摘要
武夷山稀有、贵金属矿带受 NE向构造岩浆岩带控制。稀有金属成矿的时空分布上显示出从早到晚期由南侧伟晶岩型往北部钠长石化花岗岩型的变化趋势 ,贵金属成矿由银 (金 )
Wuyishan rare and precious metal ore belt is controlled by NE trend tectonic-magmatite belt.The time space distribution of rare metal mineralization shows a trend of changing from pegmatite type of early period on west side to albitization altered granite type toward north part in later period.The precious metal mineralization evolved from Silver (Gold) to Gold and Silver mineralization.
出处
《矿产与地质》
2001年第z1期434-439,共6页
Mineral Resources and Geology
关键词
构造
岩浆岩
稀有贵金属
矿化类型
武夷山
Structure
Magmatite
Rare and Precious metal
Mineralization type
Wuyishan
