Abstract
Melt inclusions in olivine and apatite, and REE distribution of apatite were studied in one of the least differentiated members of the oldest alkaline succession of Mt. Etna. Apatite occurs both as microphenocrysts and as inclusions in olivine crystals, even in the most Mg-rich ones (Fo82). In addition phenocrysts and groundmass are composed of plagioclase, clinopyroxene, olivine and magnetite.
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