| X—ray Powder Diffraction Characterization of Pyrope |
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| 引用本文： | 王冠鑫 龚国洪. X—ray Powder Diffraction Characterization of Pyrope[J]. 中国地球化学学报, 1990, 9(3): 284-288. DOI: 10.1007/BF02837692 |
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| 作者姓名： | 王冠鑫 龚国洪 |
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| 作者单位： | InstituteofGeochemistry,AcademiaSinica |
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| 摘 要： | I332／I422，the intensity ratio of powder diffraction,is highly sensitive to variations in garnet compositon and can be taken as an identification criterion for pyrope:I332/I422-1 for pyrope while it is much smaller than unit for other members of the garnet group.
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| 关 键 词： | 榴子石 X射线 晶体结构 石榴石 组成 |
X-ray powder diffraction characterization of pyrope |
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| Wang Guanxin,Gong Guohong. X-ray powder diffraction characterization of pyrope[J]. Chinese Journal of Geochemistry, 1990, 9(3): 284-288. DOI: 10.1007/BF02837692 |
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| Authors: | Wang Guanxin Gong Guohong |
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| Affiliation: | (1) Institute of Geochemistry, Academia Sinica, China |
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| Abstract: | I332/I422, the intensity ratio of powder diffraction, is highly sensitive to variations in garnet composition and can be taken as an identification criterion for pyrope: I332/I422 ~ 1 for pyrope while it is much smaller than unit for other members of the garnet group. |
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