EXPERIMENTAL STUDIES OF CORDIERITE SATURA TION OF THE C-O-H FLUID COMPONENTS

Incorporation of hydrocarbons in the channels of cordierite crystallin e structure was experimentally proved. It is necessary for the basing of estimates of complex metamorphis fluid composition. It was found th at cordierite selectively incorporates water and corbon dioxide molecu les in relation to CH4, CO and othet components of C-O-H fluid. New ex perimental technique of CO-H2O, CH4 - H2O fluid generation and after r un gas phase composition measurement were developed.