Natural Gas Geoscience ›› 2022, Vol. 33 ›› Issue (6): 1001-1012.doi: 10.11764/j.issn.1672-1926.2021.12.009

   

Element geochemical characteristics of shale in the First Member of Benxi Formation in eastern Ordos Basin: Take Zhaoxian section and Well M115 in Linxian County, Shanxi as examples

Chenguang CUI1(),Hui ZHANG2,Wenxiang LIU2,Shifang LI3,Yan LIU2,Huanxin SONG1(),Chenjun WU1,Zhigang WEN1   

  1. 1.Key Laboratory of Oil and Gas Resources and Exploration Technology of Ministry of Education,College of Resources and Environment,Yangtze University,Wuhan 430100,China
    2.China Research Institute of Exploration and Development,PetroChina Changqing Oilfield Company,Xi 'an 710018,China
    3.No. 10 Oil Production Plant,PetroChina Changqing Oilfield Company,Qingyang 745100,China
  • Received:2021-09-14 Revised:2021-12-11 Online:2022-06-10 Published:2021-03-22
  • Contact: Huanxin SONG E-mail:987750549@qq.com;shx@yangtzeu.edu.cn
  • Supported by:
    The Scientific Research Project of Changqing Oilfield Company, PetroChina(Technology 2020-151)

Abstract:

The Carboniferous Benxi Formation shale is an important target interval for shale gas exploration in the Upper Paleozoic in the central and eastern Ordos Basin. On the basis of its representative field profile, drilling core system observation and sampling analysis, using the analyticaldata of major and trace elements, combined with the test data of the whole rock mineral composition, organic carbon content, organic microscopic composition, and so on, the palaeoclimate, water environment and the relationship with the development of organic-rich mud shale during the sedimentary period of the First Member of Benxi Formation in the eastern Ordos Basin are studied. The results show that the shale in the First Member of Benxi Formation of the study area is mainly clayey shale and siliceous shale, and quartz and clay minerals are absolutely dominant in the mineral composition; the CIA, Sr/Cu, and C value parameters indicate that the sedimentary period of the first member is mainly hot characteristics of wet paleoclimate; Sr content, Sr/Ba, Ba/Ga and other parameters indicate that the salinity of the sedimentary water in the upper and lower sub-members of the member is saline water, saline water-brass water, respectively,indicating that the water body salt in the late depositional period of this member was at relatively high degree;V/(V+Ni),Ceanom,Th/U and other parameters indicate that the water body in this sedimentary period was dominated by anoxic-poor oxygen environment. The hot and humid paleo-climate, the saline anoxic-poor sedimentary water environment and other good organic matter preservation conditions are favorable factors for the development of organic-rich shale in this section, especially the upper subsection. The development of high-quality shale provides a good foundation for shale gas exploration in the study area.

Key words: Element geochemistry, Organic-rich shale, Benxi Formation, Sedimentary environment, Paleoclimate, Ordos Basin.

CLC Number: 

  • TE122.1+13

Fig.1

Location map of the study area and histogram of the First Member of Benxi Formation"

Fig.2

Stratigraphic and lithologic characteristics of the First Member of Benxi Formation in Linxian area"

Fig.3

Divisioning scheme of shale lithofacies in the First Member of Benxi Formation(the base map is modified according to LI,et al.[19])"

Fig.4

Whole rock mineral content distribution of the First Member of Benxi Formation"

Table 1

Test results of element content analysis in the First Member of Benxi Formation"

编号层位SiO2/%Al2O3/%微量元素/10-6Sr/BaBa/GaV/ (V+Ni)CeanomTh/UCIASr/CuCP/TiTOC/%
SrVNiBaCuMoGaTh
Z-S12招贤剖面C2b1?57.3924.23217.2695.9312.88169.3213.410.4731.0420.571.285.450.88-0.034.9491.3016.200.730.112.93
Z-S1159.4624.01222.6396.249.14190.318.330.4531.4820.381.176.050.91-0.054.8691.0626.730.310.092.29
Z-S1056.2721.29193.2591.8152.91148.5319.830.6226.8815.741.305.530.63-0.023.8291.749.752.540.162.25
Z-S948.1017.11298.5581.2226.90202.8712.720.9424.3417.161.478.340.75-0.044.5490.0023.471.120.161.62
Z-S858.0522.77270.0294.0422.58167.8322.610.5031.1020.401.615.400.81-0.064.9891.4211.940.790.132.98
Z-S759.0224.14222.9096.2352.34187.3623.380.4929.4118.601.196.370.65-0.043.3891.389.530.360.172.03
Z-S655.5621.66339.2668.7811.143648.0714.870.5733.6517.440.09108.420.86-0.073.2190.1722.820.350.1412
Z-S5招贤剖面C2b157.9820.47149.25134.3957.61289.2328.040.4327.7717.820.5210.420.70-0.054.5483.525.321.380.101.97
Z-S461.5522.31184.10167.1310.49336.6612.910.7232.7622.250.5510.280.94-0.023.4482.6314.260.240.081.74
Z-S358.5423.75201.47175.5026.01357.1423.020.2334.3921.800.5610.380.87-0.024.4083.808.750.410.081.66
Z-S264.6121.00180.2989.5114.48132.4920.090.3228.2814.481.364.680.87-0.044.5792.178.971.280.141.26
Z-S147.0535.7734.1499.3234.3945.504.281.3136.746.220.751.240.74-0.031.1599.017.802.600.021.09
M-S9M115井C2b1?50.4832.69270.8293.7511.29108.4714.170.3943.3620.752.502.500.89-0.024.9797.0619.121.080.071.01
M-S847.7517.98403.32168.8226.85250.1117.992.9026.8614.461.619.310.86-0.031.9886.9722.422.041.561.44
M-S760.2324.4588.54199.4522.68281.225.480.4233.8917.940.318.300.90-0.043.4488.683.470.220.081.42
M-S646.0328.06354.52207.4986.45188.5781.311.0236.8421.351.885.120.71-0.012.2693.744.361.610.155.33
M-S5M115井C2b1?58.4020.39203.99133.6522.37318.8926.610.3528.3717.540.6411.240.86-0.054.4985.607.671.150.122.57
M-S464.2220.0675.27202.8628.4351.1422.160.1933.0420.280.2110.630.88-0.033.5683.653.400.150.090.83
M-S353.5329.62339.09144.7455.25190.2433.650.4834.0834.661.785.580.720.003.4693.1910.080.580.120.81
M-S247.6334.55138.0994.6221.5691.155.671.4848.488.731.511.880.81-0.180.6997.4924.351.150.030.46
M-S149.9334.11221.73108.8839.27180.154.70.3241.7220.071.234.320.73-0.043.4994.8547.180.130.030.67

Fig. 5

Vertical variation of element geochemical indexes in the First Member of Benxi Formation in Zhaoxian section"

Fig. 6

Vertical variation of element geochemical indexes in the First Member of Benxi Formation of Well M115"

Fig.7

Ba-Sr intersection diagram of the First Member of Benxi Formation"

Fig.8

Intersection diagram of V/(V+Ni)-Th/U in the First Member of Benxi Formation"

Fig.9

Organic maceral and core characteristics of the First Member of Benxi Formation"

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