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Vol 52 Iss. 2
Pages:
58-73
Download volume:
RUS
Article

Conditions of formation of Borovichi-Lubytyn refractory clays and their quality

Authors:
N. A. Ageyeva
Date submitted:
1966-08-06
Date accepted:
1966-10-27
Date published:
1966-12-09

Abstract

In the north-west of the RSFSR, the raw material base of the refractory industry is a group of refractory clay deposits in the Borovichi-Lubytinsky district of the Novgorod region. These deposits are exploited by the Borovichi Refractories Plant. In order to produce highly responsible fireclay refractories the plant needs dry, semi-dry and to a lesser extent plastic high refractory clays. Such clays are formed by large deposits at the deposits “Proletary”, “Bolshevik”, Ustye-Brynkino, im. Artema, etc. ...

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References

  1. Vikulova M. F. Influence of conditions of formation of Lower Carboniferous clays of the western part of the Moscow Basin on changes in their composition. In the book: Delta and Shallow-Water-Marine Sediments. PH of the AS USSR, 1963.
  2. Vishnyakov S. G. Lithologic sketch of the Tikhvin bauxite-bearing area. Gosgeolizdat, 1940.
  3. Gladovsky A. K., Ushitinskii I.N. On the material composition, origin and change of bauxites of the Tikhvin district. Proc. Mining and Geology Institute of the Ural Branch of the AS USSR, vol. 56, 1961.
  4. Goncharov V.V. Refractory clays of the Borovichi-Lubytinsky district. Metallurgizdat, 1952.
  5. Rukhin L.B. Basics of Lithology. L., Gostoptekhizdat, 1961.

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