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Own energy resources of sedimentary basins are not sufficient for their transformation into petroliferous basins. Typical of petroliferous basins pronounced dissipative systems features are determined by interaction of deep high-enthalpy fluid flows with fluid-rock systems of sedimentary cover and base-ment. Obvious underestimation of superdeep geodynamic, geothermic and fluid-geochemical factors is the common feature of tectonics, petrology, geochemistry, petroleum geology and metallogenetics in the second part of the 20th century.
The study of these superdeep fluids and mechanisms of their interplays with different lithosphera substrates is bound to become the main line of investigations in petroleum geology of XXI century. Recent researches data of geodynamics, geophysics, geochemistry, petrology testify that the deep upper-mantle (astenosphere, mantle-crust mixture) fluids and connected with them hydro-thermal ore- and hydrocarbon-forming systems are caused by fluids from Core - D" layer.
It is difficult if not impossible to appraise energy, hydrocarbons- and ore-generating potential of the Earth's interiors properly if to restrict our consideration of tectonosphere within volume of the Earth crust and Upper Mantle. Late in the XXth - early in the XXIth century new conception of "plume-tectonics" based on global seismic tomography, deep petrology and geochemistry has been developed. These data have demonstrated that the roots of tectonics and magmatism reach the Earth's Core. In the light of the plume-tectonics conception, having assumed a significance of new paradigma of the Earth's sciences in XXI century, the revision of the role of superdeep fluid must be made. From this viewpoint prigozhinites (policomponent mineral aggregates connected with superdeep fluids intrusion into Lithosphere) are of special interest. They are characterized by a number of special mineralogic and geochemic peculiarities. Dispersed particles of native metalls (intermetallic compounds, natural alloys and also carbides, nitrides, silicides and other mineral compounds unusual for the Earth crust rocks and fluids are established within different petroliferous reservoirs. Among them one ought to mention inclusions of metallic particles with the structures of solid-phases decay (Widmanstatten and other structures) are established. They can be treated as the direct evidence of superdeep fluids migration.
All the above allows to consider their substance as direct derivatives of fluids from the layer D" and Outer Liquid Core. It let us to make a principal new step forward in the investigation of those superdeep geospheres matter composion using direct but not circumstantial evidence. So assumption on presense of metals carbides in "barysphere" offered by Mendeleev 130 years ago is confirmed. It would be of decisive importance in the elucidation of the true role of superdeep fluids in the processes of hydrogenization, oil, gas and ore-bitumen fields formation
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