Abstract

Results of integrated 2D basin modelling indicate that both sedimentary loading and gas generation play an important role in the overpressure history of the Broad Fourteens Basin. We analysed the influence of time-dependent permeability of faults on the overpressure history and evolution of petroleum systems. We favour time-dependent permeability of faults as the most likely option to explain the present-day near-hydrostatic conditions in the basin, the known location of oil fields, and the location and characteristics of the gas occurrences. The model results further show that the difference in timing of oil charging of the P9 and Q1 Lower Cretaceous oil reservoirs, explains the observed differences in geochemical composition of the accumulated oils. The biodegraded and water-washed nature of the pre-inversion charged Q1 oil reservoir is consistent with the concentrated topography-induced groundwater flow through the Lower Cretaceous reservoir units during the Late Cretaceous inversion period. Late charging of the oil reservoir in the P9 area explains the non-biodegraded character of the accumulated oils. Present-day conditions in the Broad Fourteens Basin are near-hydrostatic. In general, this paper shows that paleohydrodynamic conditions and time-dependent permeability of the hydrogeological framework have influenced significantly the petroleum systems in the basin.

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