Interactions between along-slope bottom currents and down-slope turbidity flows can create
a myriad of features and deposits. Despite numerous efforts to differentiate contourites from …

With the advent of widely available 3D seismic data, numerous workflows focused on
extracting subsurface stratigraphic information have been developed. We present here tools …

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 …

Deep-water sediment waves can be classified using a combination of grain size and wave-
forming process, although in some cases one or other of these criteria may be …

High-resolution multichannel 2-D and 3-D seismic data, primarily from upper fan reaches of
near-seafloor channel-levee systems on the Niger Delta slope and in the Arabian Sea …

Turbidity currents, and other types of submarine sediment density flow, redistribute more
sediment across the surface of the Earth than any other sediment flow process, yet their …

Abstract Large-scale (20 m to 7 km wavelength) bedforms are common on the seafloor, yet
there is a lack of consensus on how they form and thus what to call them. We conducted …

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 …

Quantifying the characteristics of the turbidity currents that are responsible for the erosion,
lateral migration and filling of submarine channels maybe useful for predicting the …