Engineering and geological characterization of the Mesozoic weathering crust
Authors:
About authors
- Orenburg Branch, Mining Institute UrO RAS
Abstract
The thick (from 5 to 20 m and more) clayey weathering crust in the South Urals is a product of deep physical and chemical processing and disintegration of Paleozoic rocks in the Mesozoic. Clays (60%), medium and heavy loams (30-35%) prevail. The results of statistical processing of tests of 102 monoliths indicate the heterogeneity of properties, especially the strength characteristics of rocks.
Область исследования:
(Archived) Modern problems of geotechnical and hydrogeological surveys
Funding:
None
Similar articles
Physico-chemical basis and analysis of possibility of application of chemisorption mineral matrix technology for treatment of contaminated quarry water of bauxite mines
2003 V. M. Knatko, E. V. Shcherbakova, D. V. Smirnova, D. E. Asriyan, V. A. Yulin, M. V. Knatko, A. S. Ivanskii
The importance of V.D. Lomtadze's works in understanding the conditions of groundwater formation in sedimentary basins
2003 E. A. Baskov, V. V. Petrov
The use of isotope methods in the study of groundwater balance (Almeria, Spain)
2003 I. L. Kharkhordin, I. V. Tokarev
On the causes of oil contamination of the Ordovician horizon on the Izhora Plateau
2003 V. Yu. Abramov, M. S. Iskhakov, K. A. Soloveichik, I. L. Kharkhordin