Folding that is directly related to fault activity is an important deformation feature that occurs
all over the world in mountain belts, accretionary wedges, fold-and-thrust belts, and intra …

Recent studies have pointed out a similarity between tectonics and slope tectonic-induced
structures. Numerous studies have demonstrated that structures and fabrics previously …

Abstract The Late Pleistocene Lisan Formation contains superb examples of soft-sediment
deformation generated during gravity-driven slum** and failure down extremely gentle (< …

Erosion of the seafloor is often interpreted to be the result of turbidity currents and reflects
their frictional and non-cohesive nature. However, evidence of the interaction between …

Submarine mass‐transport deposits are important in many ancient and modern basins.
Mass‐transport deposits can play a significant role in exploration as reservoir, seal or source …

Comparatively little work has been undertaken on how sedimentary environments and
facies changes can influence detailed structural development in slump sheets associated …

The correct identification of 'sedimentary'folds and fabrics created during gravity-driven
deformation of unlithified successions from those 'tectonic'structures formed during regional …

This paper examines a glacial diamictite-bearing succession from the upper Itararé Group
(Taciba Formation) in eastern Paraná Basin, Brazil. The object of study provides the …

Folds generated in ductile metamorphic terranes and within unlithified sediments affected by
slum** are geometrically identical to one another, and distinguishing the origin of such …

The role of mass transport deposits (MTDs) in redistributing sediment from the shelf-break to
deep water is becoming increasingly apparent and important in the study of basins. While …