Phase equilibria among calcite, diopside, dolomite, enstatite, forsterite, quartz, talc and tremolite in the system CaO-MgO-SiO//2-CO//2-H//2O are calculated. The data for standard enthalpy of formation of diopside and tremolite are corrected by comparison with T-X//C//O//2 diagrams.
|Number of pages||24|
|Journal||Waseda Daigaku Rikogaku Kenkyusho Hokoku/Bulletin of Science and Engineering Research Laboratory,|
|Publication status||Published - 1982 Jan 1|
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