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首页> 外文期刊>Journal of natural gas science and engineering >Lithofacies and pore characterization of the Lower Permian Shanxi and Taiyuan shales in the southern North China Basin
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Lithofacies and pore characterization of the Lower Permian Shanxi and Taiyuan shales in the southern North China Basin

机译:华北盆地南部下二叠统山西和太原页岩的岩相和孔隙特征

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Marine-continental transitional shales with varied lithofacies are widely distributed in the Lower Permian Shanxi and Taiyuan Formations in the southern North China Basin (sNCB) where they have been subject to frequently changing depositional conditions. Despite their importance, integrative classifications of the lithofacies of such shales are not normalized primarily due to the complex composition of the formations. This work classifies and defines the pore microstructure of the Shanxi and Taiyuan shales (well Mouye-1) from the Zhongmou exploration area. Classification is performed by optical (polarizing) microscopy, X-ray diffraction, and scanning electronic microscopy (SEM) imaging of Ar-ion milled samples, yielding measurements of the total organic carbon (TOC) content, porosity, and nitrogen adsorption. The TOC content is introduced into traditional ternary plots denoting "clay-carbonate quartz". Four primary lithofacies are identified from the combined metrics of optical microscopy and inorganic and organic contents. These four divisions comprise silt bearing mudstones, silty mudstones, muddy siltstones, and silty carbonaceous mudstones. The samples exhibit porosities between 1% and 4.5%, with silty carbonaceous mudstones having the highest TOC content and returning the highest porosity. Pores hosted in both the inorganic matrix and organic substrate are imaged by SEM. The predominant and largest pore types are in the inorganic matrix and include inter-particle mineral pores, inter-crystalline mineral pores and secondary denudation pores caused by smectite illitization. The pore size distributions (PSDs) and specific surface areas are recovered from nitrogen gas adsorption using BJH and BET models that reveal a wide range of pore sizes. The pore volumes are predominately associated with larger macro-/mesopores, whereas the specific surface area is primarily from a contribution of smaller micro-/mesopores. Finally the target zone for fracturing and recovery is optimized using these integrated methods for lithofacies description, pore characterization, and petrophysical and geo-mechanical analysis. This study provides a selective completion strategy to reduce fracturing-treatment expense and improve well productivity. (C) 2016 Elsevier B.V. All rights reserved.
机译:具有不同岩相的海陆过渡页岩广泛分布在华北盆地南部(sNCB)的下二叠统山西和太原组,那里的沉积条件经常变化。尽管它们很重要,但主要由于地层的复杂组成,未对此类页岩岩相的综合分类进行归一化。这项工作对中牟勘探区的山西和太原页岩(Mouye-1井)的孔隙微观结构进行了分类和定义。通过光学(偏光)显微镜,X射线衍射和扫描电子显微镜(SEM)对Ar离子研磨的样品进行分类,得出总有机碳(TOC)含量,孔隙率和氮吸附的测量值。 TOC含量被引入到表示“粘土碳酸盐石英”的传统三元图中。从光学显微镜以及无机和有机物含量的组合指标中鉴定出四个主要岩相。这四个分区包括含泥质泥岩,粉质泥岩,泥质粉砂岩和粉质碳质泥岩。样品的孔隙率在1%至4.5%之间,粉质碳质泥岩的TOC含量最高,返回的孔隙率最高。通过SEM对无机基质和有机基质中的孔进行成像。主要和最大的孔类型在无机基质中,包括由蒙脱石非法化引起的颗粒间矿物孔,晶体间矿物孔和二次剥蚀孔。孔径分布(PSDs)和比表面积是使用BJH和BET模型从氮气吸附过程中回收的,该模型揭示了宽范围的孔径。孔体积主要与较大的大/中孔相关,而比表面积主要来自较小的微/中孔的贡献。最终,使用这些岩相描述,孔隙特征以及岩石物理和地质力学分析的综合方法,优化了压裂和采收的目标区。这项研究提供了一种选择性的完井策略,以减少压裂处理费用并提高油井生产率。 (C)2016 Elsevier B.V.保留所有权利。

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