Engineering and geological characterization of the Mesozoic weathering crust

E. N. Skvaletskii

Vol 153

Pages:

204-205

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RUS

Research article

Modern problems of geotechnical and hydrogeological surveys

Engineering and geological characterization of the Mesozoic weathering crust

Authors:

E. N. Skvaletskii

About authors

Orenburg Branch, Mining Institute UrO RAS

Date submitted:

2002-06-23

Date accepted:

2002-07-30

Date published:

2003-03-20

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.

Сквалецкий Е.Н. К инженерно-геологической характеристике мезозойской коры выветривания // Записки Горного института. 2003. Т. 153. С. 204-205.

Skvaletskii E.N. Engineering and geological characterization of the Mesozoic weathering crust // Journal of Mining Institute. 2003. Vol. 153. p. 204-205.

References

Гидрогеология СССР Том XLIII. Оренбургская область / Под редакцией Е.И.Токмачева. М: Недра, 1972.
Ломтадзе В.Д. Инженерная геология. Инженерная петрология. JI: Недра, 1970.
Сергеев Е.М. Инженерная геология. М: Изд-во МГУ, 1982.

Engineering and geological characterization of the Mesozoic weathering crust

Abstract

References

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