The Garnet to Majorite Transformation in Mafic Compositions

Computer Science

Scientific paper

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Scientific paper

The garnet to majorite transformation in mafic compositions is
controlled by bulk composition and the presence of silicate melt,
clinopyroxene, and silicate perovskite as well as pressure. Thus, the
use of empirical geobarometers based on garnet Si^{4+} and/or [Al^{3+}
+/- Cr^{3+}] (p.f.u) seems unjustified.

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