| 秦皇岛地区典型地表喀斯特地貌成因分析 |
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| 引用本文： | 路洪海,张重阳.秦皇岛地区典型地表喀斯特地貌成因分析[J].聊城大学学报(自然科学版),2007,20(1):61-63. |
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| 作者姓名： | 路洪海 张重阳 |
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| 作者单位： | 聊城大学,环境与规划学院,山东,聊城,252059 |
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| 基金项目： | 致谢 感谢李庆朝教授、石立岩教授的野外指导与帮助! |
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| 摘 要： | 通过实地观察与分析,认为秦皇岛地区沙锅店典型地表喀斯特地貌的发育应始于白垩纪后,巨厚的花岗斑岩岩墙对典型喀斯特地貌的发育起了关键作用,而左旋断层的存在则进一步促进了喀斯特地貌的发育.
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| 关 键 词： | 喀斯特地貌 成因 秦皇岛 |
| 文章编号： | 1672-6634（2007）01-0061-03 |
| 修稿时间： | 2006-11-15 |
The Formation of Typical Bare Karst in Qinghuangdao |
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| LU Hong-hai,ZHANG Chong-yang.The Formation of Typical Bare Karst in Qinghuangdao[J].Journal of Liaocheng University:Natural Science Edition,2007,20(1):61-63. |
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| Authors: | LU Hong-hai ZHANG Chong-yang |
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| Institution: | School of Environment and Planning,Liaocheng University,Liaocheng 252059,China |
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| Abstract: | By the field research and analysis, the typical bare karst in Qinghuangdao might be developed after the Cretaceous. The thick granite-porphyry dike is the key factors to the formation of the typical bare karst,and the laevogyrate fault accelerates the formation of the karst. |
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| Keywords: | the typical karst the cause of formation Qinghuangdao |
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