SEISMO FACIES OF THE WESTERN FLANK OF THE NOVOSIBIRSK - CHUKOTKA THRUST ZONE

The results of a seismostratigraphic analysis of the western part of the Novosibirsk-Chukchi thrust zone in the eastern part of the Laptev Sea are presented. Seismic facies complexes identified with the structures of the thrust zone have been identified. It is shown that the structures of the western closure of the Novosibirsk-Chukchi thrust zone began to form in the lower part of the sedimentary cover, in the Late Jurassic, belong to the thrust type.