Research Article
Effects of Glacier and Geomorphology on the Mechanism Difference of Glacier-Related Debris Flow on the South and North Banks of Parlung Zangbo River, Southeastern Tibetan Plateau
Figure 1
Geological sketch map of the eastern Himalayan syntaxis (after [21, 22]); (Abbrs.: towns, BM-Bomi, ST-Suotong, TM-Tongmai, LY-Layue, LZ-Linzhi, ML-Milin, MT-Motuo. Faults, TZF-Tongmai–Zhongkang fault; TJF-Tongmai–Jinzhula fault; DMF-Dongjiu–Milin fault; MTF-Motuo fault. Numbers: 1-bitong debris flow; 2-dada rock avalanche-debris flow; 3-jiaolong debris flow; 4-cangguo debris flow; 5-zhataduo debris flow; 6-naha debris flow; 7-guxiang rock avalanche-debris flow; 8-suotong debris flow; 9-qiuzhu debris flow; 10-chidan debris flow; 11-songrao debris flow; 12-michong debris flow; 13-danka debris flow).