东营凹陷中央背斜带沙三段砂岩石英次生加大边发育特征及其指示意义

赵文; 何生; 郭小文; 王永诗; 郝雪峰; 熊伟

doi:10.3799/dqkx.2019.229

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3487-3501

Zhao Wen, He Sheng, Guo Xiaowen, Wang Yongshi, Hao Xuefeng, Xiong Wei, 2020. Characteristics of Quartz Overgrowth in Sandstones from Es3 Interval Central Anticlinal Belt in Dongying Depression and Its Significance. Earth Science, 45(9): 3487-3501. doi: 10.3799/dqkx.2019.229

Citation:

Zhao Wen, He Sheng, Guo Xiaowen, Wang Yongshi, Hao Xuefeng, Xiong Wei, 2020. Characteristics of Quartz Overgrowth in Sandstones from Es3 Interval Central Anticlinal Belt in Dongying Depression and Its Significance. Earth Science, 45(9): 3487-3501. doi: 10.3799/dqkx.2019.229

Citation:

Zhao Wen, He Sheng, Guo Xiaowen, Wang Yongshi, Hao Xuefeng, Xiong Wei, 2020. Characteristics of Quartz Overgrowth in Sandstones from Es3 Interval Central Anticlinal Belt in Dongying Depression and Its Significance. Earth Science, 45(9): 3487-3501. doi: 10.3799/dqkx.2019.229

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Characteristics of Quartz Overgrowth in Sandstones from Es3 Interval Central Anticlinal Belt in Dongying Depression and Its Significance

doi: 10.3799/dqkx.2019.229

1.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
SINOPEC Shengli Oilfield Company, Dongying 257015, China

Received Date: 2019-09-11
Publish Date: 2020-09-15

Abstract

Abstract

Quartz overgrowth is a common and important cementation in sandstone reservoirs. On the basis of micro-observation on different oil saturation sandstone thin sections from the Es3 interval of the Central Anticlinal Belt in Dongying depression, the width and the content of quartz overgrowth were quantified and the temperature of fluid inclusions were measured. Then the characteristics of quartz overgrowth, the stage of quartz overgrowth and the possible source of silica required for quartz overgrowth were analyzed. The width and the content of quartz overgrowth vary significantly with a range 4－90 μm and 2.50－39 927.80 μm², respectively. There are two main stages of secondary quartz overgrowth related to oil and gas filling in sandstone. Combined with burial-temperature histories, the two stages of quartz overgrowth are 15－6 Ma and 4－0 Ma, respectively. The dissolution of potash feldspar and the transformation of clay minerals in sandstone and mudstone layers of the Es3 interval are the main siliceous sources for the quartz overgrowth. The characteristics of quartz overgrowth in different oil saturation sandstone can be concluded into the similarity and difference: (1) The overall distribution of maximum width of quartz overgrowth and the area of each quartz overgrowth in different oil saturation sandstone are the same; (2) the width and the area of quartz overgrowth are generally different from each other. Porosity and permeability of sandstone, acidic water environment caused by hydrocarbon-bearing fluid filling and oil-water distribution characteristics are the main reasons for the similarity and difference of quartz overgrowth in sandstones with different oil saturation. And the quartz overgrowth can be regarded as trace marker of hydrocarbon-bearing fluid filling.
- Dongying depression,
- Central Anticlinal Belt,
- Es3,
- oil saturation,
- quartz overgrowth,
- petroleum geology

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References(51)

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