Fig. 8

Tectonic contact of the Miocene basal lacustrine sediments with the crystalline basement (Geresdlak, granite quarry). a Cross-section of the quarry and b its location in a map with observed outcrops over GoogleEarth satellite image; stereoplot shows orientation of the boundary faults between Carboniferous and Miocene rocks; c tectonic boundary in outcrop (see person in centre for scale); d granite blocks in the Miocene sand next to a fault plane. For the location of the map area please see Fig. 1b