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Integrated interpretation of potential field and seismic data for shale gas potential in the Karoo Basin, South Africa

机译:南非卡卢盆地页岩气势的潜在场和地震数据的综合解释

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Recent interest in the Karoo basin of South Africa has been sparked by the possibility of extensive shale gas reserves. Here we present an integrated study of historical reflection and refraction seismic (industry and academic), borehole, MT and regional gravity and magnetic data, with the goal of evaluating the shale gas potential. The reflection seismic data, constrained by 5 deep boreholes and MT data are used to map the contact between the base of the Karoo (Dwyka Group) and the underlying basement. This provides an important constraint on the thickness of the Karoo Supergroup (~5.5 km). By constraining the gravity data with the structure known from the reflection seismic and density data from boreholes, this contact can be extended to regions where the seismic data are sparse and suggests that the basin in the region near 24° longitude is thinner than on either side. The flexure of the basin also suggests that at the time of deposition, the Kaapvaal Craton was stiff, preventing a deep basin from developing further northwards on-craton. Additionally, the magnetic and borehole data highlight pervasive Jurassic dolerite sills and dykes. These sills and dykes can be highly fractured at surface, but at depth are possibly impermeable, providing seals and traps. They are also an important source of heat and need to be accounted for when evaluating the gas potential. The borehole data indicate sills can occur at any depth throughout the basin. The near surface sills are easily mapped with the coarse national magnetic data and single flight line modeling suggests that the edges of deeper sills can be delineated with higher resolution magnetic data. This approach indicates the importance of integrated studies to evaluating the shale gas potential in the Karoo.
机译:最近在南非卡罗盆地的兴趣已经引发了广泛的页岩天然气储备的可能性。在这里,我们展示了历史反思和折射地震(工业和学术),钻孔,MT和区域重力和磁数据的综合研究,其目标是评估页岩气体潜力。由5个深钻孔和MT数据约束的反射地震数据用于映射卡罗(DWYKA组)和底层地下室之间的接触。这提供了karoo超组的厚度(〜5.5 km)的重要约束。通过将重力数据与来自钻孔的反射地震和密度数据中已知的结构约束,这种接触可以扩展到地震数据稀疏的区域,并且表明该区域在24°经度接近的区域比在任一侧更薄。盆地的弯曲还表明,在沉积时,Kaapvaal Craton僵硬,防止了深深的盆地在北方北方发展进一步发展。此外,磁性和钻孔数据突出了普拉斯侏罗纪Dolerite Sills和Dykes。这些窗台和堤坝可以在表面的高度骨折,但深度可能是不可渗透的,提供密封和陷阱。它们也是热量的重要来源,在评估气体潜力时需要考虑。钻孔数据表示盆地的任何深度都可以发生。近表面门槛容易映射,粗大的国家磁性数据,单程线材建模表明​​更深的磁台层的边缘可以用更高的分辨率磁数据描绘。这种方法表明综合研究对喀古语评估页岩气势的重要性。

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