The grain-size distribution of sediment particles is an important aspect of the architecture of submarine fans and lobes. It governs depositional sand quality and reflects distribution of particulate organic carbon and pollutants. Documenting the grain-size distribution of these deep-marine sedimentary bodies can also offer us an insight into the flows that deposited them. Submarine lobes are commonly assumed to linearly fine from an apex, meaning there should be a proportional relationship between grain size and distance from the lobe apex. However, not much detailed quantitative work has been done to test this hypothesis. Exposure of a 5 km long dip-section of basin-floor lobes in Clinoform 12, Battfjellet Formation, Spitsbergen, enable t...
Deep-water depositional systems are the ultimate sink for vast quantities of terrigenous sediment, o...
Submarine lobe fringe deposits form heterolithic successions that may include a high proportion of h...
Sediment is fractionated by size during its cascade from source to sink in sediment routing systems....
The grain-size distribution of sediment particles is an important aspect of the architecture of subm...
Submarine lobe dimensions from six different systems are compared: 1) the exhumed Permian Fan 3 lobe...
Submarine lobes have been identified within various deep-water settings, including the basin-floor, ...
Depositional models of sand-prone deep-water sheet systems are limited in the literature to those th...
Submarine lobes are high aspect ratio sand-rich deposits fed by sediment gravity flows via channels....
Deposits within the floor of the Norwegian Basin were sampled to characterize the deposition from th...
The width and depth of submarine channels change progressively as the channels evolve. This is infer...
Submarine lobe-fringe deposits form heterolithic successions that may include a high proportion of h...
Seabed topography is ubiquitous across basin-floor environments, and influences sediment gravity flo...
Seabed topography is ubiquitous across basin-floor environments, and influences sediment gravity flo...
The growth style and evolution of syn-sedimentary faults influence the architecture of the basin and...
AnsTRAcr: A comparison of outer fan sections from different parts of the Kongsfjord Formation Submar...
Deep-water depositional systems are the ultimate sink for vast quantities of terrigenous sediment, o...
Submarine lobe fringe deposits form heterolithic successions that may include a high proportion of h...
Sediment is fractionated by size during its cascade from source to sink in sediment routing systems....
The grain-size distribution of sediment particles is an important aspect of the architecture of subm...
Submarine lobe dimensions from six different systems are compared: 1) the exhumed Permian Fan 3 lobe...
Submarine lobes have been identified within various deep-water settings, including the basin-floor, ...
Depositional models of sand-prone deep-water sheet systems are limited in the literature to those th...
Submarine lobes are high aspect ratio sand-rich deposits fed by sediment gravity flows via channels....
Deposits within the floor of the Norwegian Basin were sampled to characterize the deposition from th...
The width and depth of submarine channels change progressively as the channels evolve. This is infer...
Submarine lobe-fringe deposits form heterolithic successions that may include a high proportion of h...
Seabed topography is ubiquitous across basin-floor environments, and influences sediment gravity flo...
Seabed topography is ubiquitous across basin-floor environments, and influences sediment gravity flo...
The growth style and evolution of syn-sedimentary faults influence the architecture of the basin and...
AnsTRAcr: A comparison of outer fan sections from different parts of the Kongsfjord Formation Submar...
Deep-water depositional systems are the ultimate sink for vast quantities of terrigenous sediment, o...
Submarine lobe fringe deposits form heterolithic successions that may include a high proportion of h...
Sediment is fractionated by size during its cascade from source to sink in sediment routing systems....