Fig. 8From: Three generations of monazite in Austroalpine basement rocks to the south of the Tauern Window: evidence for Variscan, Permian and Eo-Alpine metamorphic eventsXenotime versus temperature diagram showing the published monazite-xenotime miscibility gap thermometer curves and the minimum formation temperatures of Variscan, Permian and Alpine monazite under studyBack to article page