摘要
通过对常福龙金矿区地质特征及矿床地质特征的分析,指出常福龙金矿属构造作用下的低温热液型矿床,其控矿构造为北东向断裂带,容矿构造为由断裂派生的次级菱形格架构造。
Through the analysis on the geological characteristics of Changfulong Gold Field and the geological characteristics of the deposit, this paper points out that Changfulong Gold deposit is the exothermal-epithermal deposit under the tectonization, its ore-controlling structure is northwestern fault zone, and its ore-hosting structure is secondary diamond-shaped grillage structure derived by the fracture.
出处
《科技情报开发与经济》
2010年第19期178-180,共3页
Sci-Tech Information Development & Economy
关键词
常福龙金矿区
构造条件
矿床成因
Changfulong Gold Field
structural environment
metallogenesis
