莺歌海盆地构造演化与强烈沉降机制的分析和模拟

孙珍; 钟志洪; 周蒂

Volume 32 Issue 3

May 2007

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2007 > 32(3): 347-356

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

Citation:

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

Citation:

SUN Zhen, ZHONG Zhi-hong, ZHOU Di, 2007. The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin. Earth Science, 32(3): 347-356.

PDF( 1220 KB)

The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin

1.
CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China
2.
Department of Science and Technology, Shenzhen Branch of CNOOC, Guangzhou 510240, China

Received Date: 2006-08-28
Publish Date: 2007-05-25

Abstract

Abstract

During Eocene period, rapid subsidence occurred in the Yinggehai basin where more than 17 km of sedimentary cover has been accumulated.According to the analogue modeling experiments, the rigid massif on the Indochina block could be one of the most important factors contributing to the strong subsidence and high sedimentation rate of the basin.Combined the geological analysis with analogue modeling experiments, the evolution of the Yinggehai basin could be divided into four main stages: (1) Before 42 Ma, controlled by the southeastward extension of the Beibu Gulf basin on the northern continental margin, the Yinggehai basin experienced dextral pull-apart.Bounded by NS-trending Yingxi fault, the transtensional areas mainly are the northwest part and along the eastern boundary of the basin. (2) From 42 to 21 Ma, the development of the main rift body in Yinggehai basin was mainly controlled by the southward slip and clockwise rotation of the Indochina block along the Red River fault zone, and the sedimentation was strengthened due to the sinistral transtension.In the east, the subsidence is deepened due to the dextral transtension. (3) From 21 to 10.4 Ma, the sinistral movement of the Indochina block slowed down to still.From 21 to 15.5 Ma, the northwest part of the basin began to inverse locally because of post-rift thermal subsidence of the whole basin. (4) From 10.4 Ma to present, the basin was affected by the dextral movement of the South China block along the Red River fault zone and thermal accident in a new phase at 5 Ma.
- Yinggehai basin,
- tectonic evolution,
- strong subsidence,
- analogue modeling

FullText(HTML)

References(49)

References

Allen, C.R., Gillespie, A.R., Han, Y., et al., 1984. Red River and associated faults, Yunnan Province, China: Quaternary geology, slip rates and seismic hazard. Geol. Soc. Am. Bull., 95: 686-700. doi: 10.1130/0016-7606(1984)95<686:RRAAFY>2.0.CO;2

Chen, C.M., Shi, H.S., Xu, S.C., et al., 2003. The condition of oil and gas reservoir formation in the east of Pearl River Mouth basin. Science Press, Beijing, 43-76 (in Chinese).

Clift, P.D., Lin, J., Barckhausen, U., 2002. Evidence of low flexural rigidity and low viscosity of lower continental crust in the South China Sea. Mar. Pet. Geol., 19: 951-970. doi: 10.1016/S0264-8172(02)00108-3

Clift, P.D., Sun, Z., 2006. The sedimentary and tectonic evolution of the Yinggehai-Song Hong basin and the southern Hainan margin, South China Sea: Implications for Tibetan uplift and monsoon intensification. J. Geophys. Res., 111 (B6) : B06405, doi: 10.1029/2005JB004048.

Davy, P., Cobbold, P.R., 1991. Experiment on shortening of a 4-layer model of the continental lithosphere. Tectonophysics, 188: 1-25. doi: 10.1016/0040-1951(91)90311-F

Gilley, L.D., Harrison, T.M., Leloup, P.H., et al., 2003. Direct dating of left-lateral deformation along the Red River shear zone, China and Vietnam. J. Geophys. Res. , 108, 2, 2127, doi: 10.1029/2001JB001726.

Gong, Z.S., Li S.T., Wang S.S., et al., 1997. Continental margin basin analysis and hydrocarbon accumulation of the northern South China Sea. Science Press, Beijing, 81-89 (in Chinese).

Guo, L.Z., Zhong, Z.H., Wang, L.S., et al., 2001. Regional tectonic evolution around Yinggehai basin of South China Sea. Geological Journal of China Universities, 7 (1) : 1-12 (in Chinese with English abstract). https://oversea.cnki.net/kcms/detail/detail.aspx?dbcode=cjfd&dbname=cjfd2001&filename=GXDX200101000

Harrison, T.M., Leloup, P.H., Ryerson, F.J., et al., 1996. Diachronous initiation of transtension along the Ailaoshan-Red River shear zone, Yunnan and Vietname. In: Yin, A., Harrison, T.M., eds., The tectonic evolution of Asia. Cambridge Univ. Press, New York, 208-226.

