are used to demonstrate that isotopic variation and highly radiogenic isotopic compositions observed in Martinique lavas are acquired via assimilation of upper crustal sediments. Textural features and mineral trace element compositions in St Vincent plutonic xenoliths record polybaric fractional crystallization and melt mush reaction processes. These two processes control magma chemical evolution in mushes beneath the island and consequently influence the trace element compositions of St Vincent lavas. New issues of Marvel
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