Late Eocene-Early Oligocene two-mica granites in NW Turkey (the Uludağ Massif): Water-fluxed melting products of a mafic metagreywacke
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文摘
The Uludað two-mica granites show high Na2O, CaO and Sr, and lower K2O and Rb contents relative to the S-type granites. Their Sr-Nd-Pb isotopic characteristics require a compositionally mixed source. Water-fluxed partial melting of a mafic metagreywacke at lower crustal depths seems likely.

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