Distribution features of the bentonite-bearing silty-sandy-clayey sequence of the Tarusian horizon (р Serpukhovian) of the northwest the Russian Platform

A. S. Afonov

Vol 152

Pages:

11-14

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Research article

Geology

Distribution features of the bentonite-bearing silty-sandy-clayey sequence of the Tarusian horizon (р Serpukhovian) of the northwest the Russian Platform

Authors:

A. S. Afonov

About authors

Research assistant G.V. Plekhanov Saint Petersburg State Mining Institute

Date submitted:

2001-09-17

Date accepted:

2001-10-02

Date published:

2002-08-26

Abstract

The peculiarities of distribution of the bentonite-bearing silty-sandy-clayey sequence of the Tarusian stage are considered using materials of geological surveys of different years on scales 1:50 000 and 1:200 000 The result of generalization of all available materials was the construction of the schematic map of distribution of silty-sandy-clayey sediments of the Tarusian stage. It shows that the bentonite-bearing sediments are mainly confined to the west-northwestern part of the Carboniferous Plateau. The formation of this member is associated with the manifestation of a special hydrothermal-sedimentary type of lithogenesis in the northwestern part of the Russian Platform during the Serpukhov time.

Афонов А.С. Особенности распространения бентонитоносной алеврито-песчано-глинистой пачки тарусского горизонта (серпуховский ярус) северо-запада Русской платформы // Записки Горного института. 2002. Т. 152 . С. 11-14.

Afonov A.S. Distribution features of the bentonite-bearing silty-sandy-clayey sequence of the Tarusian horizon (р Serpukhovian) of the northwest the Russian Platform // Journal of Mining Institute. 2002. Vol. 152 . p. 11-14.

References

Харлашин А.П. Первая находка месторождения бентонитов в Северо-Западном регионе России / А.П.Харлашин, Н.Г Шатков, Н.Е.Уткина // Разведка и охрана недр. 1998. № 7-8.
Махлина Е.Н. Нижний карбон Московской синеклизы и Воронежской антеклизы / Е.Н.Махлина, М.В.Вдовенко, А.С.Алексеев. М.: Наука, 1993.

Distribution features of the bentonite-bearing silty-sandy-clayey sequence of the Tarusian horizon (р Serpukhovian) of the northwest the Russian Platform

Abstract

References

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