Abstract

The assemblages quartz-K feldspar-plagioclase-sillimanite-cordierite-biotite-almandine and quartz-K feldspar-plagioclase-cordierite-biotite-almandine-hypersthene characterize a newly established biotite-cordierite-almandine subfacies of the hornblende-granulite facies. The two typomorphic reactions are:

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