11 a), MIs from different plutonic xenolith types do not show a clear trend, however, there is a group of MIs from hornblende gabbronorites, gabbronorites and the basaltic andesite sample at 3–6 wt%, H 2 O < 300 ppm CO 2 .
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Evidence from plutonic xenoliths for magma differentiation, mixing and storage in a volatile-rich crystal mush beneath St. Eustatius, Lesser Antilles.
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