geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2818Research ArticleМетодика научных исследованийScientific Research MethodsО влиянии тектонического строения на размещение эрозионной сети на территории БелоруссииOn the tectonic control of the drainage network pattern in ByelorussiaНечипоренкоЛ. А.NechiporenkoL. A.ПавловскийА. И.PavlovskyA. I.Институт геохимии и геофизики АН БССРБеларусь19890112202202Геоморфология4145Copyright © Нечипоренко Л.А., Павловский А.И., 20222022Нечипоренко Л.А., Павловский А.И.Nechiporenko L.A., Pavlovsky 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/2818

Studies of spatial distribution of river and gullies revealed a certain tectonic control over the drainage network. River valleys of higher order are proved to be associated with subsided elements of the basement, with fault-lines of zones of contact between structures and blocks, sources of low order rivers are situated at neotectonic uplifts. Gullies formation is also typical for positive structures. An examination of fluvial erosion and debris transport directions permits to outline about 50 positive and negative blocks which undergo uplift or subsidence.

Studies of spatial distribution of river and gullies revealed a certain tectonic control over the drainage network. River valleys of higher order are proved to be associated with subsided elements of the basement, with fault-lines of zones of contact between structures and blocks, sources of low order rivers are situated at neotectonic uplifts. Gullies formation is also typical for positive structures. An examination of fluvial erosion and debris transport directions permits to outline about 50 positive and negative blocks which undergo uplift or subsidence.

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