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通过主要剖面、平面、长纵剖面矿化元素的空间分布、矿石多元素相关分析得出 :Cu、Sn矿化既有关、又有分离 ,二者并非总是同时空富集 ,存在独立的锡矿体和铜矿体 ;总体上Sn矿化与Cu -Ag矿化关系密切、局部与Zn矿化有关 ;Ag矿化与Cu矿化、Pb -Zn矿化均有关 ;Cu与Pb、Zn的相关性差 ,空间上经常分离。从NWW到SEE矿化元素存在Ag -Cu -Sn -Pb -Zn混合矿化→Cu -Sn -Ag矿化→Pb -Zn -Ag矿化的纵向分布。成矿地球化学阶段可划分为 :Sn +As+Co、Cu +Sn +Ag±Au±Co、弱Ag +Cu±Au、Zn +Pb +Ag±Cu四个阶段。推断NE向断裂F2 -1及F2 可能是导矿构造。F1可能是另一个类似于F2 -1的导矿构造。
According to the spatial distribution of mineralized elements in the main section, the plane and the long longitudinal section, the multi-element ore-element correlation analysis shows that the mineralization of Cu and Sn are both relevant and separate, and the two are not always empty and enriched simultaneously. Ore body and copper ore body. Generally, Sn mineralization is closely related to Cu-Ag mineralization and locally related to Zn mineralization; Ag mineralization is related to Cu mineralization and Pb-Zn mineralization; Cu and Pb, Zn Poor correlation, often separated in space. The mineralization elements from NