Origin of primitive ultra-calcic arc melts at crustal conditions — Experimental evidence on the La Sommata basalt, Vulcano, Aeolian Islands
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The experimental phase relations of a natural ultra-calcic arc basalt have been determined

Results are identical in critical aspects to those obtained previously on a synthetic ultra-calcic arc composition

Generation of primitive ultra-calcic melt leaves a clinopyroxene-rich residual source, either wehrlite or clinopyroxenite

Ultra-calcic arc compositions at Vulcano are generated at crustal pressures

They represent melts produced by the interaction between primary and clinopyroxene-rich wall-rocks

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