南海南部三大盆地油气地质条件差异性

谢晓军; 赵志刚; 张功成; 刘世翔; 王龙; 宋双; 傅宁; 张厚和; 王一博; 唐武; 郭佳; 孙瑞

doi:10.3799/dqkx.2017.508

Volume 43 Issue 3

Mar. 2018

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Article Navigation > Earth Science > 2018 > 43(3): 802-811

Xie Xiaojun, Zhao Zhigang, Zhang Gongcheng, Liu Shixiang, Wang Long, Song Shuang, Fu Ning, Zhang Houhe, Wang Yibo, Tang Wu, Guo Jia, Sun Rui, 2018. Hydrocarbon Geological Differences of Three Basins in Southern South China Sea. Earth Science, 43(3): 802-811. doi: 10.3799/dqkx.2017.508

Citation:

Xie Xiaojun, Zhao Zhigang, Zhang Gongcheng, Liu Shixiang, Wang Long, Song Shuang, Fu Ning, Zhang Houhe, Wang Yibo, Tang Wu, Guo Jia, Sun Rui, 2018. Hydrocarbon Geological Differences of Three Basins in Southern South China Sea. Earth Science, 43(3): 802-811. doi: 10.3799/dqkx.2017.508

Citation:

Xie Xiaojun, Zhao Zhigang, Zhang Gongcheng, Liu Shixiang, Wang Long, Song Shuang, Fu Ning, Zhang Houhe, Wang Yibo, Tang Wu, Guo Jia, Sun Rui, 2018. Hydrocarbon Geological Differences of Three Basins in Southern South China Sea. Earth Science, 43(3): 802-811. doi: 10.3799/dqkx.2017.508

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Hydrocarbon Geological Differences of Three Basins in Southern South China Sea

doi: 10.3799/dqkx.2017.508

CNOOC Research Institute, Beijing 10028, China

Received Date: 2017-10-08
Publish Date: 2018-03-15

Abstract

Abstract

Many studies have been carried out on the hydrocarbon geologic conditions of Wan'an, Zengmu and Brunei-Sabah basins. However, there are few studies on the difference of hydrocarbon geologic conditions among basins. Based on a lot of previous research results, drilling, seismic data and oil and gas testing data were comprehensively used to analyse the main difference of hydrocarbon geology in the Wan'an, Zengmu and Brunei-Sabah basins in southern South China Sea. The study shows that the Cenozoic of the three basins all developed two tectonic stages, mainly developing marine-land transitional facies and marine depositional environment. Three periods (Oligocene, Miocene and Pliocene) developed two types of source rocks, i.e. the coal measures and terrigenous marine facies, the period of major source rock is gradually new from west to east. Developed two types of reservoirs, i.e. clastic sandstone and carbonate rock, reservoirs distribution may be characterized by near shore sand and distant shore reef, the reservoirs period is gradually new from west to east. There are two combination of source rock and reservoris, i.e. the distant shore self-generation and self-reservoiring and the near shore lower-generation and upper-reservoiring.
- tectonic-sedimentary features,
- source rocks,
- reservoris,
- combination of source rock and reservoris,
- Southern South China Sea

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References(59)

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