摘要
大阳岔金矿床产于太古界龙岗群高级变质岩系中的石英脉型金矿床， 金矿化与黄铁绢英岩化关系密切， 本文着重论述了矿床的矿体、矿化及矿石特征， 进而探讨了该矿床的形成机理。
The Dayangcha quartz vien type gold deposit occurs in the Archaeozoic Longgang Group highgrade rock series, the gold metallization has a close relation to beresitization, in this paper, the ore body, metallization ore characteristics, and formation mechanism of the Dayangcha gold deposit are discussed emphatically.
出处
《吉林地质》
1999年第3期54-60,共7页
Jilin Geology
