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Accessory, 10-300 μm grains of Sr-apatites with SrO contents up to 33 wt% were found in a high pressure (26 ± 3 kbar, 830 ± 30 °C), garnet-rich rock from the Bohemian Massif, Czech Republic. Furthermore, this rock contains unusual, Sr-bearing, accessory monazite (SrO up to 2 wt%). It is argued that the Sr-apatite and the Sr-bearing monazite formed as a result of plagioclase breakdown during HP metamorphism.

Metamorphic formation of Sr-apatite and Sr-bearing monazite in a high-pressure rock from the Bohemian Massif