冀北坳陷中元古界洪水庄组页岩油勘探前景探讨

李志明; 孙中良; 鲍云杰; 徐二社; 周勇水; 张云献

doi:10.11781/sysydz202301029

冀北坳陷中元古界洪水庄组页岩油勘探前景探讨

doi: 10.11781/sysydz202301029

李志明^{1, 2, 3,},
孙中良^{1, 2, 3},
鲍云杰^{1, 2, 3},
徐二社^{1, 2, 3},
周勇水⁴,
张云献⁴

1.
中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126
2.
页岩油气富集机理与有效开发国家重点实验室, 江苏无锡 214126
3.
中国石化油气成藏重点实验室, 江苏无锡 214126
4.
中国石化中原油田分公司勘探开发研究院, 河南濮阳 457001

基金项目:

国家自然科学基金项目 42090022

中国石化科技开发部项目 P18084

中国石化科技开发部项目 P20049-1

详细信息

作者简介:
李志明(1968-), 男, 博士, 研究员, 从事油气地球化学、页岩油气地质研究。E-mail: lizm.syky@sinopec.com

中图分类号: TE122
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- 被引次数: 0
出版历程
- 收稿日期: 2022-01-03
- 修回日期: 2022-11-10
- 刊出日期: 2023-01-28

Discussion on prospecting shale oil potential of Mesoproterozoic Hongshuizhuang Formation in the Jibei Depression

LI Zhiming^{1, 2, 3
,},
SUN Zhongliang^{1, 2, 3},
BAO Yunjie^{1, 2, 3},
XU Ershe^{1, 2, 3},
ZHOU Yongshui⁴,
ZHANG Yunxian⁴

1.
Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China
2.
State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Wuxi, Jiangsu 214126, China
3.
SINOPEC Key Laboratory of Petroleum Accumulation Mechanisms, Wuxi, Jiangsu 214126, China
4.
Exploration and Production Research Institute of Zhongyuan Oilfield Branch Company, SINOPEC, Puyang, Henan 457001, China

摘要

摘要: 为评价冀北坳陷中元古界洪水庄组页岩油勘探前景，对钻井岩心和露头剖面典型样品开展热解、基质孔隙度与渗透率、压汞+氮吸附、氩离子抛光+扫描电镜、X衍射全岩矿物等分析，综合前人分析与研究成果，剖析了洪水庄组页岩油形成条件，估算了页岩油资源潜力并探讨勘探前景。冀北坳陷洪水庄组中部潟湖相黑色泥页岩厚度主要介于35~55 m，有机质类型以Ⅱ₁、Ⅱ₂型为主，为一套富有机质的好—极好烃源岩，等效镜质体反射率处于0.80%~1.25%；基质孔隙度主要介于1.0%~8.0%，基质渗透率介于(2~100)×10^-6 μm²，孔隙以孔径大于50 nm的无机孔缝为主；恢复后热解游离烃S₁主要介于1.60~6.50 mg/g，残余气态烃介于0.13~0.24 m³/t，具有较好的含油气性；脆性矿物含量平均介于61.9%~72.3%，具备良好的可压裂改造性。冀北坳陷洪水庄组富有机质页岩型页岩油地质资源量约为12×10⁸ t，可采资源量为0.72×10⁸ t，具备针对洪水庄组富有机质泥页岩开展页岩油勘探的资源基础，具有较好的基质型页岩油勘探前景。
- 资源潜力 /
- 勘探前景 /
- 页岩油 /
- 洪水庄组 /
- 中元古界 /
- 冀北坳陷
Abstract: In order to evaluate the shale oil prospecting potential of the Mesoproterozoic Hongshuizhuang Formation in the Jibei Depression, the analyses of routine Rock-Eval pyrolysis, matrix porosity and permeability, mercury intrusion and nitrogen adsorption, argon ion polishing SEM and X-ray diffraction of bulk rock of typical core samples were carried out in this study. The shale oil forming conditions of the Hongshuizhuang Formation were studied, the shale oil resource was assessed, and the prospecting potential was discussed based on previous results. The results show that the lagoon facies black shale in the middle section of the Hongshuizhuang Formation is mainly 35-55 m thick with organic matter types of Ⅱ₁ and Ⅱ₂, and is a set of good- to excellent-quality source rock. The equivalent vitrinite reflectance of organic-rich black shale is 0.80%-1.25%. The matrix porosity is mainly 1.0%-8.0%, and the matrix permeability is (2-100)×10^-6 μm². The pores are dominated by inorganic pores and fissures with the diameter of pore larger than 50 nm. The values of S₁ after recovery is mainly 1.60-6.50 mg/g, and the content of residual hydrocarbon gas distributes 0.13-0.24 m³/t, indicating good hydrocarbon potential. The average content of brittle minerals is 61.9%-72.3%, with good frangibility. The shale oil geological resource is about 12×10⁸ t, and the shale oil recoverable resource is about 0.72×10⁸ t for organic matter rich shale of the Hongshuizhuang Formation. These suggested that the organic matter rich shale of the Hongshuizhuang Formation in the Jibei Depression has a resource basis for shale oil exploration with good prospecting potential.
- resource potential /
- prospecting potential /
- shale oil /
- Hongshuizhuang Formation /
- Mesoproterozoic /
- Jibei Depression