Hong, H.J., Li, T., Guo, S.M., et al., 1998. Research on tectonic composite of the Yinggehai and the Qiongdongnan basin andits relation with oil & gas. Report of China Offshore Oil Nanhai West Corporation (in Chinese).

Lee, T.Y., Lawver, L.A., 1995. Cenozoic plate reconstructions of Southeast Asia. Tectonophysics, 25: 8-138. https://www.sciencedirect.com/science/article/pii/0040195195000232

Leloup, P.H., Arnaud, N., Lacassin, R., et al., 2001. New constraints on the structure, thermochronology, and timing of the Ailao Shan-Red River shear zone, SE A sia. J. Geophys. Res., 106: 6683-6732. doi: 10.1029/2000JB900322

Leloup, P.H., Harrison, T.M., Ryerson, F., et al., 1993. Structural, petrological and thermal evolution of a Tertiary ductile strike-slip shear zone, Diancang Shan, Yunnan. J. of Geophy. Res., 98: 6715-6743. doi: 10.1029/92JB02791

Li, S.T., Zhang, Q.M., 1997. Basin forming mechanism and its dynamics types. In: Gong, Z.S., Li S.T., Wang, S.S., et al., eds., Continental margin basin analysis and hydrocarbon accumulation of the northern South China Sea. Science Press, Beijing, 111-121 (inChinese).

Petrunin, A., Sobolev, S.V., 2006. What controls thickness of sediments and lithospheric deformation at a pullapart basin? Geology, 34 (5) : 389-392, doi: 10.1130/G22158.1.

Ru, K., 1988. The development of superimposed basin on the northern margin of the South China Sea and its tectonic significance. Oil and Gas Geology, 9 (1) : 12-18. (in Chinese with English abstract).

Sun, J.Z., Li, L.B., Yang, S.G., et al., 1995. Evolution of transform-extension in Yinggehai basin. Earth Science-Journal of China University of Geosciences, 20 (3) : 243-249 (in Chinese with English abstract).

Sun, Z., Zhong, Z.H., Zhou, D., et al., 2003. Deformation mechanism of the Red River fault zone during Cenozoic and the experimental evidences related to Yinggehai basin Formation. Journal of Tropical Oceanology, 22 (2) : 1-9.

Sun, Z., Zhong, Z.H., Zhou, D., et al., 2004. Experimental constraints on Cenozoic development of Ying-Qiong basin in NW South China Sea. In: Clift, P.D., Wang, P.X., Kuhnt, W., et al., eds., Continent-ocean interactions within East Asian marginal seas. AGU Monograph Series 149, Washington D.C., 109-120.

Sun, Z., Zhou, D., Zhong, Z.H., et al., 2003. Experimental evidence for the dynamics of the formation of the Yinggehai basin, NW South China Sea. Tectonophysics, 372: 41-58. doi: 10.1016/S0040-1951(03)00230-0

Sun, Z., Zhong, Z.H., Zhou, D., et al., 2006. Research on the dynamics of the South China Sea opening: Evidence from analogue modeling. Science in China (Series D), 49 (10) : 1053-1069. doi: 10.1007/s11430-006-1053-6

Tran, N.N., Yuji, S., Kentaro, T., et al., 2001. First SHRIMP U-Pb zircon dating of granulites from the Kontum massif (Vietnam) and tectonothermal implications. Journal of Asian Earth Sciences, 19: 77-84. doi: 10.1016/S1367-9120(00)00015-8

Tron, V., Brun, J.P., 1991. Experiments on oblique rifting in brittle-ductile systems. Tectonophysics, 188: 71-84. doi: 10.1016/0040-1951(91)90315-J

Wang, J.H., Yin, A., Harrison, T.M., et al., 2001. A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian zone. Earth and Planetary Science Letters, 188: 123-133. doi: 10.1016/S0012-821X(01)00315-6

Wang, P.L., Lo, C.H., Lee, T.Y., et al., 1998. Thermochronological evidence for the movement of the Ailaoshan-Red River shear zone: A perspective from Vietnam. Geology, 26: 887-890.

Xie, W.Y., Sun, Z., Zhang, Y.W., et al., 2007. The dynamic and hydrocarbon accumulation analysis of the inversion structures on the northern marginal basins of the South China Sea. Earth Science-Journal of China University of Geosciences (in press, in Chinese with English ab-stract).

Yang, K.S., 2000. Prediction of forming, evolution and type of reservoir of Yinggehai basin. Fault-Block Oil & Gas Field, 7 (2) : 4-11 (in Chinese with English abstract).

