geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3610Research ArticleНаучные сообщенияShort communicationsСклоновые ореолы рассеяния индикаторных минералов кимберлитов в геоморфологических условиях севера Сибирской платформыSlope dispersion aureole of kimberlee mineral detectors under the geomorphological conditions of the northern part of Siberian platformНовиковИ. С.NovikovI. S.ДакА. И.DuсkA. I.ОИГГиМ СО РАН, НовосибирскРоссия199916012024049299Copyright © Новиков И.С., Дак А.И., 20242024Новиков И.С., Дак А.И.Novikov I.S., Duсk A.I.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/3610

Complex geomorphological development of the territory under consideration caused the existence of several subhorizontal denudation surfaces within the height's range of 105-350 m. Uncorisolidated sediments of low thickness occurring on these surfaces serve as intermediate collectors. Their erosion makes the pattern of recent slope aureoles rather complicated and causes their propagation up the slopes and over local watersheds.

Complex geomorphological development of the territory under consideration caused the existence of several subhorizontal denudation surfaces within the height's range of 105-350 m. Uncorisolidated sediments of low thickness occurring on these surfaces serve as intermediate collectors. Their erosion makes the pattern of recent slope aureoles rather complicated and causes their propagation up the slopes and over local watersheds.

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