Abstract
The eastern part of the Russian Arctic sector remains an area of the Arctic Ocean least investigated with respect to its geological structure. Therefore, the efforts of many researchers are mainly focused on problems related to the structure of Arctic sedimen� tary basins in connection with their petroleum resource potential, evolution of key Arctic structures, type, and thickness of the Earth crust. Knowledge of the crustal structure is important for establishing the outer boundary of the continental shelf of the Russian Arctic region in connection with the corresponding claim to the UN commission [1].
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