山东牟平邓格庄金矿的叠加晕模式  

THE MODEL OF SUPERIMPOSED HALOS IN DENGGEZHUANG GOLD DEPOSIT, MUPING, SHANDONG

作　　者：李惠 刘振昌 张文华 刘宝林 耿仙湖 

机构地区：[1]冶金地球物理勘查院物化探研究所,河北保定071051 [2]山东乳山金矿,山东乳山264500

出　　处：《黄金地质》1999年第3期58-63,共6页Gold Geology

基　　金：国家攀登计划项目

摘　　要：邓格庄金矿为一大型石英脉型金矿，具有多期多阶段叠加成矿成晕的特点，根据不同成矿阶段形成的矿体（晕） 及包裹体气晕、离子晕在空间上的叠加结构， 建立了矿床的原生叠加晕模式， 确定了判断矿床剥蚀程度的标志。Denggezhuang gold deposit is a large quartz vein type. It has features of superimposed mineralization and halo of multiphase and multistage. According to the spacial superimposed structure of orebody (halo), inclusion vapor halo and ion halo in different mineralizing stages, the model of original superimposed halo in the deposit has been established and the discriminant mark of deposit denude has been defined.

关 键 词：金矿床 叠加晕模式 山东 成矿阶段 

分 类 号：P618.510.4[天文地球—矿床学] P618.510.5[天文地球—地质学]