| 北京石花洞“石花”的晶体结构、矿物组成及形态发育模拟分析 |
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| 引用本文： | 段武辉,谭明,喻学惠,施光海. 北京石花洞“石花”的晶体结构、矿物组成及形态发育模拟分析[J]. 中国岩溶, 2008, 27(3): 201-208. DOI: 10.3969/j.issn.1001-4810.2008.03.002 |
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| 作者姓名： | 段武辉 谭明 喻学惠 施光海 |
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| 作者单位： | 1.中国科学院地质与地球物理研究所新生代地质与环境重点实验室 2. 中国地质大学 |
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| 摘 要： | 以北京石花洞的石花为研究对象 ,将其分为基底、根部、冠部三个部分。 通过实地观察监测、显微镜和扫描电镜观察、 X射线粉晶衍射以及模拟石花生长实验 ,分析并确定石花的矿物组成 ,讨论其形成条件和造貌水动力特征 ,结果表明:( 1)石花晶体呈树枝状结构 , 其附生基底的矿物几乎全部为方解石 ,仅含极少微量的杂质;石花根部方解石含量 > 90% ,文石及少量杂质含量 < 5% ;石花冠部文石含量 > 90% ,方解石及杂质含量 < 5% ;而就石花整体而言 ,其矿物组成为文石含量> 90% ,方解石及杂质含量 < 5% 。 ( 2)形成石花的环境条件为较封闭、气温稍低但较稳定、洞内湿度较低且气流扰动小。 ( 3)形成石花的造貌水动力为来自基底内部渗出孔隙水的毛细作用。
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| 关 键 词： | 石花 矿物成分 形成条件 造貌水动力 模拟实验 北京石花洞 |
Analysis of the crystal structure, mineral component and simulated evolution of the cave flower from Beijing Shihua cave |
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| DUAN Wu-hui,TAN Ming,YU Xue-hui and SHI Guang-hai. Analysis of the crystal structure, mineral component and simulated evolution of the cave flower from Beijing Shihua cave[J]. Carsologica Sinica, 2008, 27(3): 201-208. DOI: 10.3969/j.issn.1001-4810.2008.03.002 |
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| Authors: | DUAN Wu-hui TAN Ming YU Xue-hui SHI Guang-hai |
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| Affiliation: | 1. Key Laboratory of Cenozoic Geology and Environmet , Institute of Geology and Geophysics , Chinese Academy of Sciences 2.China University of Geosciences |
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| Abstract: | This paper focuses on the study of a cave flower from Beijing Shihua cave. This cave flower can be divided into three parts here： the base, the root and the crown part. By means of microscope observations, x-ray power diffraction analysis, scan electron microscope analysis and the simulated experiment, the authors attempt to determine the mineral composition, to analyze the conditions under which the cave flower formed and the hydrologic dynamics which create this unique cave flower. The results show that： （1） The crystal possesses spatial distribution pattern of arborization. The speleothem base part on which the cave flower grows is almost composed of calcite with a little impurity. The root part of the cave flower contains more than 90% calcite and less than 5% aragonite as well as trace impurity. Whereas, the crown part contains more than 90% aragonite with needle-like crystal shape and less than 5% calcite as well as trace impurity. Therefore, the total of the cave flower contains more than 90% aragonite and less than 5% calcite and trace impurity. （2） The cave flower formed in low and stable temperature and a rather dry condition. （3） The shaping dynamics originating from capillary action, which drives the water seeping from the base, could be mainly responsible for the formation of the cave flower. |
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| Keywords: | cave flower mineral composition formation conditions hydraulic conditions for morph formation simulated experiment Beijing Shihua cave |
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