Base level and lithology affect fluvial geomorphic evolution at a tectonically active area
The evolutionary history of fluvial geomorphology is the consequences of combined effects of tectonic, climate, lithology and base level. Previous researches had emphasized tectonic impacts on the fluvial system at the tectonically active region, while lithology and base level get little attention. In addition, the resistance of lithology may cause knickpoint and control the evolutionary history of landscape in relatively stable areas, and difference in local base-level is sufficient to induce drainage reorganization. Nevertheless, it is still unclear how far the lithology and base level affect the evolution of fluvial landforms in tectonically active areas.
In this study, researchers chose the area in the NE Tibet Plateau (Laohu and Hasi mountains) (Figure ...














