Abstract
Principles of the transportation mechanism for a large number of interacting discrete solid particles were developed thanks to the progress in physics and mechanics of granular media. Velocity fluctuations and nonelastic collisions of fragments or their aggregates lead to the liquefaction of the clastic mass-flow, providing its travel over a long distance and simultaneously producing its sorting and stratification. Results of laboratory and field investigations carried out during the last 15 years with the use of high-precision equipment showed that this transportation mechanism is typical of slumps, debris flows, grain flows, high-density turbidity currents, and bottom avalanche transport. The universality of this mechanism made it possible to simplify the classification of subaqueous gravitational processes, propose an idealized scheme of bottom erosion processes, and interpret the Bouma cycle sequence.
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Poliakov, A.S. Properties of Granular Media and Transportation Mechanism of Subaqueous Debris Flows. Lithology and Mineral Resources 37, 25–39 (2002). https://doi.org/10.1023/A:1013631421289
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DOI: https://doi.org/10.1023/A:1013631421289