Sediment-laden gravity currents, or turbidity currents, are density-driven flows that transport
vast quantities of particulate material across the floor of lakes and oceans. Turbidity currents …

Earth's surface is composed of a staggering diversity of particulate–fluid mixtures: dry to wet,
dilute to dense, colloidal to granular and attractive to repulsive particles. This material variety …

Deep-marine strata consisting of a sandy basal part overlain sharply by a muddier and mud-
clast-rich upper part are increasingly being recognized in the deep-marine sedimentary …

Turbidity currents are one of the most significant means by which sediment is moved from
the continents into the deep ocean; their properties are interesting both as elements of the …

Clean basal and capping argillaceous sandstone couplets in deep water settings have been
previously interpreted as the result of spatially segregated turbidity currents and debris flows …

Understanding the transitional-sediment-gravity flow is essential to predicting the quality of
hydrocarbon reservoirs because the transitional flow is an important carrier of muddy sands …