Assessment of the influence of activated Precambrian faults on the relief of the Ladoga Lake depression
Abstract
The established nature of the relationship between the spatial pattern of linear elements of the relief and the Precambrian faults of the Ladoga Lake basin suggests that the direct reflection of faults in the relief may be related to the neotectonic activation of disjunctive structures. According to the data of computer and analogue tectonophysical modeling we concluded, that this process occurs in the NE stretching environment and can be considered as a significant relief formation factor along with glacier activity, hydroisostatic movements and other processes.
About the Authors
A. O. AgibalovRussian Federation
Faculty of Geology, Department of Dynamic Geology, postgraduate student
A. A. Sentsov
Russian Federation
Laboratory of Seismotectonics and Seismic Microzonation, Research Scientist
V. A. Zaitsev
Russian Federation
Faculty of Geology, Department of Dynamic Geology, Head of the Section of Geocatastrophe Research, PhD in Geology and Mineralogy
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Review
For citations:
Agibalov A.O., Sentsov A.A., Zaitsev V.A. Assessment of the influence of activated Precambrian faults on the relief of the Ladoga Lake depression. Vestnik Moskovskogo universiteta. Seriya 5, Geografiya. 2019;(3):99-105. (In Russ.)