新疆石油地质 ›› 2022, Vol. 43 ›› Issue (2): 169-176.doi: 10.7657/XJPG20220206

• 油气勘探 • 上一篇    下一篇

吉木萨尔凹陷芦草沟组储集层脆性特征

石善志1(), 邹雨时2, 王俊超1, 张士诚2, 李建民1, 张啸寰2   

  1. 1.中国石油 新疆油田分公司 工程技术研究院,新疆 克拉玛依 834000
    2.中国石油大学(北京) 石油工程学院,北京 102249
  • 收稿日期:2021-08-04 修回日期:2021-12-22 出版日期:2022-04-01 发布日期:2022-03-24
  • 作者简介:石善志(1970-),男,辽宁大连人,高级工程师,石油地质,(Tel)0990-6889018(E-mail) Ssz-kcs@petrochina.com.cn
  • 基金资助:
    中国石油战略合作科技专项(ZLZX2020-01-07)

Brittle Characteristics of Lucaogou Formation Reservoir in Jimsar Sag, Junggar Basin

SHI Shanzhi1(), ZOU Yushi2, WANG Junchao1, ZHANG Shicheng2, LI Jianmin1, ZHANG Xiaohuan2   

  1. 1. Research Institute of Engineering Technology, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China
    2. School of Petroleum Engineering, China University of Petroleum, Beijing 102249, China
  • Received:2021-08-04 Revised:2021-12-22 Online:2022-04-01 Published:2022-03-24

摘要:

吉木萨尔凹陷芦草沟组储集层岩性复杂,岩石脆性对产能影响显著。在矿物学、力学参数及能量演化特征分析的基础上,应用层次分析法,提出适合芦草沟组储集层的脆性评价新方法,对比不同岩性的脆性特征。结果表明:吉木萨尔凹陷芦草沟组储集层黏土矿物含量较少,脆性矿物各成分含量接近,矿物成分脆性指数难以准确评价其脆性;储集层非均质性强,不同岩性脆性差异较大,泥质粉砂岩、砂屑白云岩和泥页岩的综合脆性指数较大,均大于0.60;白云质粉砂岩和泥晶白云岩的综合脆性指数中等,为0.50~0.60;白云质泥岩的综合脆性指数较小,为0.49;取自同一块岩心的岩样,平行层理方向脆性大于垂直层理方向;层理发育易导致岩石破裂形态复杂,影响脆性评价结果。

关键词: 吉木萨尔凹陷, 芦草沟组, 储集层, 脆性, 矿物成分, 力学参数, 能量演化, 层理

Abstract:

The lithology of the Lucaogou formation reservoirs in Jimsar sag is complex, and the rock brittleness has a significant impact on productivity. Based on the analysis of mineralogy, mechanical parameters and energy evolution characteristics, a new method for brittleness evaluation suitable for the Lucaogou formation reservoirs was proposed, which follows an analytic hierarchy process to compare the brittleness characteristics of different lithologies. The results show that the Lucaogou formation reservoir in the Jimsar sag has a low clay content and small differences in the contents of brittle minerals, so it is difficult to accurately evaluate the rock brittleness with the brittleness index; the reservoir is very heterogeneous, and the brittleness of different rocks varies greatly: the average comprehensive brittleness index of the argillaceous siltstone, sandy dolomite and mud shale is higher than 0.60, the average comprehensive brittleness index of the dolomitic siltstone and micrite dolomite is medium, ranging from 0.50 to 0.60, and the average comprehensive brittleness index of the dolomitic mudstone is relatively lower, only 0.49; for the rock samples taken from the same core, the brittleness in parallel bedding direction is larger than that in vertical bedding direction; and the development of beddings may easily lead to complex fracture patterns, which affects the brittleness evaluation results.

Key words: Jimsar sag, Lucaogou formation, reservoir, brittleness, mineral composition, mechanical parameter, energy evolution, bedding

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