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It is generally accepted that the parental magmas of the Lesser Antilles arc were generated by partial melting of a mid-ocean ridge basalt (MORB)-type mantle source modified by slab-derived components. To determine the nature of these components, the H2O, S, Cl, F, Li and B contents and δ7Li, δ11B, δ18O and δ34S compositions were systematically determined in olivine-hosted melt inclusions from St....

Slab-Derived Fluids in the Magma Sources of St. Vincent (Lesser Antilles Arc): Volatile and Light Element Imprints