Abstract
Two new geobarometers for the assemblage garnet + hornblende + plagioclase + quartz have been calibrated on the basis of the equilibrium 6 anorthite + 3 tremolite = 2 grossular + 1 pyrope + 3 tschermakite + 6 quartz and its Fe end-member equivalent. Data representing 37 natural samples that equilibrated at conditions of 2.5 to 13 kbar and 500 to 800°C were fitted to the general equation -RT ln Keq = A-BT+(P-1)C by using a weighted least-squares method. Application of the calibrations to samples from southeastern Vermont near the Strafford Chester, and Athens domes documents relatively high pressure metamorphism (7 to 10 kbar) for these structures. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 89-96 |
| Number of pages | 8 |
| Journal | American Mineralogist |
| Volume | 75 |
| Issue number | 1-2 |
| State | Published - 1990 |
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