南海南部北康盆地晚渐新世－中中新世物源变化

雷振宇; 张莉; 王龙樟; 骆帅兵; 钱星; 徐乔; 沈奥; 肖娇静

doi:10.3799/dqkx.2019.162

Volume 45 Issue 5

May 2020

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Article Navigation > Earth Science > 2020 > 45(5): 1855-1864

Lei Zhenyu, Zhang Li, Wang Longzhang, Luo Shuaibing, Qian Xing, Xu Qiao, Shen Ao, Xiao Jiaojing, 2020. Provenance Migration in the Beikang Basin of the Southern South China Sea during the Oligocene to the Mid-Miocene. Earth Science, 45(5): 1855-1864. doi: 10.3799/dqkx.2019.162

Citation:

Lei Zhenyu, Zhang Li, Wang Longzhang, Luo Shuaibing, Qian Xing, Xu Qiao, Shen Ao, Xiao Jiaojing, 2020. Provenance Migration in the Beikang Basin of the Southern South China Sea during the Oligocene to the Mid-Miocene. Earth Science, 45(5): 1855-1864. doi: 10.3799/dqkx.2019.162

Citation:

Lei Zhenyu, Zhang Li, Wang Longzhang, Luo Shuaibing, Qian Xing, Xu Qiao, Shen Ao, Xiao Jiaojing, 2020. Provenance Migration in the Beikang Basin of the Southern South China Sea during the Oligocene to the Mid-Miocene. Earth Science, 45(5): 1855-1864. doi: 10.3799/dqkx.2019.162

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Provenance Migration in the Beikang Basin of the Southern South China Sea during the Oligocene to the Mid-Miocene

doi: 10.3799/dqkx.2019.162

Lei Zhenyu^{1, 2
,},
Zhang Li^{1, 2},
Wang Longzhang^{3
,
,
,},
Luo Shuaibing^{1, 2},
Qian Xing^{1, 2},
Xu Qiao³,
Shen Ao³,
Xiao Jiaojing³

1.
Guangzhou Marine Geological Survey, MNR, Guangzhou 510760, China
2.
MNR Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Guangzhou 510760, China
3.
College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, China

Received Date: 2019-07-18
Publish Date: 2020-05-15

Abstract

Abstract

It is significant to research the provenance of Beikang basin in the southern South China Sea, because oil and gas resources were influenced by the changes of dispersion systems resulted from tectonic-induced migration of provenance. In this paper, seismic reflection data were used in seismic attribute analysis, where stratigraphic slices of RMS (root mean square amplitude) were used to analyze dispersion systems, in order to inquire into provenance migration and its controlling factors. During the Later Oligocene to Middle Miocene, the provenance of the Beikang basin was from the south and the dispersion systems extended from south to north. Two depositional cycles were separated by the Early Miocene Uncomformity (EMU), which formed during seawater deepening. In each cycle, sedimentary supply increased gradually upward. During the Middle Miocene, the depositional provenance migrated northwestward gradually. Regional analysis show that the provenance of the Beikang basin mainly came from Zengmu Foreland basin and the provenance migration is caused by landfill and overthrust northward of the Zengmu Foreland basin.
- provenance,
- Late Oligocene to Middle Miocene,
- Beikang basin,
- southern South China Sea,
- marine geology

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References(47)

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Provenance Migration in the Beikang Basin of the Southern South China Sea during the Oligocene to the Mid-Miocene

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