Abstract：Dagougu gold deposit,occurring majorly in the albitite belt of Sinian Lechangxia group,is a new type of deposit related to albitite.The study on the geochemistry,trace elements and REE of the Au-rich albitite shows that the albitite has no genetical relation to the schist of Lechangxia group and nearby granite.The Au-rich albitite was formed mainly by hydrothermal sedimentation.The albitite is closely related to gold deposit.The genesis of the albitite-type gold deposit is hydrothermal sedimentation + reformation.
梁华英, 王秀璋, 程景平, 张湖. 大沟谷钠长石岩及金矿床形成分析[J]. 地质与资源, 1997, 6(4): 255-260,287.
Liang Huaying, Wang Xiuzhang, Cheng Jingping, Zhang Hu. STUDY ON THE FORMING OF ALBITITE AND GOLD DEPOSIT IN DAGOUGU, WESTERN GUANGDONG. GEOLOGY AND RESOURCES, 1997, 6(4): 255-260,287.
1997, Vol. 6 
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