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Synthesis of the exploration of formations with a potential of CO_2 storage: Intermediate Depression and Madrid Basin

机译:CO_2贮藏潜力勘探的探索:中间抑郁症和马德里盆地

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As a part and continuation of the work that is being done under the GeoCapacity Project,Spanish Geological Survey (IGME) has developed a selection of CO_2 storages in the great sedimentary basins of Spain. This presentation is a result of these studies in the Tagus River Basin,including the two zones in which this basin is traditionally divided in geological publications: Intermediate Depression and Madrid Basin. Using information from hydrocarbon exploration campaigns,mostly seismic and borehole logging,as a starting point,storage-seal pairs have been identified,attending to different criteria,such as depth,height,porosity or salinity of the formation water. Through the analysis of these parameters two geological formations have been selected as the most promising: Buntsandstein sandstone Formation,with a primary seal in R?t clays and a secondary seal in Keuper clays,and Utrillas sandstone Formation (Lower Cretaceous) with a seal in the Superior Evaporitical Formation (Upper Cretaceous). On the other hand,as a special case study of the GeoCapacity Project,a detailed study of a selected structure is being carried out in the Tagus River Basin,about 70 Km to the South East from Madrid. This structure is a long double-domed anticline detected under a thick Tertiary deposit that is not folded. Two different formations have been selected as potential storages: -Utrillas sandstone (L-M Cretaceous): It completely covers the extension of the structure,and it is sealed by Tertiary marls and gypsum. Average porosity varies from 7 to 18% and height is about 120 m at a depth of 1550 m. -Buntsandstein sandstone (L Triassic): It is only deposited in the Eastern dome of the structure,sealed by R?t clays of the Middle Triassic. Average porosity is 14% and height is about 50 m at a depth of 1700 m. Total capacity of the structure has been evaluated at a first stage in 812 Mt in the case both formations can be used as storage.
机译:作为在地理产科医学项目下进行的工作的份额和继续,西班牙地质调查(IGME)在西班牙的大沉积盆地开发了一系列CO_2家庭。本介绍是在塔比河流域的这些研究的结果,包括该盆地传统上分为地质出版物的两个区域:中间抑郁和马德里盆地。使用来自碳氢化合物勘探活动的信息,主要是抗震和钻孔测井,作为起点,已经识别出存储密封对,参加不同标准,例如深度,高度,孔隙度或地层水的盐度。通过对这些参数的分析,选择了两种地质形成是最有前途的:Buntsandstein砂岩形成,在R 1 T粘土中的初级密封和伴侣粘土中的二次密封,以及乌特拉斯砂岩形成(下白垩纪)卓越的蒸发炼制(上白垩纪)。另一方面,作为对地理癖项目的特殊案例研究,在塔比河流域塔斯河盆地进行了一项详细研究,距离马德里约70公里。这种结构是在没有折叠的厚度沉积物下检测的长双圆形反射线。已选择两种不同的地层作为潜在的储存:-UTRILLAS砂岩(L-M白垩纪):它完全覆盖了结构的延伸,它由第三级MARL和石膏密封。平均孔隙率从7〜18%变化,高度约为120米,深度为1550米。 -buntsandstein砂岩(l三叠峰):它仅在结构的东圆顶上沉积,由中间三叠系的中间粘土密封。平均孔隙率为14%,高度约为50米,深度为1700米。在两种形成可以用作储存的情况下,在812毫秒的第一阶段评估了结构的总容量。

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