Abstract
Al-zoning data may be used to examine that part of the granulite P-T path along which pyroxene grew. The slope of the log K curves for the reaction CaTs + quartz = anorthite is negative below 20 kbar whereas that for jadeite + quartz = albite is positive, and the two may be combined to yield both pressure and temperature. A subregular quaternary activity model for the system CaTs-jadeite-diopside-hedenbergite was fitted for these calculations. Data for the following four granulite terranes were examined: the Grenville Province, Ontario; the Furua Complex, Tanzania; the Fiordland complex; the Pikwitonei area, Manitoba. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 1328-1343 |
| Number of pages | 16 |
| Journal | American Mineralogist |
| Volume | 76 |
| Issue number | 7-8 |
| State | Published - 1991 |
| Externally published | Yes |