Structural-geomorphological analysis of the territory of the West Siberian Plate allowed us to establish its latest structural plan. Neotectonic regions (NO), regional and local newest structures, as well as weak zones and tectonic dislocations, have been identified. Automated interpretation and mapping using the method of V.P. Filosofov made it possible to clarify the boundaries of regional structures, identify the most extensive tectonic dislocations, and compare the obtained data.
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