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 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 C6–C14 compounds reach the maximum (corresponding to %Ro ∼ 1.3). Above %Ro ∼ 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 C1–C5 yields for source rocks at ∼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 ∼1.3 %Ro, with its yields being 156 ml/g TOC, 100 ml/g TOC and 117 ml/g TOC for Ed3, Es1 and Es3 source rocks, respectively. This suggests that source rocks with %Ro