Differential characteristics of lithological assemblages and gas-bearing of the Permian Longtan Formation mudstone in well L3, southeastern Sichuan Basin
Qian Cao, Hao Xu, Ke Jiang, Ruiyin Liu, Minghui Qi, Linqi Wang, Feiyu Li, Binyang Ma, Feilong Pu
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引用次数: 0
Abstract
As the main reservoir of coalbed gas in southeastern Sichuan, the mudstone of the Permian Longtan Formation has been drilled to obtain industrial gas, but the level of exploration and development is low. The researches on the types of lithological assemblages, reservoir characteristics, and gas-bearing properties are poor, which limits the evaluation and selection of the sweet point area for the marine-continental transitional shale gas. In this paper, by comparing the differential of different lithological distribution in the well L3, multiple discriminant functions and logging interpretation models for different lithology are established to determine the classification criteria of lithological assemblage types of shale formations. Based on the experimental results of high-temperature and high-pressure isothermal adsorption, the reservoir space distribution and gas-bearing characteristics of mudstone in different lithological assemblages are compared and analyzed. It is indicated that the four lithological assemblage types are found in the Permian Longtan Formation, including thick mudstone with the interlayer of coalbed (Type I), rich mudstone with the interlayer of sandstone and thin coalbed (Type II), sandstone interbedded with mudstone with the interlayer of coalbed (Type III), and limestone interbedded with sandstone with the interlayer of mudstone (Type IV), which are superimposed with each other. The different pore structure characteristics of mudstone in different lithological assemblages is the main influencing factor of differential gas-bearing property. The dominant lithological assemblages are Type I and Type II. Coalbed and carbonaceous mudstone are the source rock and primary storage space of adsorbed gas. Moreover, with low porosity and permeability, high breakthrough pressure and the strong sealing capacity of regional mudstone, it is easy to form the “microtrap” to store the natural gas. The sealing capacity of mudstone provides a favorable condition for gas preserve. Under the dynamic condition of hydrocarbon generation, the pressure storage box is formed, accompanied with the fine reservoir spaces and gas-bearing contents.
作为四川东南部煤层气的主要储层,二叠系龙潭组泥岩已钻探获得工业气,但勘探开发水平较低。岩性组合类型、储层特征、含气性质等方面的研究较少,限制了海陆过渡页岩气甜点区的评价与选择。本文通过对比 L3 井不同岩性分布的差异性,建立了不同岩性的多重判别函数和测井解释模型,确定了页岩层岩性组合类型的划分标准。根据高温高压等温吸附实验结果,对比分析了不同岩性组合中泥岩的储层空间分布和含气特征。结果表明,二叠系龙潭地层中存在厚泥岩夹煤层(Ⅰ型)、富泥岩夹砂岩和薄煤层(Ⅱ型)、砂岩夹泥岩夹煤层(Ⅲ型)、灰岩夹砂岩夹泥岩(Ⅳ型)四种岩性组合类型,并相互叠加。不同岩性组合中泥岩的孔隙结构特征不同,是影响含气性质差异的主要因素。主要岩性组合为 I 型和 II 型。煤化泥岩和碳质泥岩是吸附天然气的源岩和主要储存空间。此外,区域泥岩孔隙度和渗透率低、突破压力高、密封能力强,容易形成 "微陷阱 "储存天然气。泥岩的密封能力为天然气的保存提供了有利条件。在碳氢化合物生成的动态条件下,伴随着细小的储层空间和含气内容物,形成了压力存储箱。
期刊介绍:
This journal offers original research, new developments, and case studies in geomechanics and geophysics, focused on energy and resources in Earth’s subsurface. Covers theory, experimental results, numerical methods, modeling, engineering, technology and more.