Влияние активизированных докембрийских разрывных нарушений на рельеф котловины Ладожского озера

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.