Abstract
This paper shows that the location of large petroleum and gas hydrate deposits is related to deep ore-controlling fault zones. The large mercury deposits within these zones testify to the high differentiation maturity of the deep and crustal fluids. The mercury mineralization in compound ore assemblages is considered as the main indicator of their maturity (stable duration of development). The petroleum occurrences in Cenozoic sedimentary basins reflect only some partial changes in the location of hydrocarbon deposits with regard to the neotectonics and dynamics of the permafrost rocks.
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