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

(JA> • f <í$ • g ({(; * h © * i © -3 • e • 4 Fig. 3 Distribution of the main rock types in the ACF-ÁKF diagrams compared with the main rock types after WINKLER (1979). For rock types of Fig. 3a see Table 1. Legend for Fig. 3b: IA= Al-rich clays, IB= carbonate-free or max. 35% carbonate-bearing clays, between arrows: marls (with 35-65% carbonate content), 11= greywackes, 1= ultrabasic rocks, 2= basic and andesitic rocks, e= basalt, f= tonalité, g= granodiorite, h= calc-alkaline granite, 1= alkali granite, 3= continental clay, 4= marine clay clase, muscovite, biotite, graphite with preferred orientation in the foliation (sometimes microfolded) surfaces. 2. In the second phase post-tectonic helicitic garnet (Plate 1:2) and staurolite (Plate I: 3-4) porphyroblasts with folded graphitic inclusion-bands as well as "cross micas" penetrating and overgrowing the foliation planes of the matrix (Plate II: 1) were developed. Having reached the thermal climax the post-tectonic crystallization went on until a certain point of