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Univ. Iowa, Dep. Geol., Iowa City, IA, United States
Muscovite-bearing pelites near Rangeley, Maine. The proportion of muscovite-rich to biotite-rich pseudomorphs in the model is a function of the initial proportions of muscovite, plagioclase and staurolite, which govern the proportion of staurolite that is enclosed by sillimanite segregation mantles.--Modified journal abstract.
This record provided courtesy of AGI/GeoRef.
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J. M. Ferry Patterns of mineral occurrence in metamorphic rocks American Mineralogist, November 1, 2000; 85(11-12): 1573 - 1588. [Abstract] [Full Text] [PDF]
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