4.7 Article

Simulation experiment of fluid-feldspar sandstone interactions and their implications for tight oil and gas exploration of the Yanchang Formation, Ordos Basin, China

期刊

MARINE AND PETROLEUM GEOLOGY
卷 142, 期 -, 页码 -

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.marpetgeo.2022.105737

关键词

Tight reservoir; Fluid-rock interaction; Organic acids; Feldspar sandstone; Ordos basin

资金

  1. Key Science and Technology Projects of Sinopec [P19023]
  2. Natural Science Foundation of China [42072156, 41872151]
  3. National Science and Technology Major Project [2017ZX05036-002, 2017ZX05005-001]

向作者/读者索取更多资源

This study reveals the impact of total component fluids from source rock on reservoir transformation during hydrocarbon evolution through simulation experiments. Under closed conditions, the interaction between fluids and feldspar sandstone leads to the alteration of feldspar minerals and the generation of clay minerals, resulting in reservoir tightness. Additionally, a semi-quantitative evaluation method for feldspar dissolution and porosity was established. The geological characteristics of the Yanchang Formation of the Ordos Basin affect the retention effect of diagenetic fluids, and oil and gas exploration should focus on finding sedimentary sand facies bodies favorable for the preservation of primary pores.
Tight oil and gas reservoirs are generally formed in structurally stable and broad buffer zones, with high-quality source rocks developed in large areas and sand bodies in extensive contact with source rocks. Fluids generated from source rock during the thermal maturation are bound to dissolve or precipitate in the adjacent reservoir, which directly restricts the pore development of the reservoir and the direction of oil and gas exploration. To reveal the effect of the total component fluids from source rock on reservoir transformation during hydrocarbon evolution, taking the Yanchang Formation of the Ordos Basin as an example, a fluid-feldspar sandstone inter-action simulation experiment of different geological evolution stages under a closed environment was carried out. The results show that the fluids that formed in the hydrocarbon evolution process contain organic acids, and consist mainly of acetic acid. At the peak period of oil generation (VRo = 0.96%), the fluids are the most acidic, the acetic acid yield is the highest, and the average molar ratio is 56.11%. Under closed conditions, after the fluid-feldspar sandstone interaction, the feldspar minerals are altered and clay minerals are generated in situ, which results in a tight reservoir. The feldspar mineral content decreased from 26.1% to 20.8%-22.3%, clay mineral content increased from 11% to 14.30%-14.37%, porosity decreased 5.18%-28.79%, and permeability decreased 4%-34.16%. In addition, a semi-quantitative evaluation method of feldspar dissolution and porosity was established, which was used to evaluate the effect of fluids on feldspar sandstone reservoirs during hy-drocarbon evolution. The local semiclosed or open diagenetic system and acid fluid transport and accumulation area beneficial to the formation of the sweet spot of tight oil and gas. However, the gentle tectonic setting and extensive contact of sand and mudstone lead to the retention effect of diagenetic fluid in the Yanchang Formation of the Ordos Basin. Oil and gas exploration should be mainly directed to finding sedimentary sand facies bodies favorable for the formation and preservation of primary pores.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据