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新疆阿克提什坎金矿床稀土元素地球化学研究
引用本文:袁峰,周涛发,岳书仓.新疆阿克提什坎金矿床稀土元素地球化学研究[J].中国稀土学报,2002,20(4):357-361.
作者姓名:袁峰  周涛发  岳书仓
作者单位:合肥工业大学资源与环境科学系,安徽,合肥,230009
基金项目:“九五”国家科技攻关项目 (96 915 0 2 0 4,新疆 3 0 5 )
摘    要:研究了新疆阿尔泰特地区阿克提什坎金矿床的稀土元素及矿区二长花岗岩平衡的热液中稀土元素的组成特征及配分模型,并应用Grang等位线方法讨论了热液蚀变作用过程中稀土元素的行为。研究表明,在热液蚀变作用过程中,稀土元素保持惰性,成矿热液与岩浆热液关系不大,成矿物质主要来源于围岩。

关 键 词:阿克提什坎金矿床  稀土元素  地球化学  等位线  成矿物质  地质特征  热液蚀变过程
文章编号:1000-4343(2002)04-0357-05
修稿时间:2001年8月24日

Geochemistry of Rare Earth Elements in Aktishikan Gold Deposit, Xinjiang
Yuan Feng ,Zhou Taofa,Yue Shucang.Geochemistry of Rare Earth Elements in Aktishikan Gold Deposit, Xinjiang[J].Journal of the Chinese Rare Earth Society,2002,20(4):357-361.
Authors:Yuan Feng  Zhou Taofa  Yue Shucang
Institution:Yuan Feng *,Zhou Taofa,Yue Shucang
Abstract:The characteristics and the models of rare earth elements in the geological bodies and the hydrothermal water balanced with the adamellite were comprehensively studied in Aktishikan gold deposit, Nurt area of Altay, Xinjiang. And the behavior of rare earth elements during metasomatic alteration was discussed by using the isocon method of Grant. The results show that the rare earth elements are inert during metasomatic alteration, the hydrothermal water has no relation to the magmatic water, and the gold material sources mainly stem from the wall rock.
Keywords:rare earths  geochemistry  isocon diagram  gold deposit  Aktishikan
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