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Study on the characteristics and influencing factors of Chang 7 ultralow-porosity and low-permeability reservoirs in the Heshui area, Ordos Basin

长石 地质学 成岩作用 压实 溶解 绿泥石 胶结(地质) 地球化学 多孔性 石英 磁导率 钠长石 岩石物理学 斜长石 矿物学 碱性长石 油页岩 岩性 沉积岩 地貌学 水泥 材料科学 冶金 岩土工程 化学 古生物学 生物化学 物理化学
作者
Xinju Liu,Yuetian Liu,Zhendong Lu,Tao Zhang,Linjun Yu,Tao Yi,Hanwen Xu,Yutian Lei,Qibiao Zang,Rizwan Sarwar Awan,Wenda Li,Chenglin Liu,Yunfei Wu
出处
期刊:Interpretation [Society of Exploration Geophysicists]
卷期号:10 (4): T581-T593 被引量:1
标识
DOI:10.1190/int-2021-0138.1
摘要

Recently, the exploration and development of the Chang 7 shale oil reserves and production have increased in the Ordos Basin. However, the characteristics of the Chang 7 reservoir vary greatly in different areas, which affect the exploration and development of shale oil. We used various analytical methods such as core observation, casting section, high-pressure mercury injection, nuclear magnetic resonance, X-ray diffraction (XRD), and logging interpretation to study characteristics of the reservoir in the Heshui area. The lithology of the Chang 7 member is mainly feldspathic quartz sandstone suggesting that the content of quartz is higher than that of feldspar, and it has relatively low carbonates. In addition, the kinds of feldspar are mainly plagioclase and potassium feldspar, and the concentration of clay minerals is 80%, mainly comprising illite and chlorite. The reservoir of the Chang 7 member is chiefly comprised of submicron pores, such as feldspar dissolved pores, intergranular pores, dissolved pores, microfractures, and intergranular pores. The porosity ranges from 6% to 12%, whereas permeability is less than 0.2 × 10 −3 [Formula: see text]. The Chang 7 reservoir has a strong heterogeneity. Specifically, the heterogeneity of Chang 7 1 is weaker than that of Chang 7 2 . There is a complex diagenesis such as compaction, dissolution, and cementation, and the compaction and cementation are relatively more and the dissolution is dominated by constructive diagenesis of feldspar dissolution. Sedimentary microfacies are one of the main factors controlling reservoir development. The physical properties of the reservoir in the branch channel are better than the edges of the branch channel and the lacustrine. The diagenesis affects the development and distribution of good reservoirs, and destructive diagenesis such as compaction and cementation reduces porosity and permeability. Conversely, dissolution increases the physical properties of the reservoir. Tectonics has no obvious effects on reservoir but plays a positive role in the migration and accumulation of hydrocarbon when microfractures developed.
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