槽Being the residual island are of the convergent plate subducted to the south, the central Baiyin Minerogenetic Belt is located at the southeast edge of the north Qilian Caledonian eugeosyncline.
摘要内蒙油房一二把伙
区位于华北台北缘南兴安晚华力西
槽褶皱带，中生代火
岩系发育，燕中
性岩浆活动强烈，形成了一系列火、潜火
型银多金属矿床。
