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    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

    孙珍, 钟志洪, 周蒂, 2007. 莺歌海盆地构造演化与强烈沉降机制的分析和模拟. 地球科学, 32(3): 347-356.
    引用本文: 孙珍, 钟志洪, 周蒂, 2007. 莺歌海盆地构造演化与强烈沉降机制的分析和模拟. 地球科学, 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.

    莺歌海盆地构造演化与强烈沉降机制的分析和模拟

    基金项目: 

    中国科学院知识创新工程重要方向项目 KZCX3-SW-234-3

    国家自然科学基金项目 40406012

    详细信息
      作者简介:

      孙珍(1971-), 女, 副研究员, 主要从事构造分析与模拟研究.E-mail: zhensun@scsio.ac.cn

    • 中图分类号: P554

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

    • 摘要: 莺歌海盆地新生代发生了快速沉降, 盆内充填了最厚达17 km的沉积, 根据模拟实验, 印支地块或之上刚性地块的存在对莺歌海盆地的强烈沉降具有重要的贡献, 可能是造成莺歌海盆地裂陷期强烈沉降的重要原因之一.结合地质分析和物理模拟实验, 莺歌海盆地的演化大致可以分为以下4个主要阶段: 早期(42 Ma以前) 主要受到南海北部陆缘(主要是北部湾盆地) 裂解造成的右旋转换伸展作用的影响, 但影响范围较小, 主要为莺歌海盆地西北部和东部边界.42~21 Ma期间, 主要受控于印支地块左行走滑和顺时针旋转作用的影响, 莺歌海盆地在此期间发育了主体裂陷体系, 东侧受到右旋转换伸展应力场的叠加影响而导致沉降加强; 21~10.4 Ma期间, 受印支地块逐渐减弱直至停止的左行走滑作用的影响, 盆地西北部在21~15.5 Ma期间发生局部反转褶皱, 但盆地整体进入以热沉降为主的时期; 10.4 Ma以后, 盆地受华南地块沿红河断裂右旋走滑作用和5 Ma以后新一期热事件的影响.

       

    • 图  1  莺歌海盆地主要断裂结构和新生代沉积等厚图

      图  2  莺歌海盆地的两条地震剖面

      剖面位置见图 1, 其中剖面1解释据钟志洪等(2004); 剖面2解释据杨克绳(2000)

      Fig.  2.  Two seismic profiles of the Yinggehai basin

      图  3  莺歌海盆地Moho面深度等值伐图(据龚再升等编制, 1997)

      Fig.  3.  Moho isometric in the Yinggehai basin

      图  4  莺歌海盆地913393剖面沉降速率(龚再升等, 1997)

      Fig.  4.  Subsiding rate on Profile 913393 of the Yinggehai basin

      图  5  莺歌海盆地先右旋后左旋转换伸展作用下变形的表面图

      其中, A2、B2分别为A1、B1的解释结果, 虚线指示基底板

      Fig.  5.  Surface view of the experiment after dextral transtension and sinistral transtension in turn

      图  6  印支地块上未设置(A1, A2)和设置了刚性构造地块(B1, B2) 情况下表面变形样式的对比

      A2、B2分别为A1、B1的解释结果, 虚线椭圆指示刚性地块的位置, 白色实线为南倾断裂, 黑色实线为北倾断裂, 箭头指示地块运动方向

      Fig.  6.  Surface view comparison between model without and with rigid massif on Indochina block

      图  7  印支地块上未设置(P1)和设置了刚性构造地块(P2) 情况下最大垂向断距分布对比

      黑色实线代表断层, 箭头指示断层运动方向; 剖面位置见图 6中P1和P2

      Fig.  7.  Maximum vertical offset along profile of models without (P1) or with (P2) rigid massif

      表  1  莺歌海盆地构造演化模拟模型参数

      Table  1.   Modeling parameters used in the tectonic evolution experiment of Yinggehai basin

      表  2  设置刚性地块的模型参数

      Table  2.   Parameters used in the experiment with rigid massif

    • 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
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    • 收稿日期:  2006-08-28
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