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Crystal Structure of Correianevesite from the Emmons Pegmatite, Uncle Tom Mountain, Greenwood, Oxford County, Maine

Correianevesite is an uncommon secondary phosphate in granitic pegmatites. Electron microprobe analysis is used to obtain the chemical composition of the mineral and calculate the empirical chemical formula, and single-crystal diffraction data was used to determine and understand the crystal structure.

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Information

Authors
Pietro Vignola; Francesco Demartin; Italo Campostrini; Alexander U Falster; William B. "Skip" Simmons
Date
January 1, 2021
Source
Bulletin de la Société Royale des Sciences de Liège
Source (Long)
Bulletin de la Société Royale des Sciences de Liège 90:125-135

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