湖北蕲春位于秦岭褶皱系桐柏-大别中间隆起浠水褶皱束东段,区内出露花岗岩的岩性以燕山期黑云二长花岗岩为主,构造发育,可见数条北西向、北东向和近南北向脆性断层,围岩蚀变类型主要有硅化、黄铁矿化、钾化、绢云母化及碳酸盐化,钼矿化与硅化、钾化和黄铁矿化密切相关。蚀变强度越强烈的地方矿化程度越强,反之则越弱。 Hubei Hunchun is located in the Qinling fold belt Tongbai - Dabie uplift Xishui fold beam eastern section of the region exposed granite lithology Yanshanian biotite monzogranite mainly tectonic development, we can see a number of northwest, north In the east and near north-south brittle faults, the types of wall rock alteration are mainly silicification, pyrite, potash, sericitization and carbonate, and molybdenum mineralization is closely related to silicification, potassiumization and pyrite mineralization . The stronger the alteration intensity is, the stronger the mineralization is, and the weaker the other is.