| 陆相残余盆地的主要类型、特点及研究方法 |
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| 引用本文： | 蔡雄飞,王德珲,章泽军.陆相残余盆地的主要类型、特点及研究方法[J].世界地质,2004,23(3):221-226. |
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| 作者姓名： | 蔡雄飞 王德珲 章泽军 |
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| 作者单位： | 中国地质大学,地球科学学院,湖北,武汉,430074 |
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| 基金项目： | 国家地调项目:田坂街、游城幅联测(20001300002051) |
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| 摘 要： | 根据我国中生代陆相盆地演化特征，认为陆相盆地不存在原始沉积盆地。陆相残余盆地的基本特征，具有空间上盆地面积大为缩小，地层遭受明显剥蚀，受后期改造而成。提出了两种基本类型和它们的沉积特点以及追踪物质来源、去改造层是恢复残余盆地的基本方法，并以古鄱阳湖中生代盆地为例。
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| 关 键 词： | 陆相盆地 残余盆地 沉积特点 研究方法 |
| 文章编号： | 1004-5589(2004)03-0221-06 |
Types,features and studying method of continental relict basins |
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| CAI Xiong-fei,WANG De-hui,ZHANG Ze-junFaculty of Earth Sciences,China University of Geosciences,Wuhan ,Hubei,China.Types,features and studying method of continental relict basins[J].World Geology,2004,23(3):221-226. |
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| Authors: | CAI Xiong-fei WANG De-hui ZHANG Ze-junFaculty of Earth Sciences China University of Geosciences Wuhan Hubei China |
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| Institution: | CAI Xiong-fei,WANG De-hui,ZHANG Ze-junFaculty of Earth Sciences,China University of Geosciences,Wuhan 430074,Hubei,China |
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| Abstract: | According to the evolution of Mesozoic continetal basins,there was no proto-compressive continental basins in China. The continental relict basins characterized by their much smaller than prototype basins,noticeable denudation,considerable changes of proto-compressive basin appearance. It was formed by the later tectogenesis. There are mainly two types and some sedimentary features dealing with searching source of the basal payet rock and eliminated tectonic layers have been recovered as mainly working method of the relict basin. An example from Mesozoic basin of Old Poyanghu Lake. |
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| Keywords: | continental basin relict basin sedimentary feature study method |
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