• 责任者：Qian Zhikuan (State Key Laboratory of Ore Deposit Geochemistry ; Chinese Academy of Sciences ; Guiyang 550002 ; China) ; Wu Junde
• 刊名：Acta Mineralogica Sinica
• 出版年：2011
• 卷期：31(3)
• 关键词：锡矿 ; tin ores ; 赤铁矿 ; hematite ; 方解石 ; calcite ; 云南 ; Yunnan Province
• 页码：p.328-337
• 图表：6 illus., 47 refs.
• 分类号：1001
• 出版序号：472
• issnNo：ISSN1000-4734
• isbnNo：CN52-1045/P

///Cassiterite-hematite-calcite vein-type orebody was found in Songshujiao mining area of Gejiu Tin-deposit, and was reported in this paper. Preliminary study shows that the vein-type orebody is the result of the late ore-forming fluid condensated in the transport channel. The paper also preliminary discussed the cause of its genesis. According to the comparison between the Gejiu tin-polymetallic deposits and the Red Sea-type hydrothermal deposits, we believe that there are two models for the “Interstratified oxidized ore” of the Gejiu and the Red Sea-type orebodies; one is thermal brine staged oxidize from the top down, and another is ore-forming fluid oxidized from the bottom up gradually.