A system, consisting of a modified Fisher and Zen representation of an end-member reaction model (CaO-MgO-SiO2-H2O-CO2quartz, talc, tremolite, magnesite, calcite, dolomite, fluid), is first calibrated using a fit of Greenwood's equation to experimental data. Secondly, the same system is calibrated using tabulated thermodynamic data. The two calibrations are used to study the relationships amongst solid-solution activity models, natural assemblages, bulk compositions and fluid geochemistry over a small area at Sofala, N.S.W., where previous work has mapped a series of reactions/invariant points∗∗The Sofala assemblages used here are inferred to have formed at 415°C, 2 kbar and so the words invariant point/reaction apply to assemblages which are in fact divariant/trivariant. in greenschist facies metamorphosed basic volcanics. Between the two calibrations, the calculations indicate that there are significant differences in a(H2O), as well as in a(CO2), which are primarily related to significant differences in ΔSf(solids). A data table, necessary for the calculations, is given for the apparent free energy of formation of CO2 at P and T based on Perchuk and Karpov's work.The chemistry of the natural phases is considered in the modified Fisher and Zen equation through the use of various solid solution activity models and the mass action constant (K̄) for the solid phases in a reaction. For the Sofala rocks, this process suggests a mild preference for the first calibration and for the full Temkin activity model for solid solutions. In the first calibration, the magnesite-absent invariant point occurs twice in the interval 300–600°C, but the two occurrences approach each other, coincide, and then disappear below 0.5 kbar. The field of stability of the assemblage talc + calcite is shown to be sensitive to ø (the mole fraction of constituents other than molecules of H2O and CO2 in the fluid phase) that any implied pressure control can be reversed by 0 ≦ ø ≦ 0.05. A ln K̄ diagram reveals that the natural occurrences of the magnesite-absent invariant point imply 0 ≦ ø ≦ 0.1 at Sofala. The ln K̄ diagram also indicates that extensive dilution of the components in the end-member model (by extra components in the Sofala rocks) causes complete instability of the magnesite-absent invariant point and partial to complete instability of the reactions that define the invariant point. The ln K̄ diagram thus indicates the bulk compositions that are favourable for the existence of reaction/invariant points in the field.