Deformations formed in unconsolidated sediments are known as soft-sediment deformation
structures. Their nature, the time of their genesis, and the state in which the sediments …

Cyclic steps are long-wave (the ratio of wavelength to height is≫ 1), upstream-migrating,
upper-flow-regime bedforms bounded by internal hydraulic jumps (ie, transition from …

Submarine sediment density flows are one of the most important processes for moving
sediment across our planet, yet they are extremely difficult to monitor directly. The speed of …

The deposits of subaqueous sediment gravity flows can show evidence for abrupt and/or
progressive changes in flow behaviour making them hard to ascribe to a single flow type (eg …

Submarine gravity flows are a key process for transporting large volumes of sediment from
the continents to the deep sea. The location, volume, and character of the sediment …

Hybrid flows comprising both turbidity current and submarine debris flow are a significant
departure from many previous influential models for submarine sediment density flows …

Sandy lobe deposits on submarine fans are sensitive recorders of the types of sediment
gravity flows supplied to a basin and are economically important as hydrocarbon reservoirs …

Turbidity currents are notoriously difficult to monitor directly, therefore interpretation of their
deposits forms the basis for much of our understanding of these flows. The deceleration rate …

Sedimentary facies in the distal parts of deep‐marine lobes can diverge significantly from
those predicted by classical turbidite models, and sedimentological processes in these …

This study documents the stratigraphic and palaeogeographic distribution of hybrid event
beds that comprise both debris-flow (cohesive) and turbidity current (non-cohesive) …