Evolution of Cenozoic Sedimentary Basins in Eastern China
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摘要: 新生代, 中国东部大陆边缘系统总体受到来自印度、澳大利亚、菲律宾和太平洋板块向欧亚板块下部俯冲碰撞的作用, 在大陆边缘形成一系列边缘海盆地和断陷-坳陷盆地, 主要发育松辽、渤海湾、江汉、苏北、东海、珠江口和北部湾等盆地.基于中国东部沉积盆地的中生代构造背景分析和新生代盆地的分布特征, 对其中的7个主要沉积盆地进行了详细的沉积序列和构造演化分析.通过周缘板块和郯庐断裂的构造演化、火山活动、低温热年代学、气候演变等对比分析, 中国东部沉积盆地的演化可划分为3个阶段: 古新世-始新世、渐新世-早中新世和晚中新世-第四纪.Abstract: With subduction collision between Eurasian plate and surrounding plates such as Indian, Australian, Philippine and Pacific plates, a series of marginal sea basins, and faulted-downwarped basins formed in the continental margin of eastern China, mainly including Songliao, Bohai Bay, Jianghan, Subei, East China Sea, Pearl River Mouth and Beibuwan basins. Based on Mesozoic tectonic background analysis and Cenozoic distribution characteristics of sedimentary basins in eastern China, sedimentary sequence and tectonic evolution of 7 main basins are analyzed in detail.through a comparative study of tectonic evolution of the surrounding plates and the Tan-Lu fault, volcanism, low temperature thermochronology, climatic evolvement, and so on.It is found that the tectonic evolution of the sedimentary basins in eastern China can be divided into three phases, which are Paleocene-Eocene, Oligocene-Early Miocene and Late Miocene-Quaternary respectively.
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Key words:
- tectonics /
- sedimentology /
- basin evolution /
- Cenozoic /
- eastern China
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图 1 中国东部中生代地层露头分布和大地构造略图
图a的大型断裂系发育特征据马杏垣等(1983)，Ren et al.(2002)和万天丰和朱鸿(2002)；图b的大型断裂系发育特征据陈丕基(1988)，朱夏(1990)，李显武和周新民(1999)，李廷栋和莫杰(2002)，Ren et al.(2002)，舒良树等(2004)，孙晓猛等(2005)和索艳慧等(2012)
Fig. 1. Distribution of Menozoic strata and tectonic map in eastern China
图 2 中国东部新生代沉积盆地分布和构造略图
1.漠河坳陷盆地；2.海拉尔断陷-坳陷盆地；3.二林浩特断陷-坳陷盆地；4.松辽断陷-坳陷盆地；5.依兰走滑拉分盆地；6.伊通走滑拉分盆地；7.佳木斯-江断陷-坳陷盆地；8.敦化压陷盆地；9.延吉坳陷盆地；10.渤海湾断陷-拉分盆地；11.华北南部断陷-坳陷盆地群；12.合肥压陷盆地；13.胶莱断陷-拉分盆地；14.汾渭断陷盆地；15.鄂尔多斯压陷盆地；16.二连浩特断陷-凹陷盆地；17.南襄压陷盆地；18.吉安断陷-坳陷盆地群；19.十万大山断陷盆地；20.湛江走滑拉分盆地；21.三江断陷盆地；22.汕头断陷盆地；23.厦门断陷盆地；24.海南环岛断陷-坳陷盆地；25.台西断陷盆地；26.北部湾盆地；27.莺歌海盆地；28.珠江口-琼东南盆地；29.台西南盆地；30.东海盆地；31.长沙-衡阳断陷-坳陷盆地；32.南昌断陷-坳陷盆地；33.九江-芜湖走滑拉分盆地；34.苏北断陷-坳陷盆地；35.南黄海盆地；36.江汉-洞庭湖断陷-坳陷盆地；37.成都压陷盆地；38.百色断陷-坳陷盆地.主要参考文献：Northrup et al., 1995; Allen and Macdonald, 1997; Grimmer et al., 2002; 李国玉等，2002; Ren et al., 2002; 万天丰和朱鸿, 2002; 胡望水等, 2003; Zhang et al., 2003; 赵金海, 2004a, 2004b; 邱海峻等, 2006; 王必金等, 2006; Yin, 2010; Li et al., 2011, 2012; 索艳慧等, 2012; 王五力等, 2012; 石红才等, 2013
Fig. 2. Distribution and tectonic map of Cenozoic sedimentary basins in eastern China
图 3 中国东部主要大型盆地充填序列及其对比
据参考文献: 郑亚惠和周山富, 1983; 李云通, 1984; 吴做基, 1985; 安延恺和苏鸣钧, 1990; England and Molnar, 1990; Hunziker et al., 1992; 王国纯和朱伟林, 1992; 康西栋等, 1994; 徐论勋等, 1995; 钱勤，1997; 覃建雄等, 1998; 郑家坚等, 1999; 陈长民, 2000; 陈琳琳等, 2003; 刘丽军等, 2003; 郭华等, 2006; 方石等, 2007; 邵磊等, 2008; 赵中贤等, 2009; 《中国地层典·总论》编委会, 2009; 冯有良等, 2010; 李珊珊等，2010; 魏祥峰等, 2011; 李上卿等, 2012; 李向阳等, 2012
Fig. 3. Correlation and sedimentary sequence of the main Cenozoic basins in the eastside of China
图 4 中国东部主要大型盆地演化及其对板块运动的响应
据参考文献：Seno and Maruyama, 1984; Kimura, 1985; Jolivet et al., 1994; 任建业和李思田, 2000; Liu et al., 2001; 李娟和舒良树, 2002; Ren et al., 2002; 万天丰和朱鸿, 2002; 孙晓猛等, 2005; 方石等, 2008; Zhang et al., 2008, 2010; Wang et al., 2011; 索艳慧等, 2012; 石红才等, 2013; Wang and Shu, 2013; 张克信等, 2013
Fig. 4. Evolution of the main Cenozoic basins in the eastern China and their response to plate motion
图 5 江汉-苏北-东海盆地一线新生代构造演化阶段示意
据参考文献：Grimmer et al., 2002; Ren et al., 2002; 胡望水等, 2003; Zhang et al., 2003; 赵金海, 2004a, 2004b; 朱光等, 2004; 邱海峻等, 2006; 王必金等, 2006; Li, 2012
Fig. 5. Cenozoic tectonic evolution phases along Jianghan-Subei-East China Sea basins in the eastern China
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