南海西沙西科1井层序地层格架与礁生长单元特征

朱伟林; 王振峰; 米立军; 杜学斌; 解习农; 陆永潮; 张道军; 孙志鹏; 刘新宇; 尤丽

doi:10.3799/dqkx.2015.055

Volume 40 Issue 4

Apr. 2015

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Article Navigation > Earth Science > 2015 > 40(4): 677-687

Zhu Weilin, Wang Zhenfeng, Mi Lijun, Du Xuebin, Xie Xinong, Lu Yongchao, Zhang Daojun, Sun Zhipeng, Liu Xinyu, You Li, 2015. Sequence Stratigraphic Framework and Reef Growth Unit of Well Xike-1 from Xisha Islands, South China Sea. Earth Science, 40(4): 677-687. doi: 10.3799/dqkx.2015.055

Citation:

Zhu Weilin, Wang Zhenfeng, Mi Lijun, Du Xuebin, Xie Xinong, Lu Yongchao, Zhang Daojun, Sun Zhipeng, Liu Xinyu, You Li, 2015. Sequence Stratigraphic Framework and Reef Growth Unit of Well Xike-1 from Xisha Islands, South China Sea. Earth Science, 40(4): 677-687. doi: 10.3799/dqkx.2015.055

Citation:

Zhu Weilin, Wang Zhenfeng, Mi Lijun, Du Xuebin, Xie Xinong, Lu Yongchao, Zhang Daojun, Sun Zhipeng, Liu Xinyu, You Li, 2015. Sequence Stratigraphic Framework and Reef Growth Unit of Well Xike-1 from Xisha Islands, South China Sea. Earth Science, 40(4): 677-687. doi: 10.3799/dqkx.2015.055

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Sequence Stratigraphic Framework and Reef Growth Unit of Well Xike-1 from Xisha Islands, South China Sea

doi: 10.3799/dqkx.2015.055

1.
China National Offshore Oil Corporation, Beijing 100010, China
2.
Zhanjiang Branch of CNOOC Ltd., Zhanjiang 524057, China
3.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-06-16
Publish Date: 2015-04-01

Abstract

Abstract

Carbonatite reef-bank system is one of the most important reservoirs in South China Sea. Well Xike-1, as a full-coring scientific drilling on the Paracel Islands, provides excellent conditions for the detailed study of the carbonatite reef-bank system. A deep study on carbonatite reef-bank system is made in the paper, using the macro-description and micro-analysis of cores obtained from well Xike-1, as well as high-resolution core scanning and many other tests results. The research indicates that 6 exposed surfaces, 2 flooding surfaces are recognized since Middle Miocene, and the well Xike-1 can be divided into 9 third-order sequences. The Late Miocene Huangliu Formation and Quaternary Ledong Formation are taken as the main reef-forming intervals, according to the characteristics of flooding surface and exposed surface, reef can be generalized into 2 types: submerged growth unit and exposed growth unit, the former can be subdivided into hard-based and soft-based, the latter can be subdivided into rapid-submerge and slow-submerge. Distinctive reef complexes are assembled vertically: drowned reef, aggradational reef, exposed reef. Results can be of huge value for the exploration of carbonatite reef-bank reservoirs, as well as the study of growing process of the reef in South China Sea.
- well Xike-1,
- organic reef,
- sequence division,
- growth unit,
- marine geology

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References(43)

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Sequence Stratigraphic Framework and Reef Growth Unit of Well Xike-1 from Xisha Islands, South China Sea

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