Mineral paragenesis in the talc-water experimental hydrothermal system.
January 1, 1982
The talc-like gel was treated between 300o and 550oC at 1 kbar for 7, 30, 50, 120 and 200 days. The trends suggest that stevensite and/or corrensite are the stable minerals at <450oC. At 500o- 550oC, talc is stable.-K.A.R.
Citation Information
| Publication Year | 1982 |
|---|---|
| Title | Mineral paragenesis in the talc-water experimental hydrothermal system. |
| Authors | G. Whitney, D. D. Eberl |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | American Mineralogist |
| Index ID | 70011842 |
| Record Source | USGS Publications Warehouse |