Abstract
The stability of phlogopite in the presence of quartz and diopside is of interest in the interpretation of biotite-bearing assemblages in granitic rocks and of biotite-clinopyroxene-amphibole assemblages in metamorphic rocks. This study, begun to compliment the studies of Luth (1967), Schairer (1954), and Shaw (1963), is now being abandoned and the results to date are presented herein. Numerous persons have contributed to the study. Starting materials were contributed by W.T. Pecora, J.F. Schairer, and H.S. Yoder. Laboratory assistance was provided by J.V. Chernosky, C.J. Duffy, H.R. Shaw, and J. Whitney. N. Chatterjee, W.C. Luth, and D.A. Hewitt discussed many aspects of the theoretical and applied aspects of the study. J.S. Huebner and M.E. Woodruff were particularly helpful in the acquisition of x-ray powder intensity data. J.V. Chernosky provided library access and working space at the Univ. of Maine, Orono, so that this manuscript could be finished in the midst of an active field season. Critical reviews by J.S. Huebner, R.A. Robie, D.B. Stewart and E-an Zen helped to improve the manuscript.
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© 1977 D. Reidel Publishing Company, Dordrecht-Holland
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Wones, D.R., Dodge, F.C.W. (1977). The Stability of Phlogopite in the Presence of Quartz and Diopside. In: Fraser, D.G. (eds) Thermodynamics in Geology. NATO Advanced Study Institutes Series, vol 30. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-1252-2_12
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DOI: https://doi.org/10.1007/978-94-010-1252-2_12
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