Differentiation of heavy minerals in slope sediments of the North-Eastern part of the USSR

E. G. Ananyeva; G. N. Kolosova

Differentiation of heavy minerals in slope sediments of the North-Eastern part of the USSR

E. G. Ananyeva, G. N. Kolosova

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Abstract

Peculiarities are considered of material (lithologic-mineralogical) composition of slope sediments depending on slope-forming processes. Insignificant enrichment by heavy minerals was established of basal horizons of defluctional scree and defluctional slope deposits. Useful component concentration can't be expected in the sediments of solifluctional slopes.

About the Authors

E. G. Ananyeva

Московский государственный университет имени М.В.Ломоносова, Географический факультет
USSR

G. N. Kolosova

Московский государственный университет имени М.В.Ломоносова, Географический факультет
USSR

Review

For citations:

Ananyeva E.G., Kolosova G.N. Differentiation of heavy minerals in slope sediments of the North-Eastern part of the USSR. Geomorfologiya. 1977;(2):41-44. (In Russ.)