geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1903Research ArticleНаучные сообщенияShort communicationsОтражение активных разломов в морфологии пересекающих их русел рек и в строении руслового аллювия (бассейн р. Подкаменной Тунгуски)Reflection of active faults in morphology of river channels crossing them and in the structure of channel alluvium (the Podkamennaya Tunguska river basin)БородинВ. П.BorodinV. P.Красноярское геологическое управление, Геологосъемочная экспедицияРоссия19781406202202Геоморфология4752Copyright © Бородин В.П., 20222022Бородин В.П.Borodin V.P.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/1903

The influence of disjunctive tectonics is shown on the distribution of channel alluvium along the river profile as well as formation of shoals and bars (the case of the Podkamennaya Tunguska river basin), a possibility is proved of obtaining additional information on neotectonical structure of some region basing on the analysis of channel morphology and the character of channel alluvium.

The influence of disjunctive tectonics is shown on the distribution of channel alluvium along the river profile as well as formation of shoals and bars (the case of the Podkamennaya Tunguska river basin), a possibility is proved of obtaining additional information on neotectonical structure of some region basing on the analysis of channel morphology and the character of channel alluvium.

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