2="2" l="ENG"><s0>rhyodacites</s0></fC03><fC03 i1="07" i2="2" l="SPA"><s0>Riodacita</s0></fC03><fC03 i1="08" i2="2" l="FRE"><s0>Composition calcoalcaline</s0></fC03><fC03 i1="08" i2="2" l="ENG"><s0>calc-alkalic composition</s0></fC03><fC03 i1="08" i2="2" l="SPA"><s0>Composición calcoalcalina</s0></fC03><fC03 i1="09" i2="2" l="FRE"><s0>Analyse chimique</s0></fC03><fC03 i1="09" i2="2" l="ENG"><s0>chemical composition</s0></fC03><fC03 i1="09" i2="2" l="SPA"><s0>Análisis químico</s0></fC03><fC03 i1="10" i2="2" l="FRE"><s0>Cristallisation fractionnée</s0></fC03><fC03 i1="10" i2="2" l="ENG"><s0>fractional crystallization</s0></fC03><fC03 i1="10" i2="2" l="SPA"><s0>Cristalización fraccionada</s0></fC03><fC03 i1="11" i2="2" l="FRE"><s0>Fractionnement chimique</s0></fC03><fC03 i1="11" i2="2" l="ENG"><s0>chemical fractionation</s0></fC03><fC03 i1="11" i2="2" l="SPA"><s0>Fraccionamiento químico</s0></fC03><fC03 i1="12" i2="2" l="FRE"><s0>Ponce</s0></fC03><fC03 i1="12" i2="2" l="ENG"><s0>pumice</s0></fC03><fC03 i1="12" i2="2" l="SPA"><s0>Piedra pómez</s0></fC03><fC03 i1="13" i2="2" l="FRE"><s0>Phénocristal</s0></fC03><fC03 i1="13" i2="2" l="ENG"><s0>phenocrysts</s0></fC03><fC03 i1="13" i2="2" l="SPA"><s0>Fenocristal</s0></fC03><fC03 i1="14" i2="2" l="FRE"><s0>Chambre magmatique</s0></fC03><fC03 i1="14" i2="2" l="ENG"><s0>magma chambers</s0></fC03><fC03 i1="14" i2="2" l="SPA"><s0>Cámara magmática</s0></fC03><fC03 i1="15" i2="2" l="FRE"><s0>Magma basique</s0></fC03><fC03 i1="15" i2="2" l="ENG"><s0>mafic magmas</s0></fC03><fC03 i1="15" i2="2" l="SPA"><s0>Magma básico</s0></fC03><fC03 i1="16" i2="2" l="FRE"><s0>Association minérale</s0></fC03><fC03 i1="16" i2="2" l="ENG"><s0>mineral assemblages</s0></fC03><fC03 i1="16" i2="2" l="SPA"><s0>Asociación mineral</s0></fC03><fC03 i1="17" i2="2" l="FRE"><s0>Mer Egée</s0><s2>NG</s2></fC03><fC03 i1="17" i2="2" l="ENG"><s0>Aegean Sea</s0><s2>NG</s2></fC03><fC03 i1="17" i2="2" l="SPA"><s0>Mar Egeo</s0><s2>NG</s2></fC03><fC03 i1="18" i2="2" l="FRE"><s0>Pillow lava</s0></fC03><fC03 i1="18" i2="2" l="ENG"><s0>pillow lava</s0></fC03><fC03 i1="18" i2="2" l="SPA"><s0>Pillow lava</s0></fC03><fC03 i1="19" i2="2" l="FRE"><s0>Pyroclastique</s0></fC03><fC03 i1="19" i2="2" l="ENG"><s0>pyroclastics</s0></fC03><fC03 i1="19" i2="2" l="SPA"><s0>Piroclástico</s0></fC03><fC03 i1="20" i2="2" l="FRE"><s0>Terre rare</s0></fC03><fC03 i1="20" i2="2" l="ENG"><s0>rare earths</s0></fC03><fC03 i1="20" i2="2" l="SPA"><s0>Tierras raras</s0></fC03><fC03 i1="21" i2="2" l="FRE"><s0>Donnée microsonde électronique</s0></fC03><fC03 i1="21" i2="2" l="ENG"><s0>electron probe data</s0></fC03><fC03 i1="21" i2="2" l="SPA"><s0>Dato sonda electrónica</s0></fC03><fC03 i1="22" i2="2" l="FRE"><s0>Volcan Nisyros</s0><s4>INC</s4></fC03><fC06><s0>ANS</s0><s0>TAS</s0><s0>ILS</s0></fC06><fC07 i1="01" i2="2" l="FRE"><s0>Roche volcanique</s0></fC07><fC07 i1="01" i2="2" l="ENG"><s0>volcanic rocks</s0></fC07><fC07 i1="01" i2="2" l="SPA"><s0>Roca volcánica</s0></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Roche ignée</s0></fC07><fC07 i1="02" i2="2" l="ENG"><s0>igneous rocks</s0></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Roca ignea</s0></fC07><fC07 i1="03" i2="2" l="FRE"><s0>Mer Méditerranée Est</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="ENG"><s0>East Mediterranean</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="SPA"><s0>Mar Mediterraneo Este</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="FRE"><s0>Mer Méditerranée</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="ENG"><s0>Mediterranean Sea</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="SPA"><s0>Mar Mediterráneo</s0><s2>NG</s2></fC07><fN21><s1>354</s1></fN21></pA></standard><server><NO>PASCAL 93-0028457 INIST</NO><ET>Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</ET><AU>SEYMOUR (K. S.); VLASSOPOULOS (D.)</AU><AF>Concordia univ., geology dep./Montreal PQ H4B 1R6/Canada</AF><DT>Publication en série; Niveau analytique</DT><SO>Journal of volcanology and geothermal research; ISSN 0377-0273; Coden JVGRDQ; Pays-Bas; Da. 1992; Vol. 50; No. 3; Pp. 273-299; Bibl. 1 p.1/2</SO><LA>Anglais</LA><EA>Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite, Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60-66 wt.% SiO<sub>2</sub></EA><CC>222A01; 001E01F01</CC><FD>Magma; Mélange; Analyse élément trace; Arc volcanique; Quaternaire; Andésite; Rhyodacite; Composition calcoalcaline; Analyse chimique; Cristallisation fractionnée; Fractionnement chimique; Ponce; Phénocristal; Chambre magmatique; Magma basique; Association minérale; Mer Egée; Pillow lava; Pyroclastique; Terre rare; Donnée microsonde électronique; Volcan Nisyros</FD><FG>Roche volcanique; Roche ignée; Mer Méditerranée Est; Mer Méditerranée</FG><ED>magmas; melange; trace elements; volcanic arcs; Quaternary; andesites; rhyodacites; calc-alkalic composition; chemical composition; fractional crystallization; chemical fractionation; pumice; phenocrysts; magma chambers; mafic magmas; mineral assemblages; Aegean Sea; pillow lava; pyroclastics; rare earths; electron probe data</ED><EG>volcanic rocks; igneous rocks; East Mediterranean; Mediterranean Sea</EG><SD>Magma; Mezcla; Análisis elementos traza; Cuaternario; Andesita; Riodacita; Composición calcoalcalina; Análisis químico; Cristalización fraccionada; Fraccionamiento químico; Piedra pómez; Fenocristal; Cámara magmática; Magma básico; Asociación mineral; Mar Egeo; Pillow lava; Piroclástico; Tierras raras; Dato sonda electrónica</SD><LO>INIST-17236.354000028033600040</LO><ID>93-0028457</ID></server></inist></record>Pour manipuler ce document sous Unix (Dilib)
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