Hierarchical classifications are used in the field of clastic deep-marine sedimentary geology
to assign spatial and temporal order to the sedimentary architecture of preserved deep …

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 …

Submarine lobe-fringe deposits form heterolithic successions that may include a high
proportion of hybrid beds. The identification of lobe-fringe successions aids interpretation of …

Sedimentary facies in the distal parts of deep‐marine lobes can diverge significantly from
those predicted by classical turbidite models, and sedimentological processes in these …

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

Hybrid event beds comprising both clean and mud‐rich sandstone are important
components of many deep‐water systems and reflect the passage of turbulent sediment …

Deposits of sediment gravity flows in the Aberystwyth Grits Group (Silurian, west Wales,
United Kingdom) display evidence that sole marks are suitable for reconstructing …

Observations from outcrop and subsurface datasets indicate that key stratigraphic surfaces
in ancient submarine slope successions are diachronous and form during periods of …

Flutes and tool marks are commonly observed sedimentary structures on the bases of
sandstones in deep‐water successions. These sole structures are universally used as …

Deepwater turbidite lobe reservoirs have massive hydrocarbon potential and represent one
of the most promising exploration targets for hydrocarbon industry. Key elements of turbidite …