turbidity current वाक्य
उदाहरण वाक्य
मोबाइल
- From these turbidites the predicted history of turbidity currents in this area was determined, increasing the overall understanding of these currents.
- At the end of the canyon the turbidity current spreads out and creates giant fans of sediment that blanket the deep seafloor.
- Generally as soon as the flow begins to move, fluid turbulence results and the flow rapidly evolves into a turbidity current.
- Turbidity currents responsible for wave generation are interpreted as originating from slope failures on the adjacent Venezuela, Guyana and Suriname continental margins.
- Sediments were deposited in the ocean floor in the form of fans formed by turbidity currents off the side of a continental slope.
- It is now recognized that the vertical progression of sedimentary structures described by Bouma applies to turbidites deposited by low-density turbidity currents.
- In the long term numerical techniques are most likely the best hope of understanding and predicting three-dimensional turbidity current processes and deposits.
- A dense slurry of muds and sands accelerates towards the foot of the slope until the gradient levels off and the turbidity current slows.
- Much of this sediment is deposited from turbidity currents that have been channeled from the continental margins along submarine canyons down into deeper water.
- The extreme complexity of most turbidite systems and beds has promoted the development of quantitative models of turbidity current behaviour inferred solely from their deposits.
- In sedimentology, his most influential publications were on turbidity currents and their deposits, and on the origin of physical sedimentary structures and textures.
- When the bottom of the sea has a small inclination, for example at the continental slopes, the sedimentary cover can become unstable, causing turbidity currents.
- Turbidity currents are currents which flow downslope when an unstable mass of sediment that has been rapidly deposited on the upper slope fails, perhaps triggered by earthquakes.
- Oil and gas companies are also interested in turbidity currents because the currents deposit organic matter that over geologic time gets buried, compressed and transformed into hydrocarbons.
- Despite the variety of different landslides present in submarine environment, only slides, debris flow and turbidity currents provide a substantial contribution to gravity driven sediment transport.
- Turbidity currents can result in internal hydraulic jumps ( i . e ., hydraulic jumps as internal waves in fluids of different density ) in abyssal fan formation.
- Earthquakes have been linked to turbidity current deposition in many settings, particularly where physiography favors preservation of the deposits and limits the other sources of turbidity current deposition.
- Earthquakes have been linked to turbidity current deposition in many settings, particularly where physiography favors preservation of the deposits and limits the other sources of turbidity current deposition.
- By contrast, because the S1-S3 terminology describes sand-rich turbidites deposited by high-density turbidity currents, the S acronym derives from " Sandstone ".
- Turbidity currents are sudden disturbances of the normally quite deep marine environment and can cause the geologically speaking instantaneous deposition of large amounts of sediment, such as sand and silt.
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