Aj. Vanloon et al., SHOCK-INDUCED RESUSPENSION DEPOSITS FROM A PLEISTOCENE PROGLACTAL LAKE (KLESZCZOW GRABEN, CENTRAL POLAND), Journal of sedimentary research. Section A, Sedimentary petrology and processes, 65(2), 1995, pp. 417-422
Several glaciolacustrine successions forming part of the Quaternary fi
ll of the Kleszczow Graben contain massive and widespread fine-grained
units that are abnormally thick and homogeneous. Field studies of suc
h a unit indicate that it is the result of rapid settling of particles
from a sediment cloud consisting of material that had once settled on
the lake bottom but were resuspended. The geological setting makes it
likely that the trigger mechanism responsible for the sediment cloud
in the lake water was a shock and that this shock (most probably an ea
rthquake) was caused by tectonic activity in the graben.