Abstract
SummaryThe unusual assemblage ferroglaucophane-chloritoid-paragonite-garnet-muscovite-chlorite-quartz has been found in metapelites of the phyllite series, north-east of Neapolis, southern Peloponnese, Greece. The chemical compositions of the coexisting phases are given, and the physical and chemical constraints which may control the appearance of this assemblage are briefly discussed.
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