Naziv vsebine
Convolute Lamination
Site
Central Southern Karavanks.
Notes
The undulations, confined to a thin set of laminae, were likely caused by current-drag/shear at the water-sediment interface, because slumping tends to affect thicker packages of sediment in a more chaotic manner. Triassic.
Further observations
The dark, possibly finer grained layer, might represent a settling phase after current drag/shear stopped.