Mineral paragenesis in the talc-water experimental hydrothermal system.
American Mineralogist
By: G. Whitney and D. D. Eberl
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Abstract
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.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Mineral paragenesis in the talc-water experimental hydrothermal system. |
| Series title | American Mineralogist |
| Volume | 67 |
| Issue | 9-10 |
| Year Published | 1982 |
| Language | English |
| Publisher | Mineralogical Society of America |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | American Mineralogist |
| First page | 944 |
| Last page | 949 |