Reaction kinetics of gas generation in selected source rocks of the West Siberian Basin: implications for the mass balance of early-thermogenic methane

About one third of the actual global recoverable natural gas reserves is ac cumulated in the West Siberian Basin in several super-giant and mega-giant as well as numerous smaller gas fields. The elucidation of the nature of th is gas, its mechanisms of formation and accumulation are still a matter of discussion. For instance, it is still not yet clear whether the enormous dr y-gas accumulations in Cenomanian reservoirs are of microbial, 'early-therm ogenic' or catagenetic/metagenetic origin, or if they represent a mixture o f these possible formation mechanisms. The present contribution provides ne w results on the thermal gas generation properties of selected source rocks of the Cretaceous Pokur Formation in the West Siberian Basin. Eight select ed source rock core samples of the Pokur Formation and a recent peat sample of the same area were submitted to open-system programmed-temperature pyro lysis, in order to quantify the formation of individual gas compounds, i.e. , methane as well as C-2 and C-3 hydrocarbons. The rock samples were select ed according to geological age and maturity, i.e., from the Aptian, Albian, and Cenomanian, with the most immature samples from the latter. Organic ca rbon contents comprise the whole range from 3 to more than 60%, the elevate d values representing typical lignites. A reaction kinetic model system was applied to the 'generation curves' of the gases resulting in activation en ergy distributions and the corresponding pre-exponential 'Arrhenius factors '. The kinetic data were combined with the temperature history of two selec ted wells of the Urengoy area obtained from basin modelling in order to cal culate the gas generation on the geological time-scale. It was found that, even for the low temperatures occurring in the Pokur Formation, 'early' gas generation could have taken place to a certain, yet small, degree. Under t he assumption of a respective catchment area and the accumulation of this g as in the reservoirs, however, methane quantities are in the order of magni tude of the Urengoy gas accumulation. Thus, 'early-thermogenic' methane cou ld, at least partially, contribute to the gas accumulated in the reservoirs . (C) 1999 Elsevier Science B.V. All rights reserved.