The Upper Jurassic Bazhenov Formation in the central West Siberian Basin is a classic marine black shale unit containing abundant Type II kerogen with high oil‐generation potential. These shales source around 90% of the oil in the West Siberian Basin. They also contain oil accumulations in unconventional self‐sourced reservoirs. Reservoir zones are generally small and are located along fault planes. Primary oil migration was focused along fracture networks adjacent to the fault zones. Oil charging took place in the Tertiary and oil generation and expulsion in the Bazhenov Formation led to overpressuring. In the study area between the Surgut and Nyalinsk arches in the centre of the basin, faulting and fracturing took place in Eocene to Quaternary time. The faulting led to local increases in the thermal maturity of the Bazhenov Formation. Exploration risk in the self‐sourced Bazhenov Formation reservoirs mainly relates to seismically‐defined regional faults or to transverse faults.

Abstract. Creation technically of difficult construction projects is impossible alone. Project teams from among the certified specialists with a work experience are for this purpose formed. In Russia the civil engineer doesn't need the certificate. But without work experience of the young specialist don't take in a project team. It is possible to gain experience of team work during training in the program of a magistracy. In article experience of implementation in the Moscow State University of Civil Engineering of special discipline "Social, psychological and legal communications" is described. Content of a theoretical part and the organization of work on a practical training is stated. It is shown how the educational program helps students to purchase the social competences necessary for team work.

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SUMMARYThis work examines the importance of petrophysical studies salinization core, as it is a parameter that determines the strength and integrity of the breed in the process of development. Integrated assessment salinization manifold requires the use of petrophysical studies, chemical analysis of formation water, the method of 3D imaging that will allow us to represent the structure of the pore space and its changes in the process of leaching of salts.