Fig. 5From: Discovery of Ordovician–Silurian metamorphic monazite in garnet metapelites of the Alpine External Aiguilles Rouges Massifa–c Garnet zonations in almandine (Alm-50, due to scale), grossular (Grs), pyrope (Prp) and spessartine (Sps) components. Single analyses used for pressure and temperature calculations in Fig. 6 are marked with numbers. Position of biotite (Bt) and staurolite (Sta) enclosed in garnet are marked. a Garnet in mylonitic garnet gneiss with homogeneous pyrope-rich cores and rims with lower Mg and variable grossular (Ca). b, c Growth-zoned garnets with spessartine-rich cores in micaschistsBack to article page