High-Mg adakitic rocks and their complementary cumulates formed by crystal fractionation of hydrous mafic magmas in a continental crustal magma chamber
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High-Mg adakitic rocks formed by crystal fractionation of hydrous mafic magmas

An example of preserved fractionating system (“adakites” and complementary cumulates)

Fractionation is important to Phanerozoic high Sr/Y rocks but not Archean granitoids

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