Turbidity currents distribute sediment across the seafloor, forming important archives of
tectonic and climatic change on the Earth's surface. Turbidity current deposition is affected …

Stable supercritical‐flow bedform phases under two‐dimensional steady flow are
geometrically simple and include long‐wavelength cyclic steps at high Froude numbers and …

The depositional record of carbonate slopes provides a valuable archive of past
environmental and climatic changes. Modern carbonate slopes reveal morphological …

Turbidity currents can be characterized as net-erosive, net-depositional or net-bypassing.
Whether a flow is erosive, depositional or bypasses depends on the flow velocity …

Decimetre-scale cross-stratification is relatively rare in turbidites, yet it has been identified in
both ancient and modern systems. However, the type of bedform associated with cross …

The boundaries of deep-marine fan deposits have been targets of study over the past few
years due to their potential of stratigraphic traps in the oil and gas exploration. The onlap of …

Turbidity currents transport land-derived sediment to deep sea where their deposits form
large geological structures termed submarine fans. Given their large areal extent and high …

A turbidity current is the most prominent agent for transporting sediment from the continental
shelf to the basin floor. However, direct monitoring of modern turbidity currents is difficult to …