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Fluorine-bearing garnets in Adirondack calc-silicates

John W. Valley, Eric J. Essene, D. R. Peacor

Open publisher page 38 citations

Abstract

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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What this paper is about

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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OpenAlex reports 38 citations for this work. Citation counts describe recorded attention and do not establish research quality.

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Available abstract

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.

Key concepts: Fluorine, Metamorphism, Oxygen, Geology, Geochemistry, Wollastonite, Mineralogy, Chemistry

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