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Nyerereite from carbonatite rocks at Vulture volcano: implications for mantle metasomatism and petrogenesis of alkali carbonate melts Research Article

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Central European Journal of Geosciences

Abstract

Vulture volcano displays a wide range of mafic to alkaline, carbonate-, and/or CaO-rich volcanic rocks, with subvolcanic and plutonic rocks together with mantle xenoliths in pyroclastic ejecta. The roles of magmatic volatiles such as CO2, S, and Cl have been determined from compositions and trapping temperatures of inclusions in phenocrysts, which include the Na-K-Ca-carbonate nyerereite within melilite. We surmise that this alkali carbonate crystallised from an appropriate carbonatitic melt at relatively high temperature. Carbonatitic metasomatic features are traceable throughout many of the mantle xenoliths, and various carbonatitic components are found in the late stage extrusive suite. There is no evidence that alkali carbonatite developed as a separate magma, but it may have been an important evolutionary stage. We compare the rare occurrence of nyerereite at Vulture with other carbonatites and with an unaltered kimberlite from the Udachnaya pipe. We review the evidence at Vulture for associated carbonatitic metasomatism in the mantle, and we suggest that low viscosity alkali carbonatitic melts may have a primary and much deeper origin than previously considered.

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Authors and Affiliations

  1. Dipartimento di Scienze della Terra Università G. d’Annunzio, 66100, Chieti, Italia

    Francesco Stoppa

  2. Department of Earth Sciences, University College London, WC1E 6BT, UK

    Adrian P. Jones

  3. V. S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences,, Novosibirsk, Russia

    Victor V. Sharygin

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  1. Francesco Stoppa
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  3. Victor V. Sharygin
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Stoppa, F., Jones, A.P. & Sharygin, V.V. Nyerereite from carbonatite rocks at Vulture volcano: implications for mantle metasomatism and petrogenesis of alkali carbonate melts Research Article. Cent. Eur. J. Geosci. 1, 131–151 (2009). https://doi.org/10.2478/v10085-009-0012-9

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