摘要
污牙白钨矿床位于江南地轴九万大山W、Sn、Cu、Au、Ag成矿带上,钨矿体产于花岗岩外接触带新元古界甲路组蚀变围岩中,围岩电气石化、黑云母化及深色蚀变与矿化关系密切。预测本矿区具有良好的找矿前景。
Wuya scheelite deposit is on Jiuwandashan W, Sn, Cu, Au, Ag metallogenetic zone of Jiangnan earth＇s axis. The ore body is in Neoproterozoic Jialu Formation altered wall rock of granite outer contact. The tour- malinization, biotitization, and deep color alteration of wall rock are related close to the metallogenesis. We prog- nosticate that there is the good prospecting potentiality in this orefield.
出处
《云南地质》
2015年第1期99-103,共5页
Yunnan Geology
关键词
白钨矿
控矿条件
找矿前景
贵州从江污牙
Scheelite Deposit
Ore Control Conditions
Prospecting Potentiality
Wuya, Guizhou
