For the first time in DDD, we analyze and compare sterane biomarkers in oils (condensates) and bitumoides of the dispersed organic matter of rocks, the potential sources of oil and gas. A quite good correlation between them is established, however it is worse than that in tectonically quieter regions (Pripyat depression, Western Siberia). The conclusion is justified that it is stipulated by the different intensities of fluiddynamic processes at the late stages of development of the regions.

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