| 田黄的X射线衍射研究 |
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| 引用本文： | 韩景仪,郭立鹤. 田黄的X射线衍射研究[J]. 岩石矿物学杂志, 2010, 29(Z1): 85-87 |
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| 作者姓名： | 韩景仪 郭立鹤 |
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| 作者单位： | 中国地质科学院矿产资源研究所; |
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| 摘 要： | 用X射线衍射分析的方法测定了12个田黄样品,其中,青田石1个,寿山石9个,昌化田黄石2个。确定青田石由叶蜡石(58%)、绢云母(36.1%)和高岭石(5.9%)组成;昌化田黄石由迪开石组成;寿山石分别由迪开石、高岭石、叶蜡石及绢云母组成。
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| 关 键 词： | X射线衍射分析 田黄石 福州 |
An X-ray diffraction study of Tianhuang Stone |
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| HAN Jing_yi and GUO Li_he. An X-ray diffraction study of Tianhuang Stone[J]. Acta Petrologica Et Mineralogica, 2010, 29(Z1): 85-87 |
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| Authors: | HAN Jing_yi and GUO Li_he |
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| Affiliation: | HAN Jing-yi and GUO Li-he(Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China) |
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| Abstract: | X-ray diffraction method was employed to analyze twelve Tianhuang samples, which include one Qingtian Stone sample, nine Shoushan Stone samples and two Changhua Tianhuang Stone samples. The results show that Qingtian Stone consists of pyrophyllite(58%), sericite (36.1%) and kaolinite (5.9%), Changhua Tianhuang Stone is composed of dickite, and Shoushan Stone is comprised respectively of dickite, kaolinite, pyrophyllite and sericite. |
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| Keywords: | X-ray diffraction analysis Tianhuang Stone Fuzhou |
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