Smeaheia, A Potential Northern North Sea CO2 Storage Site: Structural Description And De-Risking Strategies

M. Mulrooney, J. Osmond, E. Skurtveit, L. Wu, A. Braathen
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引用次数: 4

Abstract

Smeaheia is a potential subsurface CO2 storage site located on the Horda platform in the Norwegian sector of the North Sea. The site is currently being investigated as part of the Norwegian CCS Research Centre, which envisages injection, and storage of CO2 into shallow-marine deposits comprising the Jurassic Viking Group. Two prospects, defined as fault-bound structural closures, have been identified, i) Alpha in the footwall of the Vette fault, and Beta in the Hanging wall of the Oygarden fault. In this contribution we present the fundamental structural framework of the Smeaheia site as derived from seismic interpretation of a high resolution 3D dataset. Qualitative and quantitative fault seal properties of the Vette fault are presented. Juxtaposition and shale gouge ratio analysis suggest the Vette fault has a high sealing probability for the Alpha closure. A relay zone to the south of the structure is more likely to be non-sealing and may facilitate pressure communication with a neighbouring fault block where hydrocarbon production has been ongoing. This communication may have resulted in Smeaheia being depleted. Risk of fault reactivation is assessed based on likely in-situ stress states, hydrostatic pressure regimes and the aforementioned depleted pressure regimes.
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Smeaheia,北海北部潜在的二氧化碳储存地点:结构描述和降低风险策略
Smeaheia是一个潜在的地下二氧化碳储存地点,位于北海挪威地区的Horda平台上。该地点目前正在作为挪威CCS研究中心的一部分进行调查,该研究中心设想将二氧化碳注入并储存到包括侏罗纪维京集团在内的浅海沉积物中。确定了两个远景区,即Vette断裂下盘的Alpha远景区和Oygarden断裂上盘的Beta远景区。在这篇文章中,我们展示了Smeaheia遗址的基本结构框架,这是由高分辨率3D数据集的地震解释得出的。介绍了维特断层的定性和定量断层封闭性。并置分析和页岩泥比值分析表明,Vette断裂具有较高的Alpha封闭概率。构造南部的中继带更有可能是非密封的,并且可能促进与相邻断块的压力通信,该断块正在进行油气生产。这种交流可能导致斯迈黑亚被耗尽。断层重新激活的风险是根据可能的地应力状态、静水压力状态和上述耗尽压力状态来评估的。
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