Fig. 4From: Three generations of monazite in Austroalpine basement rocks to the south of the Tauern Window: evidence for Variscan, Permian and Eo-Alpine metamorphic eventsTh* vs. Pb diagram after Suzuki et al. (1991) showing the trendlines defined through Alpine, Permian and Variscan monazite. Age bars on the right site are isochrones forced through 0Back to article page