Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 13. 1987. (Budapest, 1987)

the cooling evidenced by post-tectonic biotite and chlorite porphyroblasts formed mainly from garnet. 3. In a subsequent (second syn-tectonic) phase compactional (pressure shadow) structures were generated around the post-tectonic porphyroblasts (Plate 11:2). The gradual, continuous changes of the temperature are also reflected in the composition zoning of garnet grains (Fig. 4). In the internal part of the porphyroblast normal, bellshaped profiles characteristic for grain-growth under increasing temperature are common: Fig. 4 Composition zoning of garnet grains (electron microprobe data)