黑龙江太平南山一带地质特征及矿床开采地质条件评价

Geological Characteristics And Geological Conditions Of Mining Deposits In Nanshan Area Of Taiping,Heilongjiang

区域处于西伯利亚板块东南海西大陆边缘,大地构造位置属大兴安岭早古生代陆源增生构造带,断裂构造发育,对地层、岩矿体的形成、分布及成矿有一定控制作用。区域内地层、断裂构造较发育,岩浆岩出露范围较广,属地质环境质量良好的矿床。

The region is situated on the southeastern margin of the Hercynian continental margin of the Siberian plate. The geotectonic location belongs to the Early Paleozoic terrigenous accretion structural belt in the Greater Hinggan Mountains. The faulted structure is well developed, which controls the formation, distribution and mineralization of strata, rocks and ore bodies. In the region, strata and faults are well developed, and magmatic rocks are widely exposed, which belongs to deposits with good geological environment.