摘要
青龙沟金矿是辽西地区首次发现的产于元古代碳酸盐岩地层中的金矿,金成色高、品位富,其成矿类型比较特殊,属同生沉积加后期热液改造型,而辽西地区元古代碳酸盐岩地层分布范围广,找矿空间大,只要注意该种类型金矿的找矿与查定,就一定会有新的发现和突破。
First detected in the western Liaoning province, Qinglonggou the high purity and high grade gold ore which hosted in the proternozoic carbonate strata displied its special gentic type,the ore was syndeposited and evently reformed by hydrothermal fluid.The new gold ore will be found out and explored if enough attention is paid to this kind of deposits because of the wide range of proterozoic carbonate strata in the western Liaoning province.
出处
《有色矿冶》
2004年第5期1-3,共3页
Non-Ferrous Mining and Metallurgy
关键词
青龙沟
金矿
物质来源
同生沉积
变质改造
富集成矿
Qinglonggou
gold ore
matter origin
syndeposit
metamorphic reformation
concentration