摘要
牟平邓格庄金矿为一富黄铁矿石英脉型金矿床,其Ⅱ号矿体金品位及其厚度数据处理表明矿体具有向北侧 伏的规律.Ⅱ号矿体深部(-225~-345 m)地球化学原生晕研究表明,其原生晕呈反向分带.据上述研究推测Ⅱ 号矿体-345
Denggezhuang gold deposit is of quartz vein type enriched pyrite. Data of gold tenors and thickness of No. II ore body of the deposit are processed. The result shows that the ore body has a trend plunging northeast. Study on deep (- 225 ~ - 345 m) geochemical primary halo of the deposit indicates a reverse zoning of primary halo. All the information above suggests that there still exist blind ore bodies under - 345 m levle of No. II ore body.
出处
《地质与资源》
CAS
2001年第2期80-84,共5页
Geology and Resources
基金
中国科学院创新工程项目(KZCX1-Y-03-01)
重大项目和牟平金矿联合资助.