| 金红石磁化率的研究 |
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| 引用本文： | 肖金凯,张惠芬.金红石磁化率的研究[J].矿物学报,1989,9(1):76-81. |
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| 作者姓名： | 肖金凯 张惠芬 |
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| 作者单位： | 中国科学院地球化学研究所 贵阳
(肖金凯)，中国科学院地球化学研究所 贵阳(张惠芬) |
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| 摘 要： | 本文讨论了不同类型金红石样品磁化率的测定结果。金红石的磁化率与其铁的含量明显相关。其磁性来源主要有三:类质同象形式的铁离子的顺磁性(这是主要的)、出港相含钛赤铁矿的反铁磁性和出溶相钛铁矿的顺磁性。
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| 关 键 词： | 金红石 磁化率 |
A STUDY OF THE KAGNETIC SUSCEPTI BILITY OF RUTILE |
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| Xiao Jinkai,Zhang Huifen Institute of Geochemistry,Academia Sinica.A STUDY OF THE KAGNETIC SUSCEPTI BILITY OF RUTILE[J].Acta Mineralogica Sinica,1989,9(1):76-81. |
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| Authors: | Xiao Jinkai Zhang Huifen Institute of Geochemistry Academia Sinica |
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| Abstract: | The measured results of magnetic susceptibility for different types of rutileare presented in this paper. There is an obvious positive correlation betweenmagnetic susceptibility and iron content in rutile. The magnetic properties ofrutile are ascribed to the paramagnetism of isomorphic iron ions, the antife-rromagnetism of the exsolution phase-titanoferrous hematite and the para-magnetism of the exsolution phase-ilmenite. |
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| Keywords: | susceptibility rutile Abstract |
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