| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6440998 | Lithos | 2012 | 15 Pages |
Abstract
⺠Metamorphic garnet occurs in altered rocks adjacent to the St. Eugene deposit in SE British Columbia. ⺠Garnet was stabilized by ~ 100 °C due to increases in Mn and Fe in the altered rocks. ⺠Pressure-temperature conditions of formation were 3.6-4.0 kbar, 490-510 °C. ⺠Kinetics affected the development of the metamorphic mineral assemblages. ⺠Garnet is an indicator mineral for hydrothermal mineralization under greenschist-lower amphibolite facies conditions.
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Authors
David R.M. Pattison, JennaLee D. Seitz,