摘要
尖山铁矿床产于下元古界尖山群袁家村组含铁岩系中，矿体受尖山向斜构造控制，同时断裂构造对矿亦有较大的影响，使主矿体向下延伸和错移。
Jianshan iron deposit was produced in ferruginous series of Yuanjiachun formation,Jianshan group, Proterozoic erathem. The orebody was control1ed by Jianshan synclinal structure and the fracturestructure effects on the orebody to extensive downward and concealed shift.
出处
《中国矿业》
1994年第S1期139-142,共4页
China Mining Magazine
关键词
向形构造
控制孔
德优盲矿体
复式紧密褶曲
基性火山岩
Synclinal structure,Control hole,Blind orebody,Refolded compact fold,Basementvolcanic rock
