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https://doi.org/10.1007/978-3-0348-4168-9rrhenian volcanic belt, i.e., from southern Tuscany to Latium and Campania on the Apennine coastal range, Aeolian Islands, Ustica, Etna, and Sardinia. Discrepancies exist as to the origin of these fluids. Most authors suggest that the metasomatizing fluids originate from dehydration of a subducted l

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