The Formation Mechanism Of High-Steep Slopes Composed Of Huge Thick Loose Layer In The Strong Uplift Area Of The Qinghai-Tibet Plateau

DOI

10.2991/emim-15.2015.86How to use a DOI?

Keywords

Qinghai-Tibet Plateau; Loose deposition; Disaster; High-steep slope; Formation mechanism

Abstract

There exist many high-steep slopes composed of huge thick loose layer in part of (especially in the southeast of) the Qinghai-Tibet Plateau which is uplifting strongly, they are the development basis of large geological disasters such as landslide or debris flows. The slopes are the result of comprehensive effect of many loose deposition generated form crustal uplift effect mountain hazards effect such as large landslides and debris flows centrally handling accumulation and river sharp erosion slice effect.

Copyright

© 2015, the Authors. Published by Atlantis Press.

Open Access

This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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TY  - CONF
AU  - Bo Luo
PY  - 2015/04
DA  - 2015/04
TI  - The Formation Mechanism Of High-Steep Slopes Composed Of Huge Thick Loose Layer In The Strong Uplift Area Of The Qinghai-Tibet Plateau
BT  - Proceedings of the 2015 International Conference on Education, Management, Information and Medicine
PB  - Atlantis Press
SP  - 439
EP  - 444
SN  - 2352-5428
UR  - https://doi.org/10.2991/emim-15.2015.86
DO  - 10.2991/emim-15.2015.86
ID  - Luo2015/04
ER  -