Fluorine-bearing garnets in Adirondack calc-silicates
John W. Valley, Eric J. Essene, D. R. Peacor
Abstract
John W. Valley, Eric J. Essene, D. R. Peacor
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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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