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We document the pressure–temperature structure of a mylonitized metamorphic pile in the Nagasaki Metamorphic Complex (NMC), western Kyushu, Japan, and we discuss the role of advection of the lower crust in the formation of this metamorphic pile. The NMC consists of upper and lower units. The upper unit is a mylonitized metamorphic pile that consists of metamorphic rocks of amphibolite to granulite...
Two types of reaction rims occur between olivine and plagioclase in ultramafic rocks from the Sefuri Mountains, NW Kyushu, Japan, which were metamorphosed under granulite-facies conditions. One occurs as a thin film of orthopyroxene along the boundary between olivine and plagioclase (orthopyroxene zone). The other is composed of two zones: symplectite of calcic amphibole and spinel on the plagioclase-side...
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