Kovdor to Oldoinyo Lengai—The missing link in carbonatitic magma evolution

نویسندگان

چکیده

Abstract Experiments were conducted to test the hypothesis that interaction of a carbonatitic magma with quartz-rich rocks plays key role in shaping carbonatite complexes. The host represented by quartz, and was synthetic mixtures CaCO3, MgCO3, Na2CO3. With increasing distance from reaction between carbonate liquid quartz produced domain Na(Ca)-rich silicate glass, metasomatic wollastonite, diopside, forsterite, carbonate-rich domain. This zonation reproduces observed many complexes, e.g., Kovdor, Russia. experiments provide strong evidence magma/host-rock controls evolution complexes explains how Mg-Ca-carbonatitic magmas mantle can evolve produce natrocarbonatites associated alkaline at Oldoinyo Lengai, Tanzania.

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ژورنال

عنوان ژورنال: Geology

سال: 2022

ISSN: ['0091-7613', '1943-2682']

DOI: https://doi.org/10.1130/g50672.1