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Relevance of the work. According to current ideas and forecasts, the southern margins of the Pre-Caspian basin combines carbon-bearing massifs stretching from Astrakhan-Imashevsky elevation in the west to the South Embinsky one in the east. Within the margins, some large Paleozoic elevations associated with the carbonate development zones (the Kultuk Morskoy zone) have been identified with the help of geological and seismic methods. The determination of the structure of the carbonates zone of the southern margins in comparison with counterparts in the structures of adjacent areas of the earth (Karaton-Tengizsky bar and the South Embinsky elevation) poses the task of more detailed study for setting up prospecting drilling. Purpose of the paper is to substantiate the high prospects of local elevations of the Kultuk Morskaya zone in the Paleozoic complex, taking into account the use of the results of methods integration (seismic, airborne magnetic survey and gravity prospecting) obtained in recent years (2009-2013). Research methodology: comparative analysis of seismic data, anomalous magnetic field and gravity anomalies, including deep hole drilling data for recent years. Results. Taking into account the current understanding of the distribution of carbonate massifs, including the water area of the Northern Caspian, the structure of the southern border in the latitude band closer to the border with the Ustyurt-Bozashinsky basin was specified. The author gives a comparative analysis of the structure and development of carbonate deposits in the uplift areas of the South, Southwestern periclinal of the South Embinsky elevation and the Kultuk Morskoy zone, uniting the local structures of Sarytau, Burynshik, Burynshik Vostochny and Ostrovnaya. The justifying factors concerning the structural and tectonic unity of these areas are given. Based on the previously obtained results of prospecting works, lithofacial margins of the sludging basin in the southern border of the Caspian basin were justified; they are represented by carbonate massifs (Astrakhan-Imashevsky, Zhambai, Zhambai-More, Kultuk Morskoy, Yuzhnoye and South-Western periklinal of the South Embinsky elevation). Conclusions. Within the Kultuk Morskoy zone, taking into account the combination of data and features of the anomalous magnetic field and gravimetric anomalies, the high prospects of local structures of Sarytau, Burynshik, Burynshik Vostochny and Ostrovnaya are justified. On this basis, a forecast for the development of carbonates was made in the context of these structures, which in turn is based on favorable geological-geophysical, structural-tectonic and probable geoecological prerequisites.

Generalization of classical model of a displacement way on the transfer of heat exchange and mass exchange of a stream in the boundary layer, confirmed by the control action of the different nature, is undertaken. Here are given the results of numerical research which have allowed explaining the mechanism, to reveal efficiency and limits of various ways of management of intensity in exchange processes. The possibility of management of intensity in processes of a thermolysis and friction by use of the perforated surface with the damping cavities is analyzed.

In this paper, a decrease of turbulent pulsations of velocity in a boundary layer and the coefficient of friction drag for an accelerating flow on the perforated surface with blind damping cavities is experimentally found. We generalize the mathematical model of partial boundary layer laminarization [1], which is based on the experimental data [2, 3] obtained earlier on a decrease of the friction drag coefficient and deformation of average velocity profiles in the stabilized section of flow in the perforated tube with blind damping cavities.

Three versions of hybrid quadrupoles 2a0=15mm in aperture with shunting elements made of soft magnetic material (SMM) are analyzed. It is shown that Version 1 allows for gradient variation in the range of G=40-90 T/m and the regulation of magnetic center at Gmax during the rotation of external ring with shunting inserts. Authors have also analyzed the possibility to regulate the position of quadrupole magnetic axis by rotating additional rods made of hard magnetic material (HMM). The analysis has revealed that in Version 2 the radial displacement of shunts and components of their sections affect the magnetic parameters of the quadrupole. Finally, Version 3 of hybrid yokeless quadrupole is considered. The gradient variation and magnetic center regulation are provided by the radial displacement of HMM pole parts