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胶东绿岩型金矿地质地球化学特征
引用本文:李洪志, 吴悦斌. 胶东绿岩型金矿地质地球化学特征[J]. 地质与资源, 1995, 4(4): 241-246.
作者姓名:李洪志  吴悦斌
作者单位:1.中国矿业大学北京研究生部;; 2.中国地质大学·北京
摘    要:胶东绿岩型金矿分布在绿岩带中,容矿围岩为斜长角闪岩、黑云变粒岩等。控矿构造为NWW向脆韧性断裂带,带内岩石含金平均高达58.8×10-9;成矿元素Au、Ag、As、Pb、Cu、Bi等的含量在矿体上下和蚀变带中呈有规律变化,Bi可作为近矿指示元素。硫同位素特征表明矿体与绿岩有成分上的继承关系;氢氧同位素组成反映成矿热液属变质成因。

关 键 词:绿岩型金矿   地质地球化学特征   胶东地区

THE GEOCHEMICAL CHARACTERISTIC OF GOLD DESPOSITS IN JIAODONG GREENSTONE BELT
Li Hongzhi, Wu Yuebin. THE GEOCHEMICAL CHARACTERISTIC OF GOLD DESPOSITS IN JIAODONG GREENSTONE BELT[J]. Geology and Resources, 1995, 4(4): 241-246.
Authors:Li Hongzhi  Wu Yuebin
Affiliation:1.Beijing Gradnate School China University of Mining and Technology;; 2.China University of Geosciences, Beijing
Abstract:This paper discussed the general geologic characteristic of gold desposits in Jiao Donggreenstone belt at first,such as the control structure,the altcration of adjoin rock ancd soon. After that the ore-forming fluid composition and phisycal-chemical condations is anal-ysised by using trace element and isotope.
Keywords:gold desposits in greenstone belt characteristics of geochemistry Jiaodong district  
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