塘沽地区湖相白云岩储层裂缝特征及其控制因素

赵耀; 姚光庆; 穆立华; 李乐; 王刚

doi:10.3799/dqkx.2016.019

Volume 41 Issue 2

Feb. 2016

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Article Navigation > Earth Science > 2016 > 41(2): 252-264

Zhao Yao, Yao Guangqing, Mu Lihua, Li Le, Wang Gang, 2016. Characteristics and Controlling Factors of Fractures in Lacustrine Dolostones Reservoirs in Tanggu District. Earth Science, 41(2): 252-264. doi: 10.3799/dqkx.2016.019

Citation:

Zhao Yao, Yao Guangqing, Mu Lihua, Li Le, Wang Gang, 2016. Characteristics and Controlling Factors of Fractures in Lacustrine Dolostones Reservoirs in Tanggu District. Earth Science, 41(2): 252-264. doi: 10.3799/dqkx.2016.019

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Characteristics and Controlling Factors of Fractures in Lacustrine Dolostones Reservoirs in Tanggu District

doi: 10.3799/dqkx.2016.019

Zhao Yao^{1,2
,},
Yao Guangqing^{1,3*
,
,},
Mu Lihua²,
Li Le^1,3,
Wang Gang^1,3

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Jidong Oilfield Company, PetroChina, Tangshan 063004, China
3.
Key Laboratory of Tectonics & Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-08-13
Publish Date: 2016-02-15

Abstract

Abstract

The ${{\text{E}}_{1}}s_{3}^{5}$ member in Tanggu district is a fault block, high-pressure and fractured lacustrine dolostones reservoirs. Based on the core observation, thin sections and log data with Ansys, the authors study on the causes and formation periods of fractures in lacustrine dolostones reservoirs, describe the fracture characteristics and analyze the control factors of fractures. The results show that the fractures are mainly of the tectonic origin, with a few bedding fractures and dissolution fractures, and the seepage ability decreases successively. There are four stages of fractures development including bedding fractures parallel to beddings, oblique fractures with 45 and 60 degrees, tensile fractures with 75 to 90 degrees, and high angel fractures with 70 to 85 degrees. The structure, lithology, diagenesis and overpressure are the key control factors of fractures in lacustrine dolomite reservoir, which are obviously influenced by cracks and stress field. The fractures mainly develop near the fault cross zone with 2 groups of NW and NE trending faults, and the above mentioned fracture development zone with high pressure called the sweet spots should be valued in oil-gas exploration.
- fracture,
- Lacustrine Dolostones,
- controlling factors,
- Tanggu district,
- petroleum geology

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References(58)

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Characteristics and Controlling Factors of Fractures in Lacustrine Dolostones Reservoirs in Tanggu District

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