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Tectonic crustal disturbance of northeastern Yakutia


, : Tectonic crustal disturbance of northeastern Yakutia. Tikhookeanskaya Geologiya = Pacific Geology 1988(4): 50-54

The tectonic crustal disturbance in northeastern Yakutia is studied by the spatial location of the upper Mesozoic faults. It is shown that the density pattern of faults, ice bodies and their relation to seismic activity are interrelated with each other. Regions with a decreased density of faults are characterized by high seismic activity, but in this case they are weakly subjected to icing, and, on the contrary, where the quantity of crustal specific disturbance increases, its direct correlation with increasing the number of ice bodies is observed.

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