Indication of disastrous technogenic landslide development
The large landslide by a volume 1 million m3 took place on a brown-coal strip mine Urtysky in March 3-4, 2004. Analysis of the vertical and horizontal deformation development captured by mine survey, allows making a conclusion, that the strain characterizes impartially a condition of a slope massif and represents total parameter of all descending inside processes. It is offered to use critical value of relative deformation as a criterion for the estimation of section stability. The formation of a landslide is built into a definite phase of a space rhythm constituent of which is a relative position of the Sun, moon, planets, asteroids and the Earth. The active development of a landslide took place in the phase of growing Moon, when the water rising is observed including water lifting through tectonic fissures. High coal and rocks watering, reduction of rock resistance to land slide for 20-30 % and activating of suffusion processes contributed to landslide initiation.
A.M.Demine N.P.Gorbacheva A.B.Rulev
All-Russian Institute of Scientific and Technical Information of the Russian Academy of Sciences,Moscow,the Russian Federation
国际会议
International Symposium and The 7th Asian Regional Conference of IAEG(国际工程地质与环境协会年会暨第七届亚洲工程地质会议)
成都
英文
286-290
2009-09-09（万方平台首次上网日期，不代表论文的发表时间）