新疆红山顶锑矿床地质特征及成因研究

Geological characteristics and genesis of Hongshan Ding antimony deposit in Xinjiang

红山顶锑矿床大地构造位置属巴颜喀拉晚古生代-中生代边缘裂陷盆地。区内出露地层主要为黄羊岭群,区内断裂构造发育。锑矿赋存于硅化蚀变的石英砾岩中。

The Hongshanding antimony deposit is located in the Late Paleozoic-Mesozoic marginal rift basin of Bayanhara.The main strata in the area are the Huang Yang Ling group,and the fault structures are developed in the area.Antimony deposits occur in silicified altered quartz conglomerates.The genetic type of the deposit is post-magmatic low-temperature hydrothermal filling stratabound deposit occurring in clastic rocks.