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| 中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲 | |
| 引用本文： | 李三忠,张国伟,周立宏,赵国春,刘鑫,索艳慧,刘博,金宠,戴黎明.中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲[J].地学前缘,2011,18(3):79-107. |
| 作者姓名： | 李三忠 张国伟 周立宏 赵国春 刘鑫 索艳慧 刘博 金宠 戴黎明 |
| 作者单位： | 1. 海底科学与探测技术教育部重点实验室,山东青岛,266100;中国海洋大学海洋地球科学学院,山东青岛,266100 2. 海底科学与探测技术教育部重点实验室,山东青岛,266100;中国海洋大学海洋地球科学学院,山东青岛,266100;西北大学地质学系,陕西西安,710069 3. 中国石油大港油田公司,天津,300280 4. 香港大学,中国香港 5. 浙江大学,浙江杭州,310012 |
| 基金项目： | 国家自然科学基金项目(41072152); 中国地质调查局项目(1212011120103); 国家高技术研究发展计划“863”项目(2009AA093401) |
| 摘 要： | 中、新生代期间,太平洋板块向西俯冲、印度板块向北俯冲于欧亚板块下以及中生代鄂霍次克海的消亡导致中亚造山带的向南俯冲,三者围限的中心三角形地带正是中国东部两个核心地块--华北和华南地块,而且,该区中、新生代始终处于全球三大构造域超级汇聚的中心.但是,在这种超级汇聚背景下,分别于华北和华南陆块的核部形成了两种截然相反的构造... |
| 关 键 词： | 渤海湾盆地 华北克拉通 华南陆块 深部构造 大陆动力学 |
The opposite Meso-Cenozoic intracontinental deformations under the super-convergence:Rifting and extension in the North China Craton and shortening and thrusting in the South China Craton |
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| Li Sanzhong,Zhang Guowei,Zhou Lihong,Zhao Guochun,Liu Xin,Suo Yanhui,Liu Bo,Jin Chong,Dai Liming.The opposite Meso-Cenozoic intracontinental deformations under the super-convergence:Rifting and extension in the North China Craton and shortening and thrusting in the South China Craton[J].Earth Science Frontiers,2011,18(3):79-107. | |
| Authors: | Li Sanzhong Zhang Guowei Zhou Lihong Zhao Guochun Liu Xin Suo Yanhui Liu Bo Jin Chong Dai Liming |
| Institution: | Li Sanzhong1,2,Zhang Guowei1,3,Zhou Lihong4,Zhao Guochun5,Liu Xin1,Suo Yanhui1,Liu Bo1,Jin Chong6,Dai Liming1,21.Key Lab of Submarine Geosciences and Exploration Techniques,Ministry of Education,Qingdao 266100,China2.College of Marine Geoscience,Ocean University of China,China3.Department of Geology,Northwest University,Xi'an 710069,China4.Dagang Oilfield Company,CNPC,Tianjin 300280,China5.Department of Earth Sciences,The University of HongKong,HongKong,China6.Zhejiang University,Hang... |
| Abstract: | During the Mesozoic and the Cenozoic,two important blocks in East China,the North China and South China blocks,were exactly a center surrounded by westward subduction of the Pacific Plate,northward subduction of the India Plate beneath the Eurasian Plate and southward subduction of the Central Asian Orogen due to Mesozoic Okhotsk Sea.It was a convergent center of the three global tectonic domains.Under the same setting of the super-convergence,two distinct structures are the extensional structures in the Me... |
| Keywords: | Bohai Bay Basin North China Craton South China Block deep tectonic process continental dynamics |
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