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Fluid transport in the Sherwood Sandstone: influences of diagenesis and lithofacies

机译:舍伍德砂岩中的流体输运:成岩作用和岩相的影响

摘要

The Triassic age Sherwood Sandstone Group (SSG) is of great importance to the UK for several applied reasons: i) it is the lateral equivalent of the hydrocarbon producing Lower Triassic (Olenkian) Bunter Sandstone in the North Sea and the Middle Triassic (Anisian) Ormskirk Sandstone in the East Irish Sea; ii) it is a major aquifer in the UK; iii) it has storage potential for anthropogenic CO2. Increased understanding of the SSG is required to further improve efficiency of extraction, protect aquifers and reduce overall risk associated with such activities. Despite these economically important uses, the SSG has previously seen little work to ascertain any possible connections between primary sedimentological facies and diagenesis. As such, this study has analysed 30 thin sections of fluvial sandstones from 5 boreholes in and adjacent to the Needwood Basin. Using optical microscopy and scanning electron microscopy a diagenetic history was deduced and analysed with respect to sedimentological facies. The diagenetic history of the Needwood Basin SSG is comparable with the SSG from other UK sedimentary basins, with the exception of a lower quantity of well-developed authigenic quartz, feldspar and increased framework grain and cement dissolution. The results indicate that primary sedimentological facies does have a control on subsequent diagenesis. The highest porosities were found in cross bedded sandstones and massive sandstones; the lowest porosities were found in conglomerates and muddy facies; low angled cross bedded sandstones and horizontally bedded sandstones displayed a wide range of porosities. The presence of diagenetic cements had a significant effect on porosity due simply to the reduction in available pore space: calcrete or dolocrete reduced porosity on average by 17.5%, baryte by 23% and iron oxide by 8%. This data can be used to populate databases for use in fluid flow modelling to inform the hydrocarbon industry as well as hydrogeology, predictive models for contaminant transport and green technology including Carbon Capture and Storage and geothermal energy. udud
机译:三叠纪的Sherwood砂岩组(SSG)在英国具有重要的应用意义,原因如下:i)它是北海和三叠纪中部(Anisian)产烃的低三叠纪(Olenkian)Bunter砂岩的侧向等效物。东爱尔兰海的Ormskirk砂岩; ii)它是英国的主要含水层; iii)具有人为二氧化碳的储存潜力。需要进一步了解SSG,才能进一步提高提取效率,保护含水层并降低与此类活动相关的总体风险。尽管有这些重要的经济用途,但SSG以前很少能确定初级沉积相和成岩作用之间的联系。因此,本研究分析了Needwood盆地及其附近5个钻孔中的30个河流砂岩薄层。利用光学显微镜和扫描电子显微镜,推论了成岩史并就沉积相进行了分析。 Needwood盆地SSG的成岩史与其他英国沉积盆地的SSG相当,唯一不同的是,发育良好的自生石英,长石的数量减少,骨架颗粒和水泥溶解增加。结果表明,原始沉积相确实控制了随后的成岩作用。在交叉层状砂岩和块状砂岩中发现孔隙率最高。在砾岩和泥质相中孔隙率最低。低角度的交叉层状砂岩和水平层状砂岩显示出广泛的孔隙度。成岩胶结物的存在对孔隙度有显着影响,这仅是由于可用孔隙空间的减少:钙质或多洛格雷特平均将孔隙度降低了17.5%,重晶石降低了23%,氧化铁降低了8%。该数据可用于填充用于流体建模的数据库,以告知碳氢化合物行业以及水文地质学,污染物迁移的预测模型以及包括碳捕集与封存和地热能在内的绿色技术。 ud ud

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