TL;DR: The contourite paradigm was conceived a few decades ago, yet there remains a need to establish a sound connection between contourites, basin evolution and oceanographic processes.
TL;DR: In this article, the authors derived criteria for the recognition of contourite vs. turbidite deposits, based on the analysis of many seismic profiles from both published and unpublished sources.
TL;DR: In this paper, a slope model is proposed that is a debris-flow dominated setting with both non-channelized and channelized systems, based on fluid rheology and flow state.
TL;DR: In this paper, the authors proposed a new model for deep-water sedimentary systems based on the turbidity current paradigm and refinements proposed for massive sands, megabeds and immature turbidites.
TL;DR: In this paper, the authors discuss sediment transport and deposition in deep-water facies and depositional processes controls on sedimentation and sequences, including the role of plate tectonics and sedimentation.
Abstract: Part 1 Facies, processes, sequences and controls: sediment transport and deposition deep-water facies and depositional processes controls on sedimentation and sequences. Part 2 Deep-water basin elements: slope aprons and slope basins submarine canyons, gullies and valleys submarine fans sheet systems contourite drifts. Part 3 Plate tectonics and sedimentation: evolving and mature passive margins active convergent margins oblique-slip margins.