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The signs of inherited neotectonic development of the Mologo-Sheksna depression area

https://doi.org/10.31857/S043542812104012X

Abstract

The artThe article is devoted to the consideration of the contribution of tectonic and neotectonic processes to the formation of the Mologo-Sheksna depression, as well as clarification of its structural features and the nature of the inheritance of its formation. Lineament, morphological and morphostructural analyzes are used as a methodological approach. The Mologo-Sheksna depression, currently filled with the Rybinsk Sea, has signs of an inherited developing morphostructure. It is a graben-shaped depression with linear northeastern and southwestern sides. The depression is located above the graben, which is well expressed in the basement and the lower part of the cover complexes, and, also has an expression in the top of pre-Quaternary rocks. A depression was formed on the site of an area of insignificant tectonic subsidence, and the origin of its contrasting relief is mainly associated with the activity of glaciers, the traces of which were then partly smoothed out by late-post-glacial lakes and water flows. The development of the depression was influenced by the surrounding faults. This impact was expressed not so much by high-amplitude displacements (corresponding to the range of the topography or top of the surface of pre-Quaternary deposits), but by the formation of zone of weakness with increased fracturing, which controlled the manifestation of exaration and abrasion processes. Field studies confirmed the existence of an additional landscape lineament along the southwestern side of the depression, the formation of which can be explained by the existence of another zone of weakness with fractures above the Rybinsk Fault. Measurements of the orientation of fractures in outcrops in the near-edge part of the Sit’ River valley showed the coincidence of the strike of the main systems of fractures, basement faults and the main morphological elements of the area, in particular, the side scarp of the reservoir, which indicates its tectonic predetermination.

About the Authors

D. S. Zykov
Geological Institute of RAS
Russian Federation

Moscow



A. V. Poleshchuk
Geological Institute of RAS
Russian Federation

Moscow



S. Yu. Kolodyazhnyi
Geological Institute of RAS
Russian Federation

Moscow



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For citations:


Zykov D.S., Poleshchuk A.V., Kolodyazhnyi S.Yu. The signs of inherited neotectonic development of the Mologo-Sheksna depression area. Geomorfologiya. 2021;52(4):42–52. (In Russ.) https://doi.org/10.31857/S043542812104012X

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