Formation-evolutionary mechanism of large debris flow in semi-arid region, the northeastern Tibetan Plateau
Author:
Funder
the Second Tibetan Plateau Scientific Expedition and Research Program
the National Science Foundation of China
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s10346-024-02233-9.pdf
Reference98 articles.
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3. Askaripour M, Saeidi A, Mercier-Langevin P, Rouleau A (2022) A review of relationship between texture characteristic and mechanical properties of rock. Geotechnics 2:262–296. https://doi.org/10.3390/geotechnics2010012
4. Battista G, Schlunegger F, Burlando P, Molnar P (2022) Sediment supply effects in hydrology-sediment modeling of an alpine basin. Water Resour Res 58:e2020WR029408. https://doi.org/10.1029/2020WR029408
5. Blanckaert K (2010) Topographic steering, flow recirculation, velocity redistribution, and bed topography in sharp meander bends. Water Resour Res 46:W09506. https://doi.org/10.1029/2009WR008303
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