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A series of piston cylinder experiments were conducted to determine the partition coefficient of Cu between amphibole and andesitic to rhyolitic silicate melts. The experiments were run at T=740–990°C, P=0.7GPa, oxygen fugacity (fO2) ranging from that of the Ni-NiO buffer (NNO) to 2.3 log units higher (NNO+2.3 and dissolved water in variable concentrations (under-saturated to saturated conditions)...
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