西沙地区晚中新世以来碳酸盐岩的沉积演化及储层特征

张道军; 刘新宇; 王亚辉; 罗威; 尤丽; 徐守立

doi:10.3799/dqkx.2015.048

Volume 40 Issue 4

Apr. 2015

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Article Navigation > Earth Science > 2015 > 40(4): 606-614

Zhang Daojun, Liu Xinyu, Wang Yahui, Luo Wei, You Li, Xu Shouli, 2015. Sedimentary Evolution and Reservoir Characteristics of Carbonate Rocks since Late Miocene in Xisha Area of the South China Sea. Earth Science, 40(4): 606-614. doi: 10.3799/dqkx.2015.048

Citation:

Zhang Daojun, Liu Xinyu, Wang Yahui, Luo Wei, You Li, Xu Shouli, 2015. Sedimentary Evolution and Reservoir Characteristics of Carbonate Rocks since Late Miocene in Xisha Area of the South China Sea. Earth Science, 40(4): 606-614. doi: 10.3799/dqkx.2015.048

Citation:

Zhang Daojun, Liu Xinyu, Wang Yahui, Luo Wei, You Li, Xu Shouli, 2015. Sedimentary Evolution and Reservoir Characteristics of Carbonate Rocks since Late Miocene in Xisha Area of the South China Sea. Earth Science, 40(4): 606-614. doi: 10.3799/dqkx.2015.048

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Sedimentary Evolution and Reservoir Characteristics of Carbonate Rocks since Late Miocene in Xisha Area of the South China Sea

doi: 10.3799/dqkx.2015.048

Zhanjiang Branch of CNOOC Ltd., Zhanjiang 524057, China

Received Date: 2014-08-11
Publish Date: 2015-04-01

Abstract

Abstract

Reef-bank carbonate is one of the most important oil and gas reservoirs in deep-water area of the South China Sea. By macroscopic description of the well Xike-1 core (0-576.5 m) and microscopic analysis, combining with paleontology, paleomagnetism, high-resolution core scanning and large amounts of test result analysis, the carbonate reef system is studied in detail in this paper. The research indicates that this well has recorded 6 exposure events, and 2 drowning events since Late Miocene. Based on analyses of paleontology, paleomagnetism and lithium isotopes, 8 third-order sequences can be recognized, among which Late Miocene Huangliu Formation and Quaternary Ledong Formation are the main reef growth phase. By detailed petrography study, the rock types, diagenetic types and pore types of the Quaternary reef carbonate are systematically depicted, and the diagenetic environments are rebuilt.
- well Xike-1,
- reef,
- sequence division,
- diagenetic environment,
- petrology

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References(38)

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Sedimentary Evolution and Reservoir Characteristics of Carbonate Rocks since Late Miocene in Xisha Area of the South China Sea

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