摘要
泥堡金矿及水银洞金矿是大型金矿床,两矿床赋矿地层、容矿岩石、矿体产出特征、金的赋存状态等诸多特征相似;并处于富金的峨眉山玄武岩东侧,其矿床成因与该玄武岩有密切关系。应加强从泥堡—戈塘—紫木凼—水银洞一线地层中P3l的研究,指导金矿找矿及勘查工作。
Nipu gold deposit is a good-sized deposit as Shuiyindong gold deposit. In Comparison between two deposits, there exist great similarities in terms of host strata, host rocks, orebody occurrence and gold attitude emerged, in addition both in east of Emeishan basalt. The studies focused on the P 3l stratum of the belts along Nipu Getang Zimudang Shuiyindong can guide the works of prospecting and exploration of gold deposits.
出处
《贵州地质》
2005年第1期22-25,共4页
Guizhou Geology
基金
中国科学院贵阳地球化学研究所矿床地球化学重点实验室资助
关键词
泥堡金矿
水银洞金矿
地质特征
峨眉山玄武岩
Nipu gold deposit
Shuiyindong gold deposit
geological characters
Emeishan basalt
