Abstract:SUMMARYThe article presents the results of the interpretation of a complex geochemical study of the organic matter of samples of different age of Paleozoic rocks from wells in the southern part of the PreUrals foredeep. It was found that in all the studied oil and gas complexes (Lower Devonian -Frasnian, Frasnian -Tournaisian, Visean -Bashkir and Lower Permian) have their own syngenetic source rocks characterized by different generational potential and confinement to a particular litho-facies zones.
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