Genesis and diagnostic value of soft-sediment deformation structures—A review

Soft-sediment deformation structures are recognized as important diagnostic features in the rock record for determination of depositional environments and slope processes. The diagnostic value of these structures is reevaluated by analysis of the parameters controlling sediment deformation. Soft-sediment deformation is contemporaneous with deposition and occurs dominantly in course silt to fine sand. The high depositional rate, low permeability and low shear strength of grains within this sediment range maximize the occurrence of deformation. The dominant mechanisms responsible for sediment deformation include: (1) liquefaction or fluidization; (2) reverse density gradation; (3) slumping or slope failure; and (4) shear stress. In most cases a combination of these mechanisms occurs. The processes function in a continuum, producing features that are microscopic to megascopic in scale. It is shown that the processes, and thus the structures, are not environment specific. The true diagnostic value of the structures may be in defining hydrodynamic conditions, and in interpreting paleocurrents and paleoclimatic and paleoseismic events. Ultimately, for the best diagnostic results, soft-sediment deformation structures should be studied in association with all other available lithologic, structural and paleontological information.