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双王金矿具有多期多阶段叠加成矿成晕的特点 ,该矿床可分为 4个阶段 ,不同成矿阶段的元素组合是 :Ⅰ (阶段 )—Au ,As,Sb ,Mn ,Ni;Ⅱ—Au,Ag ,As,Sb ,Bi,Mo ,Mn ,Ni;Ⅲ—Au ,As,Sb ,Hg ,Mn ,Ni;Ⅳ—Au ,Ag,As,Sb ,Hg ,B ,Bi,Mo,Mn ,Ni,其中Ⅰ、Ⅱ、Ⅲ阶段为主成矿阶段。单阶段形成的矿体 (晕 )的垂直分带序列是(从上→下 ) :Hg ,B ,Sb ,As→Ag ,As→Bi,Mn→Ni。不同成矿阶段形成矿体 (晕 )在空间上叠加特点是 :从上→下 ,Ⅰ阶段由弱→强 ,Ⅱ、Ⅳ阶段由强→弱。据上述特点建立了矿床的原生叠加晕模式。
The Shuangwang gold deposit has the characteristics of multi-period multi-stage superimposed mineralization into halo, and the deposit can be divided into four stages. The element combinations in different metallogenic stages are: Ⅰ (stage) -Au, As, Sb, Mn and Ni; Ni, Ag, As, Sb, Hg, B, Bi, Mo, Mn, Ni, of which Ⅰ, Ⅱ, Ⅲ stage is mainly metallogenic stage. The vertical zoning sequence of single-stage formation of ore bodies (halo) is (from top to bottom): Hg, B, Sb, As → Ag, As → Bi, Mn → Ni. The formation of ore bodies (halo) in different mineralization stages is characterized by spatial superposition: from the upper → lower, Ⅰ stage from weak → strong, Ⅱ, Ⅳ stage from strong to weak. According to the above characteristics, the deposit superposition dimming mode was established.