扬子地区下寒武统与下志留统黑色页岩孔隙度与有机碳关系差异性及原因

徐壮; 石万忠; 翟刚毅; 包书景; 张晓明; 王任; 王健; 王超; 袁琪

doi:10.3799/dqkx.2017.099

Volume 42 Issue 7

Jul. 2017

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Xu Zhuang, Shi Wanzhong, Zhai Gangyi, Bao Shujing, Zhang Xiaoming, Wang Ren, Wang Jian, Wang Chao, Yuan Qi, 2017. Relationship Differences and Causes between Porosity and Organic Carbon in Black Shales of the Lower Cambrian and the Lower Silurian in Yangtze Area. Earth Science, 42(7): 1223-1234. doi: 10.3799/dqkx.2017.099

Citation:

Xu Zhuang, Shi Wanzhong, Zhai Gangyi, Bao Shujing, Zhang Xiaoming, Wang Ren, Wang Jian, Wang Chao, Yuan Qi, 2017. Relationship Differences and Causes between Porosity and Organic Carbon in Black Shales of the Lower Cambrian and the Lower Silurian in Yangtze Area. Earth Science, 42(7): 1223-1234. doi: 10.3799/dqkx.2017.099

Citation:

Xu Zhuang, Shi Wanzhong, Zhai Gangyi, Bao Shujing, Zhang Xiaoming, Wang Ren, Wang Jian, Wang Chao, Yuan Qi, 2017. Relationship Differences and Causes between Porosity and Organic Carbon in Black Shales of the Lower Cambrian and the Lower Silurian in Yangtze Area. Earth Science, 42(7): 1223-1234. doi: 10.3799/dqkx.2017.099

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Relationship Differences and Causes between Porosity and Organic Carbon in Black Shales of the Lower Cambrian and the Lower Silurian in Yangtze Area

doi: 10.3799/dqkx.2017.099

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Oil and Gas Survey Center, China Geological Survey, Beijing 100029, China

Received Date: 2016-12-29
Publish Date: 2017-07-15

Abstract

Abstract

The black shales in lower Cambrian Niutitang and lower Silurian Longmaxi develop well in Yangtze area, which are the key horizons for shale gas exploration because of its wide distribution, large thickness, high organic matter abundance. The porosity of Niutitang Formation shows a distinct difference from Longmaxi Formation. There are also significant differences in the pore structure, organic carbon content and density of the two sets of shales. Based on the logging data, buried depth (overlying pressure), porosity, organic carbon and maturity test data, comparative analysis is conducted. Results show that pore structure has been affected by the high degree of thermal evolution and organic carbon of Niutitang Formation. Organic matter is carbonized, organic porosity is collapsed and filled. The depth of Niutitang Formation is deep and the overburden pressure is also large, causing the inorganic porosity to be compacted. These factors make the porosity of Niutitang Formation obviously less than Longmaxi Formation.
- shale,
- porosity,
- organic carbon,
- maturity,
- Longmaxi Formation,
- Niutitang Formation,
- petroleum geology

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References(95)

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Relationship Differences and Causes between Porosity and Organic Carbon in Black Shales of the Lower Cambrian and the Lower Silurian in Yangtze Area

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