| 浙东南遂昌湖山萤石矿田成矿构造地球化学特征 |
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| 引用本文： | 张寿庭,徐旃章.浙东南遂昌湖山萤石矿田成矿构造地球化学特征[J].矿物岩石,1998(Z1). |
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| 作者姓名： | 张寿庭 徐旃章 |
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| 作者单位： | 成都理工学院地质系 |
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| 摘 要： | 本文以浙东南遂昌湖山萤石矿田为例，对此类浅成低温热液矿床成矿构造地球化学特征，进行了初步研究与探讨；进一步揭示了萤石矿成矿物质组分的分配、迁移、分散、富集特征与控矿构造之间的内在联系。
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| 关 键 词： | 控矿断裂 构造地球化学 萤石矿成矿 遂昌湖山矿田 |
THE METALLOTECTONIC GEOCHEMICAL CHARACTERISTICS OF THE HUSHAN FLUORITE ORE FIELD,SUICHANG, SOUTHEAST ZHEJIANG |
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| Zhang Shouting,Xu Zhanzhang.THE METALLOTECTONIC GEOCHEMICAL CHARACTERISTICS OF THE HUSHAN FLUORITE ORE FIELD,SUICHANG, SOUTHEAST ZHEJIANG[J].Journal of Mineralogy and Petrology,1998(Z1). |
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| Authors: | Zhang Shouting Xu Zhanzhang |
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| Abstract: | Ore formation has an intimate relationship with fault structures.Study on tectonogeochemical characteristics of ore components has become one of the most popular topics of geoscientists.Taking the Suichang Hushan fluorite ore field as an example,the present paper mainly studies the tectonogeochemical characteristies of epithermal doposits of this kind,and further discusses the bearing of ore control faults on the distribution,transportation,dispersion and enrichment of fluorite ore components. |
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| Keywords: | ore control fault tectonogeochemistry fluorite ore formation the Suichang Hushan ore field |
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