南沙海区礼乐盆地碳酸盐台地地震响应及发育演化

吴时国; 赵学燕; 董冬冬; 王大伟; 姚永坚

doi:10.3799/dqkx.2011.083

Volume 36 Issue 5

Sep. 2011

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WU Shi-guo, ZHAO Xue-yan, DONG Dong-dong, WANG Da-wei, YAO Yong-jian, 2011. Seismic Response and Development of Carbonate Platform in Liyue Basin, Nansha Sea Area. Earth Science, 36(5): 807-814. doi: 10.3799/dqkx.2011.083

Citation:

WU Shi-guo, ZHAO Xue-yan, DONG Dong-dong, WANG Da-wei, YAO Yong-jian, 2011. Seismic Response and Development of Carbonate Platform in Liyue Basin, Nansha Sea Area. Earth Science, 36(5): 807-814. doi: 10.3799/dqkx.2011.083

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Seismic Response and Development of Carbonate Platform in Liyue Basin, Nansha Sea Area

doi: 10.3799/dqkx.2011.083

1.
CAS Key Laboratory of Marine Geology and Environment, South China Sea Institute of Oceanology, Qingdao 266071, China
2.
Graduate University of Chinese Academy of Sciences, Beijing 100049, China
3.
Guangzhou Marine Geological Survey, Guangzhou 510601, China

Received Date: 2011-05-28
Publish Date: 2011-09-15

Abstract

Abstract

Liyue basin is located in the Nansha block of the South China Sea, which has been subject to compression, rifting, drifting and collision with Borneo block since Mesozoic.It is a complicated superimposed basin with great potential for exploration, with its well developed carbonate platforms being unique targets both for research and exploration.Based on new seismic profile NH973-2, in combination with published well and seismic data, the stratigraphic sequences across the section are analyzed in order to reveal the sedimentary sequences and seismic characters in the Liyue basin.The carbonate platforms are characterized by round external form, chaotic internal reflector.Based on tectonic subsidence calculation, we determine three stages of tectonic evolution in Liyue basin during Cenozoic and come to the conclusion that tectonic actions have had control over the development of Liyue carbonate platform.
- Liyue basin,
- carbonate platform,
- stratigraphic sequences,
- stratigraphy,
- earthquakes,
- marine geophysics

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References(24)

