新疆石油地质 ›› 2022, Vol. 43 ›› Issue (1): 11-17.doi: 10.7657/XJPG20220102

• 油气勘探 • 上一篇    下一篇

鄂尔多斯盆地东南部长7段页岩孔隙特征及其控制因素

曹尚1,2,3(), 李树同1, 党海龙3, 邢海雪4, 张丽霞3, 张天龙3, 白璞3   

  1. 1.中国科学院 西北生态环境资源研究院,兰州 730000
    2.中国科学院大学 地球科学学院,北京 100049
    3.陕西延长石油(集团)有限责任公司 研究院,西安 710065
    4.大庆油田有限责任公司 第七采油厂,黑龙江 大庆 163000
  • 收稿日期:2021-07-23 修回日期:2021-09-16 出版日期:2022-02-01 发布日期:2022-01-24
  • 作者简介:曹尚(1990-),女,河南南阳人,工程师,博士研究生,油气地质(Tel)18629901831(E-mail) caoshang1990@163.com
  • 基金资助:
    国家科技重大专项(2017ZX05039-001-005)

Pore Characteristics and Controlling Factors of Chang 7 Shale in Southeastern Ordos Basin

CAO Shang1,2,3(), LI Shutong1, DANG Hailong3, XING Haixue4, ZHANG Lixia3, ZHANG Tianlong3, BAI Pu3   

  1. 1. Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
    2. College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
    3. Research Institute, Shaanxi Yanchang Petroleum(Group) Co., Ltd., Xi’an, Shaanxi 710065, China
    4. No.7 Oil Production Plant, Daqing Oilfield Company Ltd., Daqing, PetroChina, Daqing, Heilongjiang 163000, China
  • Received:2021-07-23 Revised:2021-09-16 Online:2022-02-01 Published:2022-01-24

摘要:

为明确鄂尔多斯盆地长7段陆相页岩储集层孔隙特征,通过扫描电镜、铸体薄片、气体吸附法和压汞法等实验手段,对长7段页岩储集层中纯页岩和粉砂质纹层发育的页岩孔隙特征进行了对比分析,并探讨了可能影响孔隙发育的因素。纯页岩中主要发育黏土矿物粒间孔和有机孔,粉砂质纹层发育页岩中主要发育粒间孔和粒内溶孔;相比纯页岩,粉砂质纹层的中—大孔发育,孔隙度、孔径和孔体积均较大。纯页岩孔隙的发育主要受控于刚性颗粒和有机质含量,粉砂质纹层页岩孔隙的发育主要受控于保存条件,如石英和长石等刚性颗粒的富集利于孔隙保存,酸性流体对长石的溶蚀具有增孔作用,液态烃包裹矿物抑制胶结作用的发生。粉砂质纹层发育的页岩孔隙结构和物性优于纯页岩,在页岩油气勘探中应重点关注粉砂质纹层发育段。

关键词: 鄂尔多斯盆地, 延长组, 长7段, 页岩, 粉砂质纹层, 孔隙特征, 控制因素

Abstract:

In order to identify the pore characteristics of the continental shale in the seventh member of Yanchang formation (Chang 7 member) in southeastern Ordos basin, the shale cores taken from pure shale and silty laminae of Chang 7 member were analyzed for pore characteristics with the aid of experimental methods such as SEM, cast slice, gas adsorption method, and mercury intrusion, and the factors that may affect pore development were discussed. The results show that pure shale mainly contains clay mineral intergranular pores and organic pores, and silty laminae holds intergranular pores and intragranular dissolved pores. Compared with pure shale, silty laminae has mesopores-macropores with larger porosity, pore diameter and pore volume. In pure shale, the development of pores is mainly controlled by the contents of rigid particle and organic matter. In silty laminate, the controlling factors for shale pore development are mainly the preservation conditions. For instance, the enrichment of rigid particles such as quartz and feldspar is conducive to pore preservation, acidic fluid can corrode feldspar to create more pores, and liquid hydrocarbons can wrap minerals to inhibit cementation. The shale in silty laminae is superior to pure shale with respect to pore structure and physical properties. Thus, the silty laminae zones should be paid more attention in shale oil/gas exploration.

Key words: Ordos basin, Yanchang formation, Chang 7 member, shale, silty laminae, pore characteristic, controlling factor

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