摘要
“三江成矿带”内的红牛铜矿,赋存于大理岩边部矽卡岩化蚀变带及角岩体中。赋矿地层为曲嘎寺组第二段。对矿石结构、构造及矿石矿物成分、共生伴生关系等进行研究,明确找矿标志。
The Hongniu Cu deposit in ＂Sanjiang Metallogenetic Zone＂ is occurred in the skarnization alteration zone in the margin of marble and the hornfels body. The second member of Qugasi Formation is the ore -bearing strata. The ore -prospecting marks are determined according to the study on texture, structure, mineralogical composition and paragenesis of ore.
出处
《云南地质》
2006年第1期12-18,共7页
Yunnan Geology
关键词
矽卡岩铜矿
共生伴生
角岩化
找矿标志
香格里拉
云南
Skarn Cu Deposit
Paragenesis
Hornfelsization
Ore Prospecting Marks
Shangle-ra, Yunnan
