石油勘探与开发 >

2020 , Vol. 47 >Issue 5: 898 - 912

DOI: https://doi.org/10.11698/PED.2020.05.05

油气勘探

准噶尔盆地吉木萨尔凹陷二叠系芦草沟组酸碱交替成岩作用特征及对页岩储集层的影响

  • 王剑 ,
  • 周路 ,
  • 刘金 ,
  • 张欣吉 ,
  • 张帆 ,
  • 张宝真
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  • 1.西南石油大学油气藏地质及开发工程国家重点实验室,成都 610500;
    2.中国石油新疆油田公司实验检测研究院,新疆克拉玛依 834000;
    3.西南石油大学地球科学与技术学院,成都 610500;
    4.中国石油新疆油田公司勘探开发研究院,新疆克拉玛依 834000;
    5.中国石油新疆油田公司风城作业区,新疆克拉玛依 834000
王剑(1984-),男,湖北当阳人,现为西南石油大学在读博士,中国石油新疆油田公司实验检测研究院工程师,主要从事油气地质、沉积储集层、地质实验等方面的研究。地址:新疆克拉玛依市准噶尔路29号,中国石油新疆油田公司实验检测研究院,邮政编码:834000。E-mail:wangjian_2605@126.com

收稿日期: 2019-10-13

  修回日期: 2020-04-10

  网络出版日期: 2020-09-22

基金资助

国家科技重大专项(2017ZX05008-004-008);中国石油股份有限公司科技重大专项(2017E-0401)

收起

Acid-base alternation diagenesis and its influence on shale reservoirs in the Permian Lucaogou Formation, Jimusar Sag, Junggar Basin, NW China

  • WANG Jian ,
  • ZHOU Lu ,
  • LIU Jin ,
  • ZHANG Xinji ,
  • ZHANG Fan ,
  • ZHANG Baozhen
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  • 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China;
    2. Research Institute of Experiment and Detection, PetroChina Xinjiang Oilfield Company, Karamay 834000, China;
    3. School of Geosciences and Technology, Southwest Petroleum University, Chengdu 610500, China;
    4. Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, China;
    5. Fengcheng Oilfield Operation Area, PetroChina Xinjiang Oilfield Company, Karamay 834000, China

Received date: 2019-10-13

  Revised date: 2020-04-10

  Online published: 2020-09-22

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摘要

基于普通薄片、铸体薄片镜下观察与鉴定,结合X衍射、扫描电镜与电子探针等测试分析,对准噶尔盆地吉木萨尔凹陷二叠系芦草沟组页岩储集层的成岩作用及成岩相进行综合研究。结果表明,吉木萨尔凹陷二叠系芦草沟组沉积期具有碱性与酸性成岩作用交替出现的特点。页岩储集层孔隙演化受机械压实作用及酸碱交替成岩作用的双重影响,经历了碱性压实减孔-增孔段、酸性溶蚀增孔段、碱性溶蚀增孔-减孔段共3个阶段,分别发育3个次生孔隙发育带。页岩储集层划分为含凝灰质剩余粒间孔-溶蚀孔相、含凝灰质-含有机质泥晶白云岩混合孔隙相、泥晶藻云岩晶间孔相3种成岩相,其中含凝灰质剩余粒间孔-溶蚀孔相与含凝灰质-含有机质泥晶白云岩混合孔隙相分布范围大、孔隙结构好、含油程度高,为优质储集层发育的成岩相。研究成果为芦草沟组页岩储集层的深入认识及勘探开发提供了基础。图12表3参51

关键词： 酸碱交替成岩作用; 孔隙演化; 页岩油; 页岩储集层; 二叠系芦草沟组; 吉木萨尔凹陷; 准噶尔盆地

本文引用格式

王剑 , 周路 , 刘金 , 张欣吉 , 张帆 , 张宝真 . 准噶尔盆地吉木萨尔凹陷二叠系芦草沟组酸碱交替成岩作用特征及对页岩储集层的影响[J]. 石油勘探与开发, 2020 , 47(5) : 898 -912 . DOI: 10.11698/PED.2020.05.05

Abstract

The diagenesis and diagenetic facies of shale reservoirs in Lucaogou Formation of Jimusar Sag were studied by means of microscopic observation and identification of ordinary thin sections and cast thin sections, X-ray diffraction, scanning electron microscope and electron probe tests. The results show that alkaline and acidic diagenetic processes occurred alternately during the deposition of Permian Lucaogou Formation in Jimusaer Sag. The evolution of porosity in the shale reservoirs was influenced by compaction and alternate alkaline and acidic diagenetic processes jointly, and has gone through three stages, namely, stage of porosity reduction and increase caused by alkaline compaction, stage of porosity increase caused by acid dissolution, and stage of porosity increase and reduction caused by alkaline dissolution. Correspondingly, three secondary pore zones developed in Lucaogou Formation. The shale reservoirs are divided into three diagenetic facies: tuff residual intergranular pore-dissolution pore facies, tuff organic micrite dolomite mixed pore facies, and micrite alga-dolomite intercrystalline pore facies. With wide distribution, good pore structure and high oil content, the first two facies are diagenetic facies of favorable reservoirs in Lucaogou Formation. The research results provide a basis for better understanding and exploration and development of the Lucaogou Formation shale reservoirs.

Key words： acid-base alternation diagenesis; porosity evolution; shale oil; shale reservoir; Permian Lucaogou Formation; Jimusaer Sag; Junggar Basin

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