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An ultra-high-pressure metamorphic condition (~ 140 km) at ~ 950 °C is identified from a garnet -pyroxenite, containing primary supersilicic clinopyroxene, as a part of the mafic -ultramafic lenses enclosed in the Gfohl granulite at the Horni Bory quarry of the Bohemian Massif, Czech Republic. Petrological data indicate that the garnet-pyroxenite was isothermally (~ 900 °C) exhumed from the upper mantle (~ 140 km) to the lower crust (~ 50 km), and the supersilicic clinopyroxene was decomposed to sodic augite and quartz during the exhuma- tion. This ultra-high-pressure metamorphic evidence is the first to be derived from the mafic rock directly en - closed within the Horni Bory granulite in the Moldanubian zone of the Bohemian Massif.

journal of mineralogical and petrological sciences

An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet-pyroxenite in the Horní Bory granulite of the Bohemian Massif