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Hydrocarbon generation/expulsion modelling of the lower Paleozoic potential source rocks in the Gryfice and Kolobrzeg blocks (NW Poland)

机译:Gryfice和Kolobrzeg区块下古生界潜在烃源岩的生烃/驱替模型(波兰西北)

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摘要

The lower Paleozoic source rocks in the offshore part of the Gryfice and Kolobrzeg blocks (NW Poland) were studied through geochemi-cal data and numerical modelling. The geochemical study revealed a presence of effective source rocks in Caradocian strata, but with low hydrocarbon potential. The remaining lower Paleozoic source rock horizons were not documented by core samples. The timing of hydro-carbon generation and expulsion was modelled for the K1-1/86 and L2-1/87 boreholes located in the Gryfice and Kolobrzeg blocks, respectively. 1-D and 2-D modelling indicated that in the Kolobrzeg Block the onset of petroleum generation occurred at the end of the Silurian and the beginning of the Devonian. Source rocks in the Gryfice Block reached the early stage of oil generation at the beginning of the Permian and generation processes were completed by the end of the Triassic. Migration of hydrocarbons from source rocks began in the Carboniferous in both the Gryfice and Kolobrzeg blocks and lasted to the end of the Mesozoic. During hydrocarbon migration, an intensive dispersion process was observed, caused by leaking along the fault planes. The modelling revealed that hydrocarbons may have accumulated in Devonian reservoirs. The lack of any discovered accumulations could be the result of hydrocarbon dispersion caused by tectonic deformation and intense vertical fault block movements.
机译:通过地球化学数据和数值模拟研究了Gryfice和Kolobrzeg区块(西北波兰)近海的下古生界烃源岩。地球化学研究表明,卡拉多斯地层中存在有效烃源岩,但烃类潜力较低。剩余的下古生界烃源岩层位没有被岩心样本记录。分别针对位于格里菲采和科沃布热格区块的K1-1 / 86和L2-1 / 87钻孔模拟了油气生成和驱出的时间。一维和二维模型表明,在科沃布热格区块,志留纪末期和泥盆纪初生了石油。 Gryfice街区的烃源岩在二叠纪开始就达到了石油生产的早期阶段,而三叠纪末期已完成了生产过程。来自烃源岩的碳氢化合物迁移从格里菲采和科沃布热格的石炭纪开始,一直持续到中生代末期。在油气运移过程中,观察到强烈的弥散过程,这是由于沿断层面泄漏造成的。该模型表明,碳氢化合物可能已经聚集在泥盆纪储层中。缺乏任何发现的堆积物可能是由于构造变形和强烈的垂直断层块运动引起的油气扩散的结果。

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