HTML全文

图 1 燕辽裂陷带地层构造单元与冀北坳陷构造位置简图

据文献[6]修编。

Figure 1. Tectonic units of Yanliao fault belt and tectonic location of Jibei Depression

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图 2 冀北坳陷构造沉积演化简图

Figure 2. Tectonic and sedimentary evolutions of Jibei Depression

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图 3 冀北坳陷冀浅1井洪水庄组岩性与地球化学综合柱状图

Figure 3. Lithological and geochemical columns of Mesoproterozoic Hongshuizhuang Formation, well Jiqian 1, Jibei Depression

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图 4 冀北坳陷中元古界洪水庄组富有机质页岩厚度与等效镜质体反射率等值线图

Figure 4. Contours of thickness and equivalent vitrinite reflectance of organic matter rich shale of Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

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图 5 冀北坳陷中元古界洪水庄组泥页岩总有机碳含量(TOC)和生烃潜量(S₁+S₂)的关系

Figure 5. TOC vs. PG (S₁+S₂) of mudstone and shale from Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

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图 6 冀北坳陷中元古界洪水庄组富有机质页岩有机质类型图解

Figure 6. Organic matter types of organic rich shale of Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

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图 7 冀北坳陷中元古界洪水庄组典型富有机质页岩基质孔渗图解

Figure 7. Matrix porosity and permeability of typical organic matter rich shale of Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

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图 8 冀北坳陷中元古界洪水庄组典型富有机质页岩孔隙结构

a.冀浅1井，127.23 m，黑色页岩；b.冀浅1井，131.10 m，黑色页岩；c.冀浅1井，137.28 m，黑色页岩；d.冀浅1井，155.00 m，黑色页岩；e.冀浅1井，172.80 m，黑色页岩；f.冀浅1井，189.58 m，黑色硅质岩

Figure 8. Pore structure of typical organic matter rich shale of Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

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图 9 冀北坳陷中元古界洪水庄组典型富有机质页岩游离烃S₁恢复前后与TOC的关系

Figure 9. TOC vs. S₁ before and after recovery of typical organic matter rich shale of Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

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表 1 冀北坳陷钻井与露头剖面洪水庄组与富有机质页岩厚度

Table 1. Thickness of Mesoproterozoic Hongshuizhuang Formation

钻井/剖面	地层总厚度/m	富有机质页岩厚度/m	备注
冀浅1井	142	43
冀元1井	71	35	参考文献[18]
元基2井	109	42	参考文献[16]
宽1井	109	42	参考文献[18]
化1井	145	46	参考文献[17]
双洞	140	48
龙潭沟	112	43
宋杖子	110	42
清河	130	43	参考文献[12]
孙家庄—北仗子	102	41
柳树底	105	40	参考平泉幅1∶20万地质图说明书
二道杖子	99	43	参考平泉幅1∶20万地质图说明书
北水泉	125	46	参考兴隆幅1∶20万地质图说明书

下载: 导出CSV

表 2 冀北坳陷中元古界洪水庄组富有机质页岩矿物组成

Table 2. Mineral compositions of organic matter rich shale of Mesoproterozoic Hongshuizhuang Formation in Jibei Depression

样品来源	样品数	矿物成分含量/%
样品来源	样品数	黏土矿物	石英	钾长石	斜长石	方解石	白云石	菱铁矿	黄铁矿	石膏	硬石膏	钙芒硝
冀浅1井岩心	27	13.2~35.0	31.7~77.0	0~4.0	0~1.7	0.1~2.5	1.5~36.5	0.6~4.3	1.0~13.9	0~0.3	0~3.2	0
冀浅1井岩心	27	27.2	54.4	2.1	0.5	1.1	7.0	2.3	4.9	0.1	0.4	0
野外露头	25	23.5~52.5	38.9~73.1	0.9~3.8	0~1.2	0.1~4.8	0.2~3.5	0.2~1.8	0.1~1.5	0~0.2	0~0.8	0~5.7
野外露头	25	36.2	55.2	2.1	0.4	0.8	1.9	1.1	0.4	0.0	0.2	1.7
注：表中分式的意义为$\frac{\text { 最小值~最大值 }}{\text { 平均值 }}$。

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