• 责任者：Zhang Hanbin (College of Resources and Environment Engineering ; Guizhou University ; Guiyang 550003 ; China) ; Deng Xusheng
• 刊名：Guizhou Geology
• 出版年：2013
• 卷期：30(4)
• 关键词：磷矿床 ; phosphate deposit ; 构造控制 ; structural controls ; 贵州 ; Guizhou Province
• 页码：p.262-265,301
• 图表：2 illus., 7 refs.
• 分类号：1002
• issnNo：ISSN1000-5943
• isbnNo：CN52-1059/P

     Qingshuijiang phosphorite deposit in Kaiyang occurs in phosphorite-bearing rock ot Y angsnm formation, Lower Sinian. By analysis the fracture and structure in the mining area, it＇ s thought the phosphorite is influenced and controlled by 3 NNW fauhs, the structural form is NE SW thrust fracture associa- tion. The main phosphorite-bearing layers are the same, ＇ triple layers＇ ore is formed by trust fault.