Application of new experimental and garnet Margules data to the garnet-biotite geothermometer

M.J. Holdaway

doi:10.2138/am-2000-0701

Abstract

Garnet-biotite experiments now exist from Ferry and Spear (1978, FS), Perchuk and Lavrent'eva (1983, PL), and Gessmann et al. (1997, GE). Recent garnet Margules parameters exist from Berman and Aranovich (1996, BA), Ganguly et al. (1996, GA), and Mukhopadhyay et al. (1997, MU). A comparison of ∆G_mix plots for garnet binaries shows similarity among models with some significant differences. In all, 20 garnet-biotite geothermometers were retrieved from the various data using a modified form of the approach of Holdaway et al. (1997, HO) such that experimental vs. calculated values of T, in °C, were regressed stepwise to a line with intercept of zero and slope of one, maximizing r². All tests assumed the GA model for garnet MnMg and the HO Fe³⁺ correction and ∆W_Ti^Bio. The experimental combinations (sets) were: (1) GE + FS with GE values of ^VIAl^Bio in FS; (2) PL + FS with GE ^VIAl^Bio in FS; (3) PL + FS with GE ^VIAl^Bio in FS, increasing W^Gr_MnMg by 5 kJ; (4) PL + FS with no ^VIAl^Bio in FS, increasing W^Gr_MnMg by 5 kJ; (5) PL + FS with 0.10 ^VIAl^Bio in FS, increasing W^Gr_MnMg by 5 kJ; (6) PL + FS + GE with 0.10 ^VIAl^Bio in FS, increasing WGr_MnMg by 5 kJ. Models are designated by a number for the experimental set and letters to designate the above garnet model, e.g., 5BA.

Experimental sets vary in maximum r² as follows: (1) 0.892-0.896; (2) 0.943-0.956; (3) 0.943- 0.955; (4) 0.980-0.982; (5) 0.980-0.983; and (6) 0.939-0.944. Application to the HO Maine biotitegarnet data gives the following sequence of increasing quality from experimental sets: 1 < 2 < 3 < 6 < 4 ≡ 5. The various garnet models show only small differences in r² and in quality with the Maine data base. For all 20 models, average T (°C) for the Maine M3 staurolite zone varies between 554(15) and 588(13). The best models appear to be 5BA, 5GA, and 5MU, which allow for 0.10 ^VIAl in FS biotite. A model based on an average of the three garnet Margules models, 5AV, has some justification and provides a slight improvement. Model 5AV gives (in J) ∆G_ex = 40198 - 7.80T; W^Bio_FeMg = 22998 - 17.40T; ∆W_Al^Bio = 245559 - 280.31T , and Maine M3 average staurolite zone T = 571(12) °C. The high quality of sets based mainly on PL experiments (2-5 above) results in part from their experimental P of 6 kbar. The results suggest that FS biotite contained only minor ^VIAl. The wide ranges of derived exchange and biotite Margules parameters, which provide reasonable calibrations, indicate that while accuracy in parameters is important, consistency is even more important. These geothermometers (5BA, 5GA, 5MU, 5AV) are available on PC disk. I recommend geothermometer 5AV.

Application of new experimental and garnet Margules data to the garnet-biotite geothermometer

Abstract

Articles in the same Issue

Articles in the same Issue