Suite of experiments that explore the influence of input discharge rate and minibasin shape on the fluid and sediment transport dynamics of turbidity currents. TDWB-21-1 and 21-4 represent mid-flux conditions and circular basins. TDWB-21-2 represents low flux condition and circular basin. TDWB-21-3 represents high flux condition and circular basin. TDWB-21-5 represents mid-flux condition and long but narrow basin. TDWB-21-6 represents mid-flux condition and short but wide basin
Intraslope basins, or minibasins, are important morphological features of the continental slope in b...
Turbidity currents are common in the waters around the world. They can be caused by earthquakes, col...
The hydrodynamics of density currents are difficult to study in the natural envi- ronment, whereas l...
The sea floor of intraslope minibasins on passive continental margins plays a significant role in co...
The sea floor of intraslope minibasins on passive contine ntal margins plays asignificant role in cont...
Depositional turbidity currents have filled many intraslope minibasins with sediment creating targe...
Reservoirs are one of the most important components of our hydraulic systems around the world, and t...
Underwater sediment density flows, including turbidity currents, are capable of transporting vast am...
Turbidity currents are a variety of subaqueous sediment-gravity flows, in which the suspension of se...
The principle transport agent in deep ocean environments are turbidity currents, avalanches of sedim...
Small intraslope basins (~100 km^2), or "minibasins," such as those found on the continental slope o...
A turbidity current is a particle-laden current driven by density differences due to suspended sedim...
ABSTRACT: The northern continental slope of the Gulf of Mexico is riddled with numerous subsiding di...
A turbidity current is a turbulent, particle-laden gravity current that is driven by density differe...
Flume experiments are conducted to model sediment-laden density currents with continuous suspension ...
Intraslope basins, or minibasins, are important morphological features of the continental slope in b...
Turbidity currents are common in the waters around the world. They can be caused by earthquakes, col...
The hydrodynamics of density currents are difficult to study in the natural envi- ronment, whereas l...
The sea floor of intraslope minibasins on passive continental margins plays a significant role in co...
The sea floor of intraslope minibasins on passive contine ntal margins plays asignificant role in cont...
Depositional turbidity currents have filled many intraslope minibasins with sediment creating targe...
Reservoirs are one of the most important components of our hydraulic systems around the world, and t...
Underwater sediment density flows, including turbidity currents, are capable of transporting vast am...
Turbidity currents are a variety of subaqueous sediment-gravity flows, in which the suspension of se...
The principle transport agent in deep ocean environments are turbidity currents, avalanches of sedim...
Small intraslope basins (~100 km^2), or "minibasins," such as those found on the continental slope o...
A turbidity current is a particle-laden current driven by density differences due to suspended sedim...
ABSTRACT: The northern continental slope of the Gulf of Mexico is riddled with numerous subsiding di...
A turbidity current is a turbulent, particle-laden gravity current that is driven by density differe...
Flume experiments are conducted to model sediment-laden density currents with continuous suspension ...
Intraslope basins, or minibasins, are important morphological features of the continental slope in b...
Turbidity currents are common in the waters around the world. They can be caused by earthquakes, col...
The hydrodynamics of density currents are difficult to study in the natural envi- ronment, whereas l...