Issues of the journals for 2010 y.

For classification of model descriptions of oil and gas reservoirs

(Kozhevnikov D.A. Kovalenko K.V. )

Effective (dynamic) porosity is an essential and sufficient criterion of the reservoir. Petrophysical model of the residual water saturation is a part of the effective porosity evaluation routine. There are few known models which describe dependence between residual water saturation and porosity. It is needed to systematize these models along with used parameters and approaches for understanding and analytical description of the filtration-capacity properties of the oil/gas reservoirs.......

  • 2010  № 5, pp. 66-70

Petrophysical connections at geological interpretation of data obtained by seismic inversion

(Kondratiev I.K. Bondarenko M.T. Kissin Yu.M. )

Forecasting of the capacity parameters of reservoirs according to the data of seismic inversion based on the connection between capacity parameters and acoustic impedance. However due to objective reasons it is not always possible to install representative or close enough interrelations. Practical examples demonstrate that in such cases geological connections of capacity parameters with each other can be useful.......

  • 2010  № 6, pp. 3-8

Geo-soliton model of hydrocarbon deposits generation in the North of Western Siberia

(MEGERJA V.M. Bembel R.M. Bembel M.R. )

This article gives an overview of morphological features of oil and gas hydrocarbon deposits of Northern areas of Western Siberia, Yamal and contiguous water areas of Kara Sea. The article discloses high degree of locality high-flow-rate sites and mosaic character of their spatial distribution. The author states that the solution of the genetic mechanism of formation of local centers of high-rate-flow zones predetermines not only methodology of exploration of hydrocarbon deposits, but also technology of reliable contouring and development. The certain features of a seismic wave field, revealed through processing and geological interpretation, are the signs of high-flow-rate areas. These features prove in the form of sub vertical zones of the lowered amplitudes, low sized positive structural forms and in the raised level of disseminated and diffracted waves.......

  • 2010  № 6, pp. 9-17