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Shale Gas Potential of the Major Marine Shale Formations in the Upper Yangtze Platform, South China, Part III: Mineralogical, Lithofacial, Petrophysical, and Rock Mechanical Properties

机译:上长江平台的主要海洋页岩的页岩气体潜力,南方,第三部分:矿物学,岩石,岩石物理,岩石力学性能

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The marine black shale formations on the Upper Yangtze Platform, South China, are currently exploration targets for shale gas. Here, we report on the mineralogy, lithofacies, petrophysics, and rock mechanics of samples collected from the Ediacaran (Upper Sinian), Lower Cambrian, and Lower Silurian black shale intervals. All three formations are composed of high proportion of quartz, low content of clay, and rare or nonexistent content of carbonates. The Ediacaran and Lower Cambrian shales deposited in restricted deep water marine platform to marine basin environments are characterized by a higher quartz content and lower clay content than the Lower Silurian shales that were deposited in a more restricted marine basin environment. The carbonate content varies from 0 to over 50%, with the higher values measured in the Lower Silurian samples. These stratigraphic units were formed during bottom water anoxic conditions; therefore, they were rarely influenced by hioturbation Lithologically, laminated and nonlaminated siliceous mudstones predominate, with minor contributions of other lithotypes. Pores generally have diameters in the nanometer (nm) to micrometer (μm) range, and numerous pores occur in organic matter. Most of the measured samples have porosities less than 4%, although a few samples show porosity in excess of 10%. Pores with radii less than 50 run contribute significantly to total pore volume and total porosity. Permeability is extremely low, and helium permeability coefficients (Klinkenherg corrected permeability coefficient) are less than 20.2 nD (nano-Darcy, ~2 X 10~(-20) m~2). The rock mechanical properties of the samples are characterized by high brittle behavior, which coincides with their high compressive and tensile strengths and elastic properties. The Lower Cambrian shale is generally more brittle than the Lower Silurian shales, which possess a relatively higher content of clay minerals. The rock mechanical properties of the measured samples, however, depend on the overall mineral compositions and physical properties.
机译:南方中国上长江平台上的海洋黑页岩形成目前是页岩气的探索目标。在这里,我们报告从埃德拉甘(上北安),下寒武纪和较低的硅子黑色页岩间隔中收集的样品的矿物学,岩石,岩石物理学和岩石力学。所有三种形成由高比例的石英,粘土含量低,稀有或不存在的碳酸含量组成。埃德拉兰和下寒册子沉积在限制的深水海洋平台到海洋盆地环境中的特征在于较高的石英含量和较低的粘土含量,而不是沉积在更限制的海洋盆地环境中的下硅子。碳酸酯含量从0〜超过50%变化,在下硅子样品中测量的较高值。这些地层单位在底部水缺氧条件下形成;因此,它们很少受到Hioturnuctation思维,层压和脱脂的硅质泥岩占主导地位的影响,其它碎石的少量贡献。孔通常在纳米(nm)中的直径(nm)至千分尺(μm)范围,并且有机物质中发生了许多孔隙。大多数测量样品具有小于4%的孔隙率,尽管少数样品显示出超过10%的孔隙率。孔径小于50的孔隙显着促成总孔体积和总孔隙率。渗透性极低,氦渗透系数(Klinkehherg校正渗透系数)小于20.2nd(纳米达锡,〜2×10〜(-20)m〜2)。样品的岩石力学性质的特征在于高脆性行为,这与其高压压和拉伸强度和弹性性能一致。下部寒武纪女士通常比下硅子较低的粘土矿物含量更脆。然而,测量样品的岩石力学性能取决于整体矿物质组合物和物理性质。

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