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福建政和夏山铅锌矿微量元素特征及矿床成因
引用本文:郑开旗,周乐生.福建政和夏山铅锌矿微量元素特征及矿床成因[J].福州大学学报(自然科学版),1987(2):93-101.
作者姓名:郑开旗  周乐生
作者单位:福州大学地矿系 (郑开旗),福州大学地矿系(周乐生)
摘    要:本文主要论述:(1)方铅矿具有高含量的Ag、Bi、Se和高的Se/S比值;闪铲矿富含Cd、In、 Fe,贫Ga和Zn/Cd比值低的特点,黄铁矿中Co/Ni比值大于1:这些特点都与国内外热液、矽卡 岩型铅锌矿相似.(2)花岗斑岩中成矿元素丰度高,而且元素组合情况与矿石中元素组合极相似, 反映它们的成因联系.

关 键 词:矿床成因  微量元素  矽卡岩型  成矿元素丰度

The Characterics of Trace Elements and Genesis of Xiashan Pb-Zn Deposit, Zhenghe, Fujign
Zheng Kaiqi and Zhou Lesheng.The Characterics of Trace Elements and Genesis of Xiashan Pb-Zn Deposit, Zhenghe, Fujign[J].Journal of Fuzhou University(Natural Science Edition),1987(2):93-101.
Authors:Zheng Kaiqi and Zhou Lesheng
Institution:Department of Geology and Mining Engineering
Abstract:Hereof mentions are chiefly made that in Zhenghe there are high contents of Ag, Bi, Se and Se/S ratio in galena; high contents of Cd, In, Fe and low content of Ga and low Zn/Cd ratio in sphalerite; Co / Ni>1 in pyrite. The characteristics of the above are in consistence with those of hydrothermal type and skarn type Pb-Zn deposits at home and abroad. There are high contents of ore elements in the granite porphyry; and the elements assemblages have stri- king similarities with those of the ores. Thus a genetical relationship is sug- gested between the both above.
Keywords:trace elements  genesis of deposit  skarn type  
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