A common origin of carbonatite magmas
Na-carbonatite lavas predominantly consist of nyerereite [Na 2 Ca(CO 3) 2] and gregoryite [(Na, Ca x, K) 2-x CO 3] phenocrysts embedded in a heterogeneously quenched matrix of Ba-rich nyerereite, gregoryite, Na-sylvite, fluorite, and quenched Ba-Ca-Sr-Na carbonate solid solutions (Gittins and Jago, 1998).The formation of Na …
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