Volume self diffusion of oxygen in biotite muscovite and phlogopite
Values for the fractional approach to equilibrium for muscovite experiments were calculated using the equation for muscovite water fractionation from experimental data O NEIL and TAYLOR 1969; BOTTINGA and JAVOY 1973 103 In a muscovite H^O = X lO /T2 2 where 103 In a as A "0 muscovite H >0 the difference in o^O