山羊坪铁矿地质特征及成因探讨

Geological Features and Mineralization Genesis of the Shanyangping Iron Mine

山西代县山羊坪铁矿矿床成因类型属海底火山喷发—沉积—区域变质成因的受变质硅铁建造型铁矿床,即鞍山式铁矿床。赋存于台怀亚群柏枝岩组地层中,矿体严格受地层层位及复向斜的控制,为找矿提供标志。

Shanyangping Iron Mine mineral bed become to belong to a sea volcano eruption because of the type-deposition-the district change in character because of being subjected to and change in character the Huo iron construct an iron mine bed,namely the saddle mountain type iron mine bed.Endow with to save a second cluster a cypress a rock set geologic strata at the set bosom in,the mineral body is strict to be subjected to a geologic strata layer and reply syncline of control,for seek a mineral to provide marking.