Modeling hydrocarbon generation from the Paleogene source rocks in Liaodong Bay, Bohai Sea: A study on gas potential of oil-prone source rocks

The exploration history of Bohai Sea reveals that Liaodong Bay is relatively rich in natural gas, which is mainly gas condensate; however, the source rocks in Liaodong Bay share a medium maturity level with values of %Ro being generally < 1.3. This study was undertaken to better understand gas potential of Paleogene oil-prone source rocks (II) in Liaodong Bay, Bohai Sea. Three immature Paleogene source rocks were selected to complete gold tube pyrolysis experiments. The experiment results reveal that the secondary gas from oil cracking can be neglected until the cumulative yields of C-6-C-14 compounds reach the maximum (corresponding to %Ro similar to 1.3). Above %Ro similar to 1.3%, oil starts to crack to wet gases substantially. Based on comparative analysis of pyrolysis results and source rock geochemical parameters, we constructed a hydrocarbon generation model, especially for hydrocarbon gas, and validated the calculated %Ro values for pyrolysis conditions. The C-1-C-5 yields for source rocks at similar to 1.3 %Ro in gold tube pyrolysis approximate the maximum gas yield for source rock in open system pyrolysis, indicating the majority of primary gas from kerogen cracking has been generated at similar to 1.3 %Ro, with its yields being 156 ml/g TOC, 100 ml/g TOC and 117 ml/g TOC for Ed(3), Es-1 and Es-3 source rocks, respectively. This suggests that source rocks with %Ro < 1.3 are of good primary gas generation potential. The extrapolation of kinetic parameters of C-1-C-5 shows that source rocks are generally at the stage of primary gas in Liaodong Bay, where proved gases are primary gas with estimated values of %Ro < 1.3. (C) 2014 Elsevier Ltd. All rights reserved.