On drainage of Lebedinsky open pit of KMA
Abstract
The Lebedinskoye deposit belongs to the Staro-Oskol group of iron ore deposits in the KMA. Precambrian crystalline rocks overlain by sedimentary deposits of Paleozoic and Meso-Cenozoic age are developed in the area of the deposit. Iron ores are confined to the upper part of the Precambrian crystalline formations and occur at a depth of 60-120 meters. The overburden is represented (from bottom to top) by: Upper Jurassic sandy, in some places dusty, clays and clayey sands (0.5-25 m thick), Apt-Albian sands (20-35 m thick), marl and chalky rocks of Santon-Cognac-Turonian age (5-60 m thick) and Quaternary loess-like loams (10-20 m thick).
Область исследования:
(Archived) Hydrogeology, engineering geology
References
- Verigin N. N. Groundwater movement near reservoirs, canals and methods of calculation of backwater and filtration losses. Proc. VODGEO (anniversary collection), Gosstroyizdat, 1958.
- Mironenko V.A. About application of horizontal wells at drainage of quarries. Proc. VNIMI, coll. XLYII, 1962.
- Mironenko V.A. To the question of stability of watered sandy slopes at the KMA quarries. University Proc., Geology and Exploration, 1962, No. 7.
- Shestakov V. M., Pavlovskaya L. N. Methodical instructions on filtration calculations of dewatering installations. Gosenergoizdat, 1961.