摘要
通过对胶东邓格庄金矿深部 (- 2 2 5m～ - 345m)进行地球化学原生晕研究 ,结果表明Ⅰ2号脉的原生晕具有正向分带的特征 ,Ⅱ号脉的原生晕呈反向分带。据此推测在 - 345m以下地段Ⅰ2 号矿体延伸不大 ,而Ⅱ号脉在 -
This paper Studied deep-seated (-225 m～-345 m) geochemistry primary halo for Denggezhuang gold deposit, Jiaodong of China. It is showed that the primary halo of Ⅰ 2 vein has characteristics of axial zonality sequence and that Ⅱ vein has characteristics of reversed axial zonality. Therefor, authors consider that underlying port of Ⅰ 2 body is not deep in -345 m level and of Ⅱ body was superposed by a blind ore-body in deep-seated.
出处
《地质与勘探》
CAS
CSCD
北大核心
2001年第1期27-29,37,共4页
Geology and Exploration
基金
中国科学院创新工程项目!(KZCX1-Y -0 3)
"九五"重大黄金项目!(KZ95 1-A1-4 0 4-0 2 )
牟平金矿联合资助
