Na2O-FeO-Al2O3-SiO2 & K2O-FeO-Al2O3-SiO2
Riebeckite thermodynamic data are now fitted to experiments of Ernst (1962) for the reaction rieb + 3hem = 2acm + 3mt + 4q + H2O. This equilibrium relies on the availability of data for acmite, which were retrieved on the basis of the reaction 2acm + pa + 2q = 3ab + hem + H2O. No experiments are available for this reaction, but it has occurred in the Eastern Alps at around 9 kbar and 450°C (Holland & Ray, 1985) in an assemblage with pure albite, hematite, paragonite and a sodic pyroxene of composition jadeite{44}acmite{56}. Thus data for both acmite and riebeckite must be regarded as provisional.
Data for ferroglaucophane are now fitted to the experiments of Hoffmann (1972) on the reaction 2fgl = 4abh + 3fa + q + 2H2O. These data are in agreement with the Fe-Mg exchange equilibria seen in natural assemblages (see the exchange section of table 7).
Data for annite, derived from the exchange reaction of Ferry & Spear (1978) also fit the experiments of Holdaway & Lee (1977) for the reaction 2ann + 6sill + 9q = 2san + 3fcrd + 2H2O.
241) 2fgl = 4abh + 3fa + q + 2H2O (Hoffmann, 1972) ln_K x(CO2) P(kbar) T(C) H(low) H(high) miss calc 2sd summary 0 0 3.0 340 370 247.91 257.62 351 28 2 (243.13 <-> 247.91) 0 0 5.0 350 370 236.77 243.14 27 397 30 cH = 251.49 (sd 5.22) 3 too high but OK uH = 1.71, d/s = -1.4, h = 0.47 242) rieb + 3hem = 2acm + 3mt + 4q + H2O (Ernst, 1962) ln_K x(CO2) P(kbar) T(C) H(low) H(high) miss calc 2sd summary 0 0 0.5 465 490 104.46 108.10 485 8 3 (106.57 <-> 108.18) 0 0 1.0 489 499 106.48 107.86 495 8 cH = 107.38 (sd 0.56) 0 0 2.0 511 516 107.71 108.38 -2 509 8 within bracket uH = 0.68, d/s = 0.1, h = 1.00 * 2ann + 6sill + 9q = 3fcrd + 2san + 2H2O (Holdaway & Lee, 1977) ln_K x(CO2) P(kbar) T(C) H(low) H(high) miss calc 2sd summary 1.60 0 2.1 1.9 640 270.85 273.32 -0.30 1.60 0.29 ** NOT USED ** 1.60 0 2.8 2.6 710 276.20 278.60 2.72 0.31 cH = 277.19 (sd 2.70)
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