| 岩(矿)石磁参数与原生晕关系的研究及其地质意义 |
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| 引用本文： | 齐家喆,李燕. 岩(矿)石磁参数与原生晕关系的研究及其地质意义[J]. 物探与化探, 1990, 14(2): 135-143 |
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| 作者姓名： | 齐家喆 李燕 |
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| 作者单位： | 广西地矿局物探队(齐家喆)，广西地矿局物探队(李燕) |
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| 摘 要： | 本文阐述了岩浆热液矿床中含磁性的岩(矿)石磁参数和其些元素原生晕的数据处理。发现岩(矿)石磁性和某些元素热液渗滤晕之间存在着某种关系。通过获取某特征值,可以发掘元素组合、成矿阶段、矿体赋存规律等方面的信息。这些信息,具有很重要的地质找矿意义。
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| 关 键 词： | 岩石 磁参数 原生晕 矿石 找矿 |
THE RELATIONSHIP BETWEEN MAGNETIC PARAMETERSOF ROCKS (ORES) AND PRIMARY HALOES AND ITSGEOLOGICAL SIGNIFICANCE |
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| Affiliation: | Geopnysical Prospecting Party, Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonmous Region |
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| Abstract: | This paper deals with the magnetic parameters of rocks (ores) frommagmatic-hydrothermal ore deposits and the data-processing of primaryhaloes. It is found that a certain relationship exists between the magneticproperties of rocks (ores) and the hydrothermal leakage haloes of some ele-ments. By evaluating its characteristic values, we can obtain information insuch aspects as element association, ore-forming stage and mode of occurrenceof the orebody. Such information is of great geological-ore prospecting signifi-cance. |
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