辽东湾断陷油气成藏模式及主控因素

杨宝林; 叶加仁; 王子嵩; 薛海琴

doi:10.3799/dqkx.2014.133

Volume 39 Issue 10

Oct. 2014

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Article Navigation > Earth Science > 2014 > 39(10): 1407-1420

Yang Baolin, Ye Jiaren, Wang Zisong, Xue Haiqin, 2014. Hydrocarbon Accumulation Models and Main Controlling Factors in Liaodong Bay Depression. Earth Science, 39(10): 1407-1420. doi: 10.3799/dqkx.2014.133

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Yang Baolin, Ye Jiaren, Wang Zisong, Xue Haiqin, 2014. Hydrocarbon Accumulation Models and Main Controlling Factors in Liaodong Bay Depression. Earth Science, 39(10): 1407-1420. doi: 10.3799/dqkx.2014.133

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Hydrocarbon Accumulation Models and Main Controlling Factors in Liaodong Bay Depression

doi: 10.3799/dqkx.2014.133

Yang Baolin^{1, 2
,},
Ye Jiaren^{1, 2},
Wang Zisong³,
Xue Haiqin⁴

1.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Jidong Oilfield Company, PetroChina, Tangshan 063004, China
4.
Jiangcheng College of China University of Geosicences, Wuhan 430200, China

Received Date: 2014-01-11
Publish Date: 2014-10-01

Abstract

Abstract

To further explore the hydrocarbon accumulation mechanism in Liaodong bay depression, its typical accumulation models are summarized and grouped, and the main controlling factors of each model are studied in this paper based on the analyses of hydrocarbon accumulation conditions and characteristics using seismic, drilling, geochemical and oil testing data. The research results show that Liaodong bay depression has superior hydrocarbon accumulation conditions including three sets of source rocks (Es₃, Es₁ and Ed₃), three reservoir-cap assemblages (upper, middle and lower), multi-type of conducting medium, and the oil and gas reservoirs which have been found are mainly tectonic reservoirs. The distribution rule of reservoirs is rich in Pre-E, Ed₂ and vertical Es₁₊₂ formation and abundant in the transverse fault zones. The hydrocarbon accumulation models of Liaodong bay depression can be grouped into 5 major types and 15 sub-types, including one-direction single-source single-migration path Pre-E reservoir, one-direction single-migration path Palaeocene reservoir, complex-migration path Palaeocene reservoir, one-direction deep-source complex-migration path Neogene reservoir and self-source-reservoir-capping reservoir. The Pre-E reservoir is mainly distributed in the northern and central sections of Liaoxi low uplift and the main controlling factors are hydrodynamic and physical property of Pre-E formation. Single-migration path Palaeocene reservoirs are mainly distributed in the sag zones and steep slope zones of Liaoxi and Liaozhong sag, and the main controlling factors are fault and maturity of the source rock. Complex-migration path Palaeocene reservoirs are mainly distributed in the northern and central sections of Liaoxi low uplift and the gentle slope zone of Liaozhong southern sag, and the main controlling factors are hydrodynamic and migration path. Neogene reservoirs are mainly distributed in the fault zones of southern part of Liaodong bay depression, and the hydrocarbon accumulation of this type is mainly controlled by cap rock and the faulting of Neogene. Self-source-reservoir-capping reservoirs are mainly formed in the inner part of the source rock, and mainly influenced by the physical property of the reservoir.
- hydrocarbon,
- accumulation characteristic,
- accumulation model,
- main controlling factor,
- Liaodong bay depression,
- petroleum geology

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Hydrocarbon Accumulation Models and Main Controlling Factors in Liaodong Bay Depression

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