Abstract
Comparison of the latest structural plan of the West Siberian plate with the dislocations of the basement and sedimentary cover allowed us to rank the latest plicative and disjunctive structures according to the degree of inheritance. As a result of the work carried out, inherited, reversed and newly formed plicative structural forms were established. It is noted that the prostrations of ancient structures differ from modern ones and inheritance occurs only in fragments. When comparing the newest faults with the oldest ones, inherited and newly formed discontinuous faults are noted. The newly discovered inherited structures can be considered as promising areas for the search for hydrocarbon deposits.
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