| 论中国东部中、新生代大地构造的基本特征 |
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| 引用本文： | 林宗满.论中国东部中、新生代大地构造的基本特征[J].地质力学学报,2010,16(3):246-259. |
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| 作者姓名： | 林宗满 |
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| 作者单位： | 中国地质科学院地质力学研究所，北京 100081 |
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| 基金项目： | 国家科技支撑计划重点项目(编号: 2007BAB25B02) 资助。 |
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| 摘 要： | 把中国东部中、新生界划分为6个构造-沉积旋回, 相应地发育6期构造运动主幕, 侏罗纪末幕运动是一场变格运动。进一步将研究区构造形变史划分为两个形变阶段和一个过渡阶段。两个构造形变阶段发育两种类型的沉积盆地、两种型式的构造体系, 它们之间存在着广泛的构造不整合, 显示二元结构即为中国东部中、新生代大地构造的基本特征。
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| 关 键 词： | 中国东部 中、新生代 构造—沉积旋回 大地构造 形变阶段 构造体系 |
| 收稿时间： | 2009/12/24 0:00:00 |
GENERAL CHARACTERISTICS OF THE MESOZOIC-CENOZOIC TECTONICS IN EASTERN CHINA |
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| LIN Zong-man.GENERAL CHARACTERISTICS OF THE MESOZOIC-CENOZOIC TECTONICS IN EASTERN CHINA[J].Journal of Geomechanics,2010,16(3):246-259. |
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| Authors: | LIN Zong-man |
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| Institution: | Institute of Geomechanics, Chinese Academy of Geological Science, Beijing 100081, China |
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| Abstract: | In this paper,the author divided the Mesozoic-Cenozoic in eastern China into six tectonic-sedimentary cycles.The movement occurred in the Late Jurassic was a style-changed movement.In addition,the author further divided the tectonic deformation history of this region into two deformation phases(T-J) and one transitional phase(K1).During the two deformation phases,two types of basins and two tectonic systems developed.There exists extensive tectonic unconformity,which shows that the duel structures are basic... |
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| Keywords: | Eastern China Mesozoic-Cenozoic tectonic-sedimentary cycle geotectonics defor-mation phases tectonic system |
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