Petrogenesis of migmatites and granites of the Western Papuk

Istraživano područje obuhvaća lokalitete Koturić, Jankovac, Zvečevo i Čarugin kamen, a pripadaju Papučkom metamorfnom kompleksu u zapadnom Papuku i Ravnoj gori. Uzorci predstavljaju granite, migmatite i gnajseve. Na temelju mikrofiziografije stijena, cjelostjenske geokemije, mineralne kemije i geotermobarometrije dobivene su informacije o p - T uvjetima postanka stijena (granit pri 3 kbar i 651°C te migmatit pri 5 kbar i 634°C), okolišu nastanka, geotektonskoj pripadnosti (VAG- graniti vulkanskog luka) i p - T putu koji se odvijao za vrijeme geneze stijena (''clockwise''). Također je potvrđena genetska veza s uzorcima obrađenim u literaturi.The examined area consist of localities of Koturić, Jankovac, Zvečevo and Čarugin kamen, all of which belong to the Papuk's metamorphic complex, located in western Mts. Papuk and Ravna gora. Samples consist of granites, migmatites and gneisses. Based on thin section microscopy, whole-rock geochemistry, mineral chemistry and geothermobarometry, information on p - T conditions during the formation of rocks (granite at 3 kbar and 651°C, and migmatite at 5 kbar and 634 °C), enviroment in which rocks were formed, geotectonical background (VAG – volcanic arc granites) and the p - T path that took place during the formation of said rocks (clockwise). Furthermore, genetic link was confirmed with samples previously analysed in literature