The Hydrogeological Feature and Geological Hazard Prevention of M Coal Mine in Xinjiang Fukang

Abstract:

M coal mine is located in the hilly terrain of mountain front in the southern margin of Junggar Basin in Fukang. The geological structure belongs to a medium type in the mine area where there are surface faults (two larger faults) and structural developments. The stratigraphic dips of south limb of Fukang syncline and southern Fukang anticline are large while that near F5 fault of anticline axis are larger and even upright. Brittle rocks develop fractures. In consideration of meteorology, earthquakes and other factors, mining may lead to such geological hazards as eboulement and surface subsidence, which should be highlighted.

• Periodical: Applied Mechanics and Materials (Volumes 405-408)
• Pages: 562-565
• DOI: https://doi.org/10.4028/www.scientific.net/AMM.405-408.562
• Online since: September 2013
• Authors: Chun Hui Yao, Qiu Hui Yao
• Keywords: Fault Structure, Geological Hazard, Hydrometeorology, Pevention

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