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American Mineralogist; April 1983; v. 68; no. 3-4; p. 444-448
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Fluorine-bearing garnets in Adirondack calc-silicates

J. W. Valley, E. J. Essene, and D. R. Peacor

Rice Univ., Dep. Geol., Houston, TX, United States

Several grossulars have been found to contain up to 0.76 weight percent fluorine substituted in the structure, equivalent to a 1.5 mole percent substitution of fluorine for oxygen. Retrogradation of wollastonite after the peak of Grenville regional metamorphism.--Modified journal abstract.

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