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The last eruption from Volcano Mountain produced young nephelinitic lava flows that remain unvegetated and appear to be only a few hundred years old.
Plume heads may be re-enriched by percolation of small-degree partial melts, such as nephelinitic magmas.
Low-viscosity carbonatitic liquids may separate from immiscible nephelinitic liquids at small degrees of melting with concomitant fractionation of incompatible elements.
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