The fundamentals of a new solution of the elaboration of oil-gas-searching technologies (methods) of a non-traditional type based upon the thermobarometry and geochemistry of gases of a veinlet-impregnated mineralization in the deposits of oil-gas-bearing areas and metallogenic provinces are grounded. They foresee the creation of new oil-gas-searching technologies and the realization of searching for hydrocarbon fields simultaneously with the elucidation of the problem of their genesis and synthesis at the atomic-molecular level fixed by defects in the crystals of minerals, fluid inclusions first of all. Based upon the theoretical premises and experimental data, a new technology for the determination of the prospects of oil-gas-bearingness of a local area is proposed, the probability of a revealing of which increases with the ratio of the hydrocarbon concentrations in inclusions of veinlet-impregnated minerals and in inclusions - defects of the rocks. The first original results provided by the approvement of the technology carried out within the scope of sedimentary oil-gas-bearing strata of the Carpathian Foredeep are presented.The notions about the thermobarometry and geochemistry of gases of veinlet-impregnated mineralization in the deposits of oil-gas-bearing areas and metallogenic provinces as the unique natural phenomenon of the Earth's lithosphere are substantiated and developed. This enables us to explain, from new positions, both the hydrocarbon synthesis and formation of actually veins and inclusions, to consider the fundamental problems of genesis, migration, and differentiation of paleofluids, formation of and searching for useful minerals of different genetic types. Proceeding from the results reached, it is determined that exactly a character of the distribution and the general composition of volatile components of fluid inclusions in veined minerals and rocks of potentially perspective strata is the most important indicator of genesis and a scale value of oil-gas rocks and many ore deposits (fields), especially gold. This is confirmed by the given results provided by investigations of the parageneses of veinlet-impregnated mineralization in the deposits of oil-gas-bearing areas and metallogenic provinces.It is established that the character of distribution and general composition of volatile-gaseous components of the fluid inclusions of veinlet-impregnated mineralization in the deposits of oil- and gas-bearing regions and metallogenic provinces appears to be one of the most important indications of the fixation of fluid-conducting fault zones, the occurrence of deep fluid flows in them, and the genesis and formation of oil, gas, and some ore deposits (first of all, gold-containing ones). Closeness of the composition and temperature conditions of the hydrocarbon conservation in inclusions of the vein minerals in series of different ages testifies to the simultaneousness or nearness of their migration through the fault zones in the vast territories of oil- and gas-bearing regions, including the Ukraine, and lets the reason to envisage their accumulation in structures-traps (under the favorable conditions) with formation of oil and gas deposits. The obtained results and the new theory of genesis and synthesis of natural hydrocarbons created by the authors from the positions of abiogenic dualism corroborate the views of the Corresponding member of the NAS of Ukraine M. R. Ladyzhens'kyi about that oil from the Carpathian fields contains a constituent originated via inorganic synthesis and migrated from depths through the regional fractures-faults with ultrahigh pressures in the course of a short period of time that also is not in conformity with the knowledge about the oil- and gas-bearing basins.Розроблено фізико-хімічну модель формування вугільних пластів, відповідно до якої вугільні пласти сформувалися з органічних решток в осадових шарах під дією метановмісного глибинного високотемпературного флюїду. Внаслідок субвертикально-міграційного втілення суміш метану разом з Ca(OH)2, CO2 і H2O (температурою понад 580 <$E symbol Р>C) піддала ці осадові товщі з потужним шаром органічних решток однонапрямленому потужному агресивному фізико-хімічному впливу та нагріла ці породи до температур, значно вищих за температури гомогенізації включень флюїду в новоутворених мінералах. Заліковування та цементація парових порожнин порід і дефектів у мінералах із утворенням прожилково-вкрапленої мінералізації та їх метанонасиченням спричинили консервацію метану як новоутвореними породами, так і вугіллям. Оскільки метан надходив у складі глибинного високотемпературного флюїду порожниною глибинного розлому, його концентрація в напрямі до розлому повинна зростати та мати зв'язок із можливим метановим покладом-родовищем.

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