Yang, Z., Basse, J., 1993. Paleomagnetic study of Permian and Mesozoic sedimentary rocks from northern Thailand supports the extrusion model for Indochina. Earth and Planetary Science Letters, 117: 525-552. doi: 10.1016/0012-821X(93)90101-E

Yin, X.L., Ma, Y.S., Feng, X.Y., et al., 2005. Thermal stresses and their effects during the deep hot fluids penetrating upward in DF 1-1 diapiric area, Yinggehai basin. Earth Science-Journal of China University of Geosciences, 30 (1) : 83-88 (in Chinese with English abstract).

Zhang, Q.M., Hao, F., 1997. Evolution and hydrocarbon systemin Ying-Qiong basin. Science in China (Series D), 27 (2) : 149-154 (in Chinese).

Zhang, Q.M., 1999. Evolution of Yinggehai-Qiongdongnan basin and its tectonic-thermal mechanics. Natural GasIndustry, 19 (1) : 12-19 (in Chinese with English abstract).

Zhu, W.L., Jiang, W.R., 1998. Relation between fractures and hydrocarbon reservoirs in Weixinan sag. Acta Petroleum Sinica, 19 (3) : 6-11 (in Chinese with English abstract).

Zhong, Z.H., Wang, L.S., Xia, B., et al., 2004. The dynamics of Yinggehai basin formation andits tectonic significance. Acta Geologica Sinica, 78 (3) : 302-309 (in Chinese with English abstract).

陈长民, 施和生, 许仕策, 等, 2003. 珠江口盆地(东部) 第三系油气藏形成条件. 北京: 科学出版社, 43-76.

龚再升, 李思田, 王善书, 等, 1997. 南海北部大陆边缘盆地分析与油气聚集. 北京: 科学出版社, 81-89.

郭令智, 钟志洪, 王良书, 等, 2001. 莺歌海盆地周边区域构造演化. 高校地质学报, 7 (1) : 1-12. doi: 10.3969/j.issn.1006-7493.2001.01.001

洪汉净, 李涛, 虢顺民, 等, 1998. 莺-琼盆地构造复合及其与油气关系的研究. 中海石油西部公司研究报告.

李思田, 张启明, 1997. 盆地形成机制及其动力学类型. 龚再升, 李思田, 王善书, 等著, 南海北部大陆边缘盆地分析与油气聚集, 北京: 科学出版社, 111-121.

茹克, 1988. 南海北部边缘叠合式盆地的发育与其大地构造意义. 石油与天然气地质, 9 (1) : 21-31. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT198801002.htm

孙家振, 李兰斌, 杨世恭, 等, 1995. 转换-伸展盆地-莺歌海盆地的演化. 地球科学——中国地质大学学报, 20 (3) : 243-249. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX503.001.htm

孙珍, 钟志洪, 周蒂, 等, 2003. 红河断裂带的新生代变形机制及莺歌海盆地的实验证据. 热带海洋学报, 22 (2) : 1-9. doi: 10.3969/j.issn.1009-5470.2003.02.001

孙珍, 钟志洪, 周蒂, 等, 2006. 南海的发育机制研究——相似模拟证据. 中国科学(D), 36 (9) : 797-810. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200609001.htm

谢文彦, 孙珍, 张一伟, 等, 2007. 南海北部陆缘盆地新生代反转构造动力学与成藏分析. 地球科学——中国地质大学学报, 待刊.

杨克绳, 2000. 莺歌海盆地几个地质问题的探讨. 断块油气田, 7 (2) : 4-11. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT200002001.htm

殷秀兰, 马寅生, 冯向阳, 等, 2005. 莺歌海盆地东方1-1底辟区深部热流体穿层的热应力及其效应. 地球科学——中国地质大学学报, 30 (1) : 83-88. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200501011.htm

张启明, 1999. 莺琼盆地的演化与构造-热体制. 天然气工业, 19 (1) : 12-19. doi: 10.3321/j.issn:1000-0976.1999.01.004

张启明, 郝芳, 1997. 莺-琼盆地演化与含油气系统. 中国科学(D), 27 (2) : 149-154. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199702009.htm

钟志洪, 王良书, 夏斌, 等, 2004. 莺歌海盆地成因及其大地构造意义. 地质学报, 78 (3) : 302-309. doi: 10.3321/j.issn:0001-5717.2004.03.003

朱伟林, 江文荣, 1998. 北部湾盆地涠西南凹陷断裂与油气藏. 石油学报, 19 (3) : 6-11. doi: 10.3321/j.issn:0253-2697.1998.03.002

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(7) / Tables(2)

Get Citation

PDF

XML

Article views (3528) PDF downloads(298)

The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content