Fig. 8From: Triassic magmatism on the transition from Variscan to Alpine cycles: evidence from U–Pb, Hf, and geochemistry of detrital mineralsTernary diagram showing compositional variation of garnets using electron microprobe; Py pyrope, Al almandine, Sp spessartine, Gr grossular, An andradite. The boundaries of the compositional fields (A, Bi, Bii, Ci, Cii and D) and their probable provenance were taken from Mange and Morton (2007)Back to article page