| 湘中南推覆构造及其产出的大地构造背景 |
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| 引用本文： | 王志鸿,陈世益,周芳.湘中南推覆构造及其产出的大地构造背景[J].成都理工大学学报(自然科学版),1990(4). |
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| 作者姓名： | 王志鸿 陈世益 周芳 |
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| 作者单位： | 成都地质学院地质学系
(王志鸿)，中南工业大学
(陈世益)，中南工业大学(周芳) |
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| 摘 要： | 湖南中南部于中新生代地洼发展阶段发育许多推覆构造,基本特征与发育于地槽褶皱带的阿尔卑斯式推覆构造不同,表现在:数量多,分布广,单个推覆构造规模较小,推覆方向各异,成因类型多。
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| 关 键 词： | 湖南 地洼型推覆构造 地洼区 大地构造背景 中新生代 煤田 |
NAPPE STRUCTURES IN CENTRAL-SOUTH HUNAN AND GEOTECTONIC SETTING OF THEIR DEVELOPMENT |
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| Wang Zhihong,Chen Shiyi,Zhou Fang.NAPPE STRUCTURES IN CENTRAL-SOUTH HUNAN AND GEOTECTONIC SETTING OF THEIR DEVELOPMENT[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1990(4). |
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| Authors: | Wang Zhihong Chen Shiyi Zhou Fang |
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| Institution: | Wang Zhihong;Chen Shiyi;Zhou Fang |
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| Abstract: | Many nappe structures were developed in Central-South Hunan during Diwa developingstage of Meso-Cenozoic period. Their essential characteristics are different from those of the Alpino-type nappe structures occurred in geosynclinal fold belt. It is of important significance for regional ge-ological investigation and reconnaissance to describe this kind of structure pattern. |
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| Keywords: | Hunan Diwa-type nappe structures Diwa region geotectonic setting Meso-Cenozoic coalfild |
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