NissirosV1, Istex, Corpus, bibRecord, 000018

The potential for future explosive volcanism associated with dome growth at Nisyros, Aegean volcanic arc, Greece

Identifieur interne : 000018 ( Istex/Corpus ); précédent : 000017; suivant : 000019

The potential for future explosive volcanism associated with dome growth at Nisyros, Aegean volcanic arc, Greece

Auteurs : Karen St. Seymour ; Dimitrios Vlassopoulos

Source :

Journal of Volcanology and Geothermal Research [ 0377-0273 ] ; 1989.

RBID : ISTEX:6D32FF8D2A860499AE49BE30DD9F5B9B95A3E2D5

English descriptors

Abstract

Abstract: Monitoring of the explosivity-controlling parameters in magmas associated with dome growth in the Quaternary volcano at Nisyros, Aegean Sea involves determining the chemical composition, including dissolved volatiles (H2O, CO2, F, Cl, and S), of melt inclusions in phenocrysts and interstitial matrices in pre- and post-caldera volcanic products. Our results indicate that the volatile content of the pre-caldera magma was a dominant factor responsible for the catastrophic explosivity of the caldera-forming episode. The relatively high estimated volatile contents and apparent interstitial viscosities of the post-caldera magmas, as well as the geophysical evidence for the existence of an active magma chamber beneath Nisyros, all suggest that this volcano is presently dormant but has a high potential for future explosive volcanism.

Url:

https://api.istex.fr/document/6D32FF8D2A860499AE49BE30DD9F5B9B95A3E2D5/fulltext/pdf

DOI: 10.1016/0377-0273(89)90089-9

Links to Exploration step

ISTEX:6D32FF8D2A860499AE49BE30DD9F5B9B95A3E2D5

Le document en format XML

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<abstract lang="en">Abstract: Monitoring of the explosivity-controlling parameters in magmas associated with dome growth in the Quaternary volcano at Nisyros, Aegean Sea involves determining the chemical composition, including dissolved volatiles (H2O, CO2, F, Cl, and S), of melt inclusions in phenocrysts and interstitial matrices in pre- and post-caldera volcanic products. Our results indicate that the volatile content of the pre-caldera magma was a dominant factor responsible for the catastrophic explosivity of the caldera-forming episode. The relatively high estimated volatile contents and apparent interstitial viscosities of the post-caldera magmas, as well as the geophysical evidence for the existence of an active magma chamber beneath Nisyros, all suggest that this volcano is presently dormant but has a high potential for future explosive volcanism.</abstract>
<note type="content">Section title: Research paper</note>
<relatedItem type="host"><titleInfo><title>Journal of Volcanology and Geothermal Research</title>
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<titleInfo type="abbreviated"><title>VOLGEO</title>
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<originInfo><publisher>ELSEVIER</publisher>
<dateIssued encoding="w3cdtf">198907</dateIssued>
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<identifier type="ISSN">0377-0273</identifier>
<identifier type="PII">S0377-0273(00)X0148-5</identifier>
<part><date>198907</date>
<detail type="volume"><number>37</number>
<caption>vol.</caption>
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<detail type="issue"><number>3–4</number>
<caption>no.</caption>
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<extent unit="issue-pages"><start>205</start>
<end>380</end>
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<extent unit="pages"><start>351</start>
<end>364</end>
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<identifier type="DOI">10.1016/0377-0273(89)90089-9</identifier>
<identifier type="PII">0377-0273(89)90089-9</identifier>
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The potential for future explosive volcanism associated with dome growth at Nisyros, Aegean volcanic arc, Greece

The potential for future explosive volcanism associated with dome growth at Nisyros, Aegean volcanic arc, Greece

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