Fig. 8From: Deep structure of the Pieniny Klippen Belt in PolandSynthetic seismogram of borehole Bańska IG-1. GR gamma ray, VP_CS interval velocities from check shot, VP_well log interval velocities acoustic log, VP_seism. Process interval velocities from stacking process (calibration of time to depth conversion velocity model). Markers: Sz_top top of Szaflary Formation, En_top top of Eocene nummulitic limestone, BD base base of Biały Dunajec Unit, Bańska base base of Bańska UnitBack to article page