| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4684768 | Geomorphology | 2013 | 15 Pages |
Abstract
The analysed part of the margin of the BudÄjovice basin that is not fault controlled revealed geomorphic parameters that are not indicative for differential vertical displacements (Smf 1.30 to 4,16, SL up to 57, Vf 2.10 to 4.80). Concave-up stream profiles of creeks draining into the basin are characteristic for equilibrated streams.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Angelika Popotnig, Dana Tschegg, Kurt Decker,