Distribution features of the bentonite-bearing silty-sandy-clayey sequence of the Tarusian horizon (р Serpukhovian) of the northwest the Russian Platform
Authors:
About authors
- Research assistant G.V. Plekhanov Saint Petersburg State Mining Institute
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.
Область исследования:
Geology
Funding:
None
Similar articles
Study of the relationship between the process of discretization of coal during mining and electromagnetic emissions in the face
2002 V. E. Bolshakov
Identification of parameters of the fuzzy control system of the gas mode of a horizontal converter
2002 A. S. Anashkin
Development and research of a method for separating nickel and copper in solutions
2002 P. N. Devyatkin