Scaling properties of gravity-driven sediments
Recent field observations of the statistical distribution of turbidite and debris flow deposits are discussed. In some cases one finds a good fit over 1.5-2 orders of magnitude to the scaling law <i>N(h)</i> α <i>h<sup>-B</sup></i>, where <i>N(h)</i> i...
| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
1995-01-01
|
| Series: | Nonlinear Processes in Geophysics |
| Online Access: | http://www.nonlin-processes-geophys.net/2/178/1995/npg-2-178-1995.pdf |