| extending from Belgium, in the West, through the Ruhr District, Germany, to the Upper Silesian Coal Basin, Poland...and changes strike from ENE towards NNE through Slovakia, Poland and Hungary (Raumer et al., 2003; Froitzheim...hypogene occurrence described from Muránska Zdychava, Slovakia, as a result of hydrothermal metasomatic transformation...Nevertheless as being a common phyllosilicate also in the region under consideration it deserves a closer look at...and talc-magnesite deposits the latter one from Slovakia (Table 3). It is not anything out of the ordinary |
