Process-product studies have been central to the development of process sedimentology
over the past few decades, with the ability to first measure flows, and then examine the …

The distinction between turbidites, contourites and hemipelagites in modern and ancient
deep-water systems has long been a matter of controversy. This is partly because the …

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 …

A unique synthesis of grain size-distance data is presented, comparing, for the first time,
grain size and fining trends in a wide range of modern and ancient axial sediment dispersal …

The dimensions and dynamics of subaqueous bedforms are well known for cohesionless
sediments. However, the effect of physical cohesion imparted by cohesive clay within mixed …

Initial porosity and permeability in deep-water systems are controlled by primary
sedimentary texture and mineralogy. Therefore, understanding the sedimentary processes …

The fringe of fine‐grained deep‐marine systems often exhibits complex sedimentary facies
and facies associations, because the presence of clay promotes the development of …

Hybrid event beds comprising clay‐poor and clay‐rich sandstone are abundant in
Maastrichtian‐aged sandstones of the Springar Formation in the north‐west Vøring Basin …

Channel‐lobe transition zones are dynamic areas located between deepwater channels
and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone …

Hybrid event beds form when turbidity currents that transport or locally acquire significant
quantities of mud decelerate. The mud dampens turbulence driving flow transformations …