NissirosV1, PascalFrancis, Curation, bibRecord, 000063

Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics

Identifieur interne : 000063 ( PascalFrancis/Curation ); précédent : 000062; suivant : 000064

Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics

Auteurs : K. S. Seymour [Canada] ; D. Vlassopoulos

Source :

Journal of volcanology and geothermal research [ 0377-0273 ] ; 1992.

RBID : Pascal:93-0028457

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

A01	`01`	`1`		`@0 0377-0273`
A02	`01`			`@0 JVGRDQ`
A03		`1`		`@0 J. volcanol. geotherm. res.`
A05				`@2 50`
A06				`@2 3`
A08	`01`	`1`	`ENG`	`@1 Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics`
A11	`01`	`1`		`@1 SEYMOUR (K. S.)`
A11	`02`	`1`		`@1 VLASSOPOULOS (D.)`
A14	`01`			`@1 Concordia univ., geology dep. @2 Montreal PQ H4B 1R6 @3 CAN`
A20				`@1 273-299 @7 8`
A21				`@1 1992`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 17236 @5 354000028033600040`
A44				`@0 0000`
A45				`@0 1 p.1/2`
A47	`01`	`1`		`@0 93-0028457`
A60				`@1 P`
A61				`@0 A`
A64		`1`		`@0 Journal of volcanology and geothermal research`
A66	`01`			`@0 NLD`
C01	`01`		`ENG`	@0 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
C02	`01`	`2`		`@0 222A01`
C02	`02`	`X`		`@0 001E01F01`
C03	`01`	`2`	`FRE`	`@0 Magma`
C03	`01`	`2`	`ENG`	`@0 magmas`
C03	`01`	`2`	`SPA`	`@0 Magma`
C03	`02`	`2`	`FRE`	`@0 Mélange`
C03	`02`	`2`	`ENG`	`@0 melange`
C03	`02`	`2`	`SPA`	`@0 Mezcla`
C03	`03`	`2`	`FRE`	`@0 Analyse élément trace`
C03	`03`	`2`	`ENG`	`@0 trace elements`
C03	`03`	`2`	`SPA`	`@0 Análisis elementos traza`
C03	`04`	`2`	`FRE`	`@0 Arc volcanique`
C03	`04`	`2`	`ENG`	`@0 volcanic arcs`
C03	`05`	`2`	`FRE`	`@0 Quaternaire`
C03	`05`	`2`	`ENG`	`@0 Quaternary`
C03	`05`	`2`	`SPA`	`@0 Cuaternario`
C03	`06`	`2`	`FRE`	`@0 Andésite`
C03	`06`	`2`	`ENG`	`@0 andesites`
C03	`06`	`2`	`SPA`	`@0 Andesita`
C03	`07`	`2`	`FRE`	`@0 Rhyodacite`
C03	`07`	`2`	`ENG`	`@0 rhyodacites`
C03	`07`	`2`	`SPA`	`@0 Riodacita`
C03	`08`	`2`	`FRE`	`@0 Composition calcoalcaline`
C03	`08`	`2`	`ENG`	`@0 calc-alkalic composition`
C03	`08`	`2`	`SPA`	`@0 Composición calcoalcalina`
C03	`09`	`2`	`FRE`	`@0 Analyse chimique`
C03	`09`	`2`	`ENG`	`@0 chemical composition`
C03	`09`	`2`	`SPA`	`@0 Análisis químico`
C03	`10`	`2`	`FRE`	`@0 Cristallisation fractionnée`
C03	`10`	`2`	`ENG`	`@0 fractional crystallization`
C03	`10`	`2`	`SPA`	`@0 Cristalización fraccionada`
C03	`11`	`2`	`FRE`	`@0 Fractionnement chimique`
C03	`11`	`2`	`ENG`	`@0 chemical fractionation`
C03	`11`	`2`	`SPA`	`@0 Fraccionamiento químico`
C03	`12`	`2`	`FRE`	`@0 Ponce`
C03	`12`	`2`	`ENG`	`@0 pumice`
C03	`12`	`2`	`SPA`	`@0 Piedra pómez`
C03	`13`	`2`	`FRE`	`@0 Phénocristal`
C03	`13`	`2`	`ENG`	`@0 phenocrysts`
C03	`13`	`2`	`SPA`	`@0 Fenocristal`
C03	`14`	`2`	`FRE`	`@0 Chambre magmatique`
C03	`14`	`2`	`ENG`	`@0 magma chambers`
C03	`14`	`2`	`SPA`	`@0 Cámara magmática`
C03	`15`	`2`	`FRE`	`@0 Magma basique`
C03	`15`	`2`	`ENG`	`@0 mafic magmas`
C03	`15`	`2`	`SPA`	`@0 Magma básico`
C03	`16`	`2`	`FRE`	`@0 Association minérale`
C03	`16`	`2`	`ENG`	`@0 mineral assemblages`
C03	`16`	`2`	`SPA`	`@0 Asociación mineral`
C03	`17`	`2`	`FRE`	`@0 Mer Egée @2 NG`
