鄂尔多斯盆地杭锦旗地区盒一段致密砂岩储层特征及其主控因素

覃硕; 石万忠; 王任; 刘凯; 张威; 齐荣; 徐清海

doi:10.3799/dqkx.2022.007

Volume 47 Issue 5

May 2022

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Article Navigation > Earth Science > 2022 > 47(5): 1604-1618

Qin Shuo, Shi Wanzhong, Wang Ren, Liu Kai, Zhang Wei, Qi Rong, Xu Qinghai, 2022. Characteristics of Tight Sandstone Reservoirs and Their Controlling Factors of He-1 Member in Hangjinqi Block, Ordos Basin. Earth Science, 47(5): 1604-1618. doi: 10.3799/dqkx.2022.007

Citation:

Qin Shuo, Shi Wanzhong, Wang Ren, Liu Kai, Zhang Wei, Qi Rong, Xu Qinghai, 2022. Characteristics of Tight Sandstone Reservoirs and Their Controlling Factors of He-1 Member in Hangjinqi Block, Ordos Basin. Earth Science, 47(5): 1604-1618. doi: 10.3799/dqkx.2022.007

Citation:

Qin Shuo, Shi Wanzhong, Wang Ren, Liu Kai, Zhang Wei, Qi Rong, Xu Qinghai, 2022. Characteristics of Tight Sandstone Reservoirs and Their Controlling Factors of He-1 Member in Hangjinqi Block, Ordos Basin. Earth Science, 47(5): 1604-1618. doi: 10.3799/dqkx.2022.007

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Characteristics of Tight Sandstone Reservoirs and Their Controlling Factors of He-1 Member in Hangjinqi Block, Ordos Basin

doi: 10.3799/dqkx.2022.007

Qin Shuo^{1
,
,},
Shi Wanzhong^{1, 2
,
,
,},
Wang Ren^{1, 2},
Liu Kai^{1, 2},
Zhang Wei³,
Qi Rong³,
Xu Qinghai⁴

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Exploration and Development Research Institute, SINOPEC North China Company, Zhengzhou 450006, China
4.
School of Geosciences, Yangtze University, Wuhan 430100, China

Received Date: 2021-12-28
Publish Date: 2022-05-25

Abstract

Abstract

The He-1 Member of Hangjinqi block in Ordos basin is rich in natural gas, but the reservoir is dense and heterogeneous which restricts the increase of natural gas storage and production in this area. In this paper it makes full use of cores, casting thin section observation, field emission scanning electron microscopy (FE-SEM) observation, porosity and permeability test, X-ray diffraction (XRD) analysis, high-pressure mercury injection and constant-rate mercury injection analysis to illustrate the reservoir characteristics and controlling factors of He-1 Member in the study area. Based on that, the reservoirs are divided into superior reservoirs and poor reservoirs. The superior reservoirs are mainly composed of coarse-grained sublitharenite and litharenite developed in diara with less matrix and developed dissolution pores. The poor reservoirs are mainly composed of fine-grained litharenite developed with much matrix and undeveloped pores. The difference of provenance resulted in higher quartz content in the west than in the east. The strength of hydrodynamic condition is the initial condition that determines the quality of reservoir. Early argillaceous filling results in lower original porosity in poor reservoirs. The superior reservoir is more resistant to overburden pressure due to the less matrix. And the pore fluid is more active in superior reservoir which is benefitial to the formation of disolutionpore.
- tight sandstone reservoir,
- reservoir characteristic,
- main controlling factor,
- Hangjinqi block,
- Ordos basin,
- petroleum geology

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Characteristics of Tight Sandstone Reservoirs and Their Controlling Factors of He-1 Member in Hangjinqi Block, Ordos Basin

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