东海盆地丽水凹陷CO<sub>2</sub>分布特征及成藏主控因素

牛杏; 何云龙; 庄新国

doi:10.3799/dqkx.2021.021

Volume 46 Issue 10

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(10): 3549-3559

Niu Xing, He Yunlong, Zhuang Xinguo, 2021. Distribution and Major Controlling Factors of CO2 Reservoirs in Lishui Sag, East China Sea Basin. Earth Science, 46(10): 3549-3559. doi: 10.3799/dqkx.2021.021

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Niu Xing, He Yunlong, Zhuang Xinguo, 2021. Distribution and Major Controlling Factors of CO₂ Reservoirs in Lishui Sag, East China Sea Basin. Earth Science, 46(10): 3549-3559. doi: 10.3799/dqkx.2021.021

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Distribution and Major Controlling Factors of CO₂ Reservoirs in Lishui Sag, East China Sea Basin

doi: 10.3799/dqkx.2021.021

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, China
3.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2020-12-15
Available Online: 2021-11-03
Publish Date: 2021-11-03

Abstract

Abstract

Based on the drilling data and seismic data of Lishui sag, the distribution and major controlling factors of CO₂ reservoirs are studied by combining geochemical parameters of natural gas and development characteristics of basement faults and magma diapirs. The results show that CO₂ is mainly concentrated in Lingfeng Formation, lower segment of Mingyuefeng Formation and Proterozoic basal gneiss in the vertical. Besides, the content of CO₂ varies greatly in different layers. Laterally, Wenzhou 13-1, Lishui 35-7 and Nanping 5-2 structural CO₂ gas reservoirs are located on or near the magma diapirs, and there are faults around these CO₂ gas reservoirs. Whereas, there is no diapir near Lishui 36-1 structural CO₂ gas reservoirs and LF-1 containing CO₂ gas reservoir, but they are adjacent to large depression-controlling faults which are located at west side of Lingfeng uplift. The distribution of CO₂ gas reservoirs in the Lishui sag is mainly controlled by two stages magmatic activities, which are respectively in Early Miocene and Late Miocene. Mantle-derived CO₂ gas is carried by the deep volcanic magma activities to shallow crust, then migrates along with sand body to favorable traps and forms CO₂ gas pools.
- origin of carbon dioxide,
- spatiotemporal distribution,
- magmatic activity,
- controlling factor,
- Lishui sag,
- hydrocarbon

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Distribution and Major Controlling Factors of CO2 Reservoirs in Lishui Sag, East China Sea Basin

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