松辽盆地青山口组页岩有机碳含量分布特征

武田田; 商斐; 陈睿倩; 钟志

doi:10.3799/dqkx.2022.337

Volume 47 Issue 11

Nov. 2022

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Article Navigation > Earth Science > 2022 > 47(11): 4309-4318

Wu Tiantian, Shang Fei, Chen Ruiqian, Zhong Zhi, 2022. Organic Carbon Distribution Characteristics of Qingshankou Shale in Songliao Basin, China. Earth Science, 47(11): 4309-4318. doi: 10.3799/dqkx.2022.337

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Wu Tiantian, Shang Fei, Chen Ruiqian, Zhong Zhi, 2022. Organic Carbon Distribution Characteristics of Qingshankou Shale in Songliao Basin, China. Earth Science, 47(11): 4309-4318. doi: 10.3799/dqkx.2022.337

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Organic Carbon Distribution Characteristics of Qingshankou Shale in Songliao Basin, China

doi: 10.3799/dqkx.2022.337

Wu Tiantian^{1, 2
,
,},
Shang Fei³,
Chen Ruiqian⁴,
Zhong Zhi^{1, 2
,
,
,}

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Theory and Technology of Petroleum Exploration and Development in Hubei Province, China University of Geosciences, Wuhan 430074, China
3.
Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
4.
College of Geosciences, China University of Petroleum, Beijing 102249, China

Received Date: 2022-05-28
Available Online: 2022-12-07
Publish Date: 2022-11-25

Abstract

Abstract

Total organic carbon (TOC) content is one of the key parameters to evaluate shale oil and gas resources. In order to quantitatively evaluate the TOC distribution characteristics and predict the sweet spots of shale of Qingshankou Formation in Songliao basin, the three-dimensional (3D) structural model of the Qingshankou shale reservoir was firstly constructed based on the logging data. Then, vitrinite reflectance (R_o) was calculated by restoring the ancient burial depth of reservoir rocks, and the TOC content of the Qingshankou Formation was predicted using the ∆logR method. Finally, the 3D model of TOC content in Qingshankou Formation was built using the geostatistical method. The results show that, vertically, the TOC content of Qing 1 Member is in the range of 0%-4%. However, the TOC content of Qing 2 Member and Qing 3 Member is significantly lower than that of Qing 1 Member. Horizontally, the TOC content of Qing 1 Member in the south of Sanzhao sag and the middle of Chaoyanggou terrace is the highest. The TOC content of Qing 2 Member is lower than 2%, and that in the north part of Gulong sag is the highest. The TOC content of Qing 3 Member is generally lower than 1.4%. This work provides important guidance and reference for selecting favorable shale oil exploration and development areas in Songliao basin.
- Songliao basin,
- Qingshankou Formation,
- shale oil,
- total organic carbon,
- 3D geological modeling,
- petroleum geology

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References(62)

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Organic Carbon Distribution Characteristics of Qingshankou Shale in Songliao Basin, China

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