摘要
白云金矿床位于青城子矿田外围,产出于白云推覆构造带中,围岩主要为辽河群盖县组的矽线石云母片岩和黑云母变粒岩。主要矿化类型为硅钾蚀变岩型。
Baiyun gold ore deposit is located at the periphery of Qingchengzi mine field, occurring in Baiyun nappe structure belt, the wall rock is mainly the sillimanite mica schist and biotite of Liaohe groap Gaixian formation. The main mineralization category is silicon--potassium altered rock category.
出处
《有色矿冶》
2009年第3期4-7,共4页
Non-Ferrous Mining and Metallurgy
关键词
推覆构造
硅钾蚀变岩
矿床特征
成因探讨
nappe structure , silicon--potassium altered rock , deposit feature , discussion of the genesis
