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

Identifieur interne : 000400 ( Main/Exploration ); précédent : 000399; suivant : 000401

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

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

Source :

RBID : Pascal:93-0028457

Descripteurs français

English descriptors

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


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<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>
<term>pillow lava</term>
<term>pumice</term>
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<term>rhyodacites</term>
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<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>
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<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
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