Abstract
The article presents the results of structural and geomorphological analysis of the Taimyr Peninsula North-Eastern part. The main neotectonic structures of the region are identified. It is shown that the intensity of neotectonic processes increases in the North-East direction, which is due to the approach to the spreading zone of the Gakkel ridge in the Arctic ocean. In the same direction, the tectonic fragmentation of Taimyr, the height of mountain structures, and seismic activity are increasing.
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