geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3258Research ArticleНаучные сообщенияShort communicationsГеоморфология и новейшая история междуречья Течи и Зюзелки (Зауральский пенеплен)Geomorphology and Cenozoic history of the Techa-Zyuzelka interfluvial areaКочкинБ. Т.KochkinB. T.ИГЕМ РАНРоссия199620032023027989Copyright © Кочкин Б.Т., 20232023Кочкин Б.Т.Kochkin B.T.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/3258

A complex of geomorphological and geological methods has been applied to studies of a poorly known region on The Trans-Uralian peneplain. Characteristics of the Cenozoic deposits and landforms provide a basis for the most widely spread planation surface to be attributed to the Late Miocene. Both older and younger surfaces are limited in their distribution. Vertical displacement values have been estimated for the Cenozoic faults. The ascertained tectonic movements are considered in their relation to denudation processes which modelled the present-day relief.

 

A complex of geomorphological and geological methods has been applied to studies of a poorly known region on The Trans-Uralian peneplain. Characteristics of the Cenozoic deposits and landforms provide a basis for the most widely spread planation surface to be attributed to the Late Miocene. Both older and younger surfaces are limited in their distribution. Vertical displacement values have been estimated for the Cenozoic faults. The ascertained tectonic movements are considered in their relation to denudation processes which modelled the present-day relief.

 

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