Synsedimentary disturbances in Middle Triassic carbonates of the Holy Cross Mts

Abstract

A number of synsedimentary disturbances resulting from mass movements, mainly unstable laminar systems, and occasionally mud flows, were noted in the Lower Muschelkalk of the Holy Cross Mts. The origin of these structures is discussed in the background of sedimentary conditions prevailing during the Lower Muschelkalk.