On the relative stability of talc, anthophyllite, and enstatite

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ID: 298864
1962
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Abstract
Over a limited range of conditions between 670 degrees to 800 degrees C. at 2000 bars it has been found possible to convert talc to anthophyllite + quartz, and enstatite + quartz to anthophyllite, in the presence of water. The concept that anthophyllite can be formed only in the water-deficient region is thus untenable.
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openalex_W2035793906 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors W. S. Fyfe
Journal american journal of science
Year 1962
DOI
10.2475/ajs.260.6.460
URL
https://ajs.scholasticahq.com/article/58940.pdf
Keywords Keywords not found

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