geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1842Research ArticleНаучные сообщенияShort communicationsДифференциация тяжелых минералов в склоновых отложениях Северо-Востока СССРDifferentiation of heavy minerals in slope sediments of the North-Eastern part of the USSRАнаньеваЭ. Г.AnanyevaE. G.КолосоваГ. Н.KolosovaG. N.Московский государственный университет имени М.В.Ломоносова, Географический факультетСССР19770606202202Геоморфология4144Copyright © Ананьева Э.Г., Колосова Г.Н., 20222022Ананьева Э.Г., Колосова Г.Н.Ananyeva E.G., Kolosova G.N.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/1842

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.

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.

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The authors declare that there are no conflicts of interest present.