Reflection of active faults in morphology of river channels crossing them and in the structure of channel alluvium (the Podkamennaya Tunguska river basin)

V. P. Borodin

Reflection of active faults in morphology of river channels crossing them and in the structure of channel alluvium (the Podkamennaya Tunguska river basin)

V. P. Borodin

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Abstract

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.

About the Author

V. P. Borodin

Красноярское геологическое управление, Геологосъемочная экспедиция
Russian Federation

Review

For citations:

Borodin V.P. Reflection of active faults in morphology of river channels crossing them and in the structure of channel alluvium (the Podkamennaya Tunguska river basin). Geomorfologiya. 1978;(2):47-52. (In Russ.)