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The Tolbachik Volcanic Center: The composition of ejecta, phases of activity, a petrologic model
We present new geological and isotopic geochemical data on rock compositions at the earlier stage (basement, the shield edifice) in the evolution of the Tolbachik Volcanic Center and the basement plateau of Ushkovskii Volcano. We used additional material from the literature to get a general picture...
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Published in: | Journal of volcanology and seismology 2017-07, Vol.11 (4), p.235-265 |
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creator | Koloskov, A. V. Davydova, M. Yu Anan’ev, V. V. Kandrin, A. A. |
description | We present new geological and isotopic geochemical data on rock compositions at the earlier stage (basement, the shield edifice) in the evolution of the Tolbachik Volcanic Center and the basement plateau of Ushkovskii Volcano. We used additional material from the literature to get a general picture of the evolution of both centers of volcanism. The increasing concentrations of nearly all trace components (except Sr) combined with decreasing degrees of differentiation in most major components and Sr isotope ratios in rocks of the Tolbachik Center are controlled by the change from a lithospheric mantle reservoir to an asthenosheric one and by a decreasing degree of melting in the reservoirs (25–20% → 15–10% → |
doi_str_mv | 10.1134/S0742046317040042 |
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V. ; Davydova, M. Yu ; Anan’ev, V. V. ; Kandrin, A. A.</creator><creatorcontrib>Koloskov, A. V. ; Davydova, M. Yu ; Anan’ev, V. V. ; Kandrin, A. A.</creatorcontrib><description>We present new geological and isotopic geochemical data on rock compositions at the earlier stage (basement, the shield edifice) in the evolution of the Tolbachik Volcanic Center and the basement plateau of Ushkovskii Volcano. We used additional material from the literature to get a general picture of the evolution of both centers of volcanism. The increasing concentrations of nearly all trace components (except Sr) combined with decreasing degrees of differentiation in most major components and Sr isotope ratios in rocks of the Tolbachik Center are controlled by the change from a lithospheric mantle reservoir to an asthenosheric one and by a decreasing degree of melting in the reservoirs (25–20% → 15–10% → <5%). The change of mantle sources and the diminution of their endogenous activity may indicate a decay of the Tolbachik Center volcanism. Ushkovskii Volcano has no shield edifice, but the composition of this stratovolcano itself shows many signs indicating rocks of a basement plateau. Here, an asthenospheric mantle reservoir was evident at the very beginning, although the rocks show both island-arc and intraplate geochemical characteristics.</description><identifier>ISSN: 0742-0463</identifier><identifier>EISSN: 1819-7108</identifier><identifier>DOI: 10.1134/S0742046317040042</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Asthenosphere ; Components ; Composition ; Earth and Environmental Science ; Earth Sciences ; Ejecta ; Ejection ; Evolution ; Geochemistry ; Geology ; Geophysics/Geodesy ; Island arcs ; Isotope ratios ; Isotopes ; Magma ; Mantle ; Petrology ; Ratios ; Reservoirs ; Rock ; Rocks ; Volcanic activity ; Volcanism ; Volcanoes</subject><ispartof>Journal of volcanology and seismology, 2017-07, Vol.11 (4), p.235-265</ispartof><rights>Pleiades Publishing, Ltd. 2017</rights><rights>Journal of Volcanology and Seismology is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-b6b64fc9ec4733fd62f9c3e102949ffa1a648dd208208e2dda36cccfccf75ffb3</citedby><cites>FETCH-LOGICAL-c316t-b6b64fc9ec4733fd62f9c3e102949ffa1a648dd208208e2dda36cccfccf75ffb3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Koloskov, A. V.</creatorcontrib><creatorcontrib>Davydova, M. Yu</creatorcontrib><creatorcontrib>Anan’ev, V. V.</creatorcontrib><creatorcontrib>Kandrin, A. A.</creatorcontrib><title>The Tolbachik Volcanic Center: The composition of ejecta, phases of activity, a petrologic model</title><title>Journal of volcanology and seismology</title><addtitle>J. Volcanolog. Seismol</addtitle><description>We present new geological and isotopic geochemical data on rock compositions at the earlier stage (basement, the shield edifice) in the evolution of the Tolbachik Volcanic Center and the basement plateau of Ushkovskii Volcano. We used additional material from the literature to get a general picture of the evolution of both centers of volcanism. The increasing concentrations of nearly all trace components (except Sr) combined with decreasing degrees of differentiation in most major components and Sr isotope ratios in rocks of the Tolbachik Center are controlled by the change from a lithospheric mantle reservoir to an asthenosheric one and by a decreasing degree of melting in the reservoirs (25–20% → 15–10% → <5%). The change of mantle sources and the diminution of their endogenous activity may indicate a decay of the Tolbachik Center volcanism. Ushkovskii Volcano has no shield edifice, but the composition of this stratovolcano itself shows many signs indicating rocks of a basement plateau. 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subjects | Asthenosphere Components Composition Earth and Environmental Science Earth Sciences Ejecta Ejection Evolution Geochemistry Geology Geophysics/Geodesy Island arcs Isotope ratios Isotopes Magma Mantle Petrology Ratios Reservoirs Rock Rocks Volcanic activity Volcanism Volcanoes |
title | The Tolbachik Volcanic Center: The composition of ejecta, phases of activity, a petrologic model |
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