摘要
金红石在基性岩中是由于自变质作用和后期热液作用的结果,使矿体中金红石加富,该区矿床属岩浆矿床。介绍了代县碾子沟矿区金红石矿产的地质特征,就代县碾子沟矿区金红石矿的成矿原因进行了分析。
In the radicel rock, ruffle＇ s formation is due to the metamorphism and the function of hydrotherm making the ruffle rich in the orebody, and this deposit belongs to magmatic deposit, Introduce the geological features of ruffle mineral in Nianzigou, Dai county, and analyze the reason of the rutile＇s formation in this mining area.
出处
《太原科技》
2007年第10期75-76,共2页
Taiyuan Science and Technology
关键词
代县碾子沟
金红石
成因
Nianzigou, Dai county
rutile
the reason of formation