References

[1]	Briais, A., Patriat, P., Tapponnier, P., 1993. Updated interpretation of magnetic anomalies and seafloor spreading stages inthe South China Sea: implications for the Tertiary tectonicsof Southeast Asia. Journal of Geophysical Research, 98(B4): 6299-6328. doi: 10.1029/92JB02280.
[2]	Franke, D., Barckhausen, U., Baristeas, N., et al., 2011. Thecontinent-ocean transition at the southeastern margin of theSouth China Sea. Marine and Petroleum Geology, 28(6): 1187-1204. doi: 10.1016/j.marpetgeo.2011.01.004.
[3]	Gao, H. F., Zeng, X. H., Liu, Z. H., et al., 2005. Subsidencemodeling and tectonic evolution characteristics analysis ofLiyue basin in Nansha area. Tectonics and Metallogeny, 29(3): 385-390(in Chinese with English abstract).
[4]	Haq, B. U., Hardenbol, J., Vail, P. R., 1987. Chronology of fluctuating sea levels since the Triassic. Science, 235(4793): 1156-1167. doi: 10.1126/science.235.4793.1156.
[5]	Hinz, K., Schlüter, H. U., 1985. Geology of the dangerousgrounds, South China Sea, and the continental marginoff Southwest Palawan: results of SONNE Cruises SO-23and SO-27. Energy, 10(3-4): 297-315. doi: 10.1016/0360-5442(85)90048-9.
[6]	Holloway, N. H., 1982. North Palawan block Philippines—its relation to Asian mainland and role in evolution ofSouth China Sea. AAPG Bulletin, 66(9): 1355-1383.
[7]	Hutchison, C. S., 2004. Marginal basin evolution: the southern South China Sea. Marine and Petroleum Geology, 21(9): 1129-1148. doi: 10.1016/j.marpetgeo.2004.07.002.
[8]	Kudrass, H. R., Wiedicke, M., Cepeck, P., et al., 1986. Mesozoic and Cainozoic rocks dredged from the South China Sea (Reed bank area)and Sulu Sea and their significance for plate tectonic reconstructions. Marine and Petroleum Geology, 3(1): 19-30. doi: 10.1016/02648172(86)90053-X.
[9]	Müller, R. D., Lim, V. S. L., Isern, A. R., 2000. Late Tertiary tectonic subsidence on the Northeast Australian passive margin: response to dynamic topography. Marine Geology, 162(2-4): 337-352. doi: 10.1016/S00253227(99)00089-4.
[10]	Schlüter, H. U., Hinz, K., Block, M., 1996. Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu Sea. Marine Geology, 130(1-2): 39-78. doi: 10.1016/0025-3227(95)00137-9.
[11]	Sun, L. T., Sun, Z., Zhou, D., et al., 2008. Sedimentary stratigraphic and tectonic characteristics analysis of Liyuebasin in Nansha area. Tectonics and Metallogeny, 32(2): 151-158(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK200802004.htm
[12]	Sun, L. T., Sun, Z., Zhan, W. H., et al., 2010. Oil and gasresource potential of Liyue basin in Nansha area. Journal of Earth Science, 35(1): 137-145(in Chinese withEnglish abstract).
[13]	Taylor, B., Hayes, D. E., 1980. The tectonic evolution of theSouth China Sea. In: Hayes, D. E., ed., The tectonic andgeologic evolution of Southeast Asian seas and islands. Geophys. Monograph, AGU, Washington, D. C., 23: 89-104.
[14]	Wilson, M. E. J., 2002. Cenozoic carbonates in SoutheastAsia: implications for equatorial carbonate development. Sedimentary Geology, 147(3-4): 295-428. doi: 10.1016/S0037-0738(01)00228-7.
[15]	Wu, S. G., Han, Q. H., Dong, D., et al., 2009. Petroleumsystem in deepwater basins of the northern South China Sea. Journal of Earth Science, 20(1): 124-135. doi: 10.1007/s12583-009-0014-3
[16]	Xia, K. Y., 1996. Geologic geographic and oil/gas resource of inand out of Nansha islands. Science Press, Beijing, 252.
[17]	Yan, P., Liu, H. L., 2004. Tectonic-stratigraphic division andblind fold structures in Nansha waters, South China Sea. Journal of Asian Earth Sciences, 24(3): 337-348. doi: 10.1016/j.jseaes.2003.12.005
[18]	Yao, Y. J., Jiang, Y. K., Zeng, X. H., 2002. Cenozoic tectonic characteristics of Nansha area. China Offshore Oil and Gas, 6(2): 113-117(in Chinese with English abstract).
[19]	Yu, K., Zhao, J., 2009. Coral reefs. In: Wang, P. X., Li, Q. Y., eds., The South China Sea: paleoceanography andsedimentology. Springer, Heidelberg, 229-255.
[20]	高红芳, 曾祥辉, 刘振湖, 等, 2005. 南海礼乐盆地沉降史模拟及构造演化特征分析. 大地构造与成矿学, 29(3): 385-390. doi: 10.3969/j.issn.1001-1552.2005.03.014
[21]	孙龙涛, 孙珍, 周蒂, 等, 2008. 南沙海区礼乐盆地沉积地层与构造特征分析. 大地构造与成矿学, 32(2): 151-158. doi: 10.3969/j.issn.1001-1552.2008.02.003
[22]	孙龙涛, 孙珍, 詹文欢, 等, 2010. 南沙海域礼乐盆地油气资源潜力. 地球科学——中国地质大学学报, 35(1): 137-145. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201001017.htm
[23]	夏勘原, 1996. 南沙群岛及其邻近海区地质地球物理与油气资源. 北京: 科学出版社.
[24]	姚永坚, 姜玉坤, 曾祥辉, 2002. 南沙海域新生代构造特征. 中国海上油气(地质), 16(2): 113-117. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200202009.htm