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2014 | OriginalPaper | Chapter

6. System CaO–MgO–Al2O3–SiO2 Saturated with Silica

Author : Professor Tibor Gasparik

Published in: Phase Diagrams for Geoscientists

Publisher: Springer New York

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Abstract

The silica–saturated CMAS system includes assemblages with anorthite, kyanite, and quartz or coesite. Clinopyroxene coexisting with such silica–rich phases can dissolve an excess of silica charge balanced by vacancies in the M2 site. Such “non-stoichiometric” pyroxenes were first reported by Eskola [165] and synthesized by Mao [313]. Other natural occurrences were reported by Smyth [416] and McCormick [317]. The compositions of clinopyroxene with vacancies can be extrapolated to the end–member Ca0.5AlSi2O6. Following Khanukhova et al. [269], Gasparik and Lindsley [2] started to use for this component the name Ca–Eskola pyroxene (CaEs), and reported the synthesis of a pyroxene along the CaTs–CaEs join with up to 40 mol% of CaEs.

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Metadata
Title
System CaO–MgO–Al2O3–SiO2 Saturated with Silica
Author
Professor Tibor Gasparik
Copyright Year
2014
Publisher
Springer New York
DOI
https://doi.org/10.1007/978-1-4614-5776-3_6