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矿区位于中祁连地背斜东段龙王山复向斜西南翼,出露地层为中寒武统的中上部。已知有硫铁矿、钛铁矿、磁铁矿、胶磷矿、黄铜矿、石灰岩、白云岩等矿床矿(化)点。上述硫、磷、铜、钛的生成与海底火山喷发——沉积作用有关。现根据所掌握的资料,着重对硫铁矿床的地质特征及找矿方向提出一些看法。
The mining area is located in the southwestern wing of the Longwangshan synclinorium in the eastern anticline of the central Qilian, exposing the middle and upper part of the Middle Cambrian. Known pyrite, ilmenite, magnetite, phosphate rock, chalcopyrite, limestone, dolomite and other mineral deposits (points). The above sulfur, phosphorus, copper, titanium formation and submarine volcanic eruption - sedimentation effect. Now based on the available information, focusing on the geological characteristics of pyrite deposits and prospecting put forward some views.