C03	`17`	`2`	`ENG`	`@0 Aegean Sea @2 NG`
C03	`17`	`2`	`SPA`	`@0 Mar Egeo @2 NG`
C03	`18`	`2`	`FRE`	`@0 Pillow lava`
C03	`18`	`2`	`ENG`	`@0 pillow lava`
C03	`18`	`2`	`SPA`	`@0 Pillow lava`
C03	`19`	`2`	`FRE`	`@0 Pyroclastique`
C03	`19`	`2`	`ENG`	`@0 pyroclastics`
C03	`19`	`2`	`SPA`	`@0 Piroclástico`
C03	`20`	`2`	`FRE`	`@0 Terre rare`
C03	`20`	`2`	`ENG`	`@0 rare earths`
C03	`20`	`2`	`SPA`	`@0 Tierras raras`
C03	`21`	`2`	`FRE`	`@0 Donnée microsonde électronique`
C03	`21`	`2`	`ENG`	`@0 electron probe data`
C03	`21`	`2`	`SPA`	`@0 Dato sonda electrónica`
C03	`22`	`2`	`FRE`	`@0 Volcan Nisyros @4 INC`
C06				`@0 ANS @0 TAS @0 ILS`
C07	`01`	`2`	`FRE`	`@0 Roche volcanique`
C07	`01`	`2`	`ENG`	`@0 volcanic rocks`
C07	`01`	`2`	`SPA`	`@0 Roca volcánica`
C07	`02`	`2`	`FRE`	`@0 Roche ignée`
C07	`02`	`2`	`ENG`	`@0 igneous rocks`
C07	`02`	`2`	`SPA`	`@0 Roca ignea`
C07	`03`	`2`	`FRE`	`@0 Mer Méditerranée Est @2 NG`
C07	`03`	`2`	`ENG`	`@0 East Mediterranean @2 NG`
C07	`03`	`2`	`SPA`	`@0 Mar Mediterraneo Este @2 NG`
C07	`04`	`2`	`FRE`	`@0 Mer Méditerranée @2 NG`
C07	`04`	`2`	`ENG`	`@0 Mediterranean Sea @2 NG`
C07	`04`	`2`	`SPA`	`@0 Mar Mediterráneo @2 NG`
N21				`@1 354`

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Le document en format XML

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<s3>CAN</s3>
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<country>Canada</country>
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<author><name sortKey="Vlassopoulos, D" sort="Vlassopoulos, D" uniqKey="Vlassopoulos D" first="D." last="Vlassopoulos">D. Vlassopoulos</name>
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<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 wicri:level="1"><inist:fA14 i1="01"><s1>Concordia univ., geology dep.</s1>
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<series><title level="j" type="main">Journal of volcanology and geothermal research</title>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Aegean Sea</term>
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<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>
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<term>Phénocristal</term>
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<term>Magma basique</term>
<term>Association minérale</term>
<term>Mer Egée</term>
<term>Pillow lava</term>
<term>Pyroclastique</term>
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<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>
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</fA11>
<fA14 i1="01"><s1>Concordia univ., geology dep.</s1>
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<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>
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<fC02 i1="02" i2="X"><s0>001E01F01</s0>
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<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>
</inist>
</record>

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Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics

Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics

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