| 北京石花洞的岩溶地质特征 |
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| 引用本文： | 吕金波,李铁英,孙永华,车用太.北京石花洞的岩溶地质特征[J].地质通报,1999,18(4):42. |
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| 作者姓名： | 吕金波 李铁英 孙永华 车用太 |
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| 作者单位： | 1. 国家地震局地质研究所,北京,100029
2. 北京市地质调查所,北京,102206 |
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| 摘 要： | 在全国范围内，北京石花洞洞层最多，钟乳石叠置关系明显，石笋中具有微层理，月奶石发育最好。这些特征为研究西山的新构造运动及古环境的变化提供了新的信息，奠定了首次利用钟乳石建立第四系剖面的基础。
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| 关 键 词： | 洞层 微层理 月奶石 钟乳石剖面 石花洞 |
| 文章编号： | 1000-3967(1999)04-0373-06 |
| 修稿时间： | 1998-05-17 |
Karst geology of the Shihua cave,Beijing |
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| L Jin-bo,LI Tie-ying,SUN Yong-hua,CHE Yong-tai.Karst geology of the Shihua cave,Beijing[J].Geologcal Bulletin OF China,1999,18(4):42. |
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| Authors: | L Jin-bo LI Tie-ying SUN Yong-hua CHE Yong-tai |
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| Institution: | L(U) Jin-bo,LI Tie-ying,SUN Yong-hua,CHE Yong-tai |
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| Abstract: | Across China,Shihua cave is well known for its characteristic multi levels,superimposed stalactite,micro banding and best developed moonmilk.These features provide new information for understanding the neo tectonics and paleo environment in Xishan area,and also help to set up Quaternary stratigraphy by study of stalactite for the first time. |
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| Keywords: | cave level micro banding moonmilk stalactite section Shihua cave |
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