A new mechanism of the hydrocarbon synthesis in natural processes of the oil-gas formation is substantiated. It is shown that it can be actually realized only in the environment of a deep-seated high-temperature fluid: in fact, the principal, main, and important source of powerful energy in the lithosphere. Precisely here, hydrogen and carbon in the atomic, radical, and ionic forms, i. e. in the form of separate atoms or radicals and their ions (H, <$E roman H sup +>, C, <$E roman C sup +>, CO, <$E roman CO sup +>, CH, <$E roman CH sup +>, CH2, <$E roman CH sub 2 sup +>, etc.), interact actively with the hydrocarbon formation. Under the generally accepted conditions of the maximum reservation of hydrocarbon components in the Earth's crust (limits of temperature are 250 <$E symbol Р>C), the realization of the hydrocarbon synthesis upon the interaction of deep-seated hydrogen (most probably, in the molecular form H2) and sedimentary carbon is impracticable at all.

• Наумко Ігор Михайлович (геологічні науки)

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