Changes in geoenvironment upon the high-rise construction in Moscow
At present, the construction of high-rise buildings is intensely going on in Moscow, upon which the subsurface is being used to a substantial depth. The geological conditions vary considerably in Moscow, with karstified and fractured terrigenous carbonate deposits of the Carboniferous age occuring at a depth ranging from 5-10 to 100 m and three generations of river valleys of different age being known. The geological structure undergoes considerable changes upon the construction of buildings with deep foundations. The detailed survey of engineering geological conditions was performed at the construction site of a complex of Moscow government office buildings located at the territory of the Moscow City international business centre. The geoenvironmental changes have been analyzed at the construction site and the hazard of karst and suffosion development after the end of construction has been assessed for this site and for the ad- jacent area.
V.M.Kutepov N.G.Anisimova E.M.Gribov O.N.Eremina
Sergeev Institute of Environmental Geoscience RAS, Moscow,Russia
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
523-525
2009-09-09（万方平台首次上网日期，不代表论文的发表时间）