首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Geodynamic and hydrodynamic evolution of the Broad Fourteens Basin and the development of its petroleum systems: an integrated 2D basin modelling approach
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Geodynamic and hydrodynamic evolution of the Broad Fourteens Basin and the development of its petroleum systems: an integrated 2D basin modelling approach

机译:十四大盆地的地球动力学和水动力学演化及其石油系统的发展:综合二维盆地建模方法

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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 Forteens Basin. We analysed the influence oftime-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 Lowere 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.
机译:二维盆地综合模型的结果表明,沉积物负荷和天然气的产生都在广阔的Forteens盆地的超压历史中起着重要的作用。我们分析了断层随时间变化的渗透率对石油超压历史和演化的影响。我们倾向于断层的随时间变化的渗透率,这是最有可能的解释盆地近代静水条件,已知油田位置以及天然气发生位置和特征的选项。模型结果进一步表明,P9和Q1下白垩统油藏充油时间的差异,解释了所观测到的成藏油地球化学组成的差异。反转前装填的Q1油藏的生物降解和水洗性质与晚白垩世反转时期通过下白垩统储层单元的地形引起的浓水流一致。 P9区储油层的后期充注解释了所积累油的非生物降解特征。十四区的当前状况几乎是静水压力。总体而言,本文表明,古水动力条件和随时间变化的水文地质框架对盆地的石油系统产生了重大影响。

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