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The Görcsöny Ridge is part of the complicated Variscan metamorphic basement of the SW Tisza plate. It was penetrated by several wells, one of which (Baksa-2) has 1200 m of well core available for petrological examination. Amphibolite samples of this core are of two different sorts: the fi rst group contains biot ite, rutile, and garnet, while the second group contains ilmenite and is free of garnet. The two rock types occur separately in the borehole, defining a lower and an upper unit (LU,doi:10.4154/gc.2014.02 fatcat:ogpk4txbunguvcw2wyhteim6ma