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Mineral paragenesis in the talc-water experimental hydrothermal system.

American Mineralogist

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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.

Additional Publication Details

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
Number of Pages:
6