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Sequential Mineralogy Characterization of Organic-Rich Shale: Example from the Hanadir Shale, Northwest Saudi Arabia

机译:有机富含页岩的顺序矿物学特征:来自沙特阿拉伯西北部的Hanadir Shale的示例

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The Middle Ordovician (Middle to Late Cardocian) Hanadir Shale member of the Qasim Formation is a potential shale gas exploration target. This paper quantitatively characterizes the mineralogy of the Hanadir Shale using an applied methodology to better understand the interrelationship between mineralogy and reservoir properties of shale gas formations. A 9-m thick sequence of the Hanadir Shale within the Tabuk quadrangle in northwest Saudi Arabia was investigated using sedimentological, geochemical, and mineralogical analyses. Sequential analyses were performed on shale samples: X-ray diffraction (XRD), X-ray fluorescence (XRF), cations exchange capacity (CEC), and linear swelling meter (LSM). This shale sequence is dominantly comprised of laminated clay-rich shale interbedded with thin siltstone to very fine sandstone beds. It is overlying a 5-m thick bearing with massive-to-low-angle crossbedding in the uppermost intervals of the Sajir member of the Saq Formation and underlying 30-m thick tigillites in the Kahfah member. The XRD results showed the Hanadir Shale is characterized by similar mineralogical composition of different proportions with all the samples containing high silica content (-50%), K-feldspar (-30%), and Na-feldspar (3%). Compared to the bulk mineralogy of the shale gas, clay content in the samples (10 to 20%) is relatively low. The identified clay types include kaolinite, illite, and smectite. Carbonate minerals (calcite and dolomite) also occur as traces (-1%) in all the samples. Swelling tests were performed to understand the swelling properties of the clay content and better understand reservoir properties, performance, and fluid properties in the Qasim Shale's reservoir equivalents. The study contributes to the existing database of shale gas exploration information. Clay mineral distribution patterns and their effects on the reservoir quality of the unconventional shale gas are not well understood; therefore, this study contributes to the understanding of the reservoir behavior of not only the Hanadir Shale but also other regional potential shale formations.
机译:中间奥陶凡氏(中间至晚期Cardocian)Qasim形成的Hanadir页岩成员是潜在的页岩气勘探目标。本文使用应用方法来定量表征Hanadir Shale的矿物学,以更好地了解页岩气体形成的矿物学和储层性质之间的相互关系。使用沉积学,地球化学和矿物学分析研究了西北沙特阿拉伯西北地区塔杜群岛内塔巴德群岛内的9米厚的Hanadir页岩序列。对页岩样品进行顺序分析:X射线衍射(XRD),X射线荧光(XRF),阳离子交换能力(CEC)和线性溶胀表(LSM)。这种页岩序列主要由层压粘土的页岩组成,嵌入薄晶体晶晶床中。它覆盖了5米厚的轴承,在SAQ形成的Sajir成员的最高间隔和底层30米厚的千毛地区的最高间隔,在Kahfah成员的最高间隔中覆盖。 XRD结果表明,Hanadir Shale的特征在于不同比例的类似比例的矿物组合物,所有含有高二氧化硅含量(-50%),K-Feldspar(-30%)和Na-Feldspar(3%)的样品。与页岩气的散装矿物相比,样品中的粘土含量(10至20%)相对较低。所识别的粘土类型包括高岭石,伊利石和蒙脱土。碳酸盐矿物(方解石和白云石)也以所有样品中的痕迹(-1%)发生。进行肿胀试验以了解粘土含量的溶胀性能,更好地了解Qasim Shale的储层等同物中的储层性质,性能和流体性能。该研究有助于现有的页岩气勘探信息数据库。粘土矿物分布模式及其对非传统页岩气体的储层质量的影响并不充分理解;因此,这项研究有助于了解不仅是Hanadir Shale的水库行为,还有助于其他区域潜在的页岩形成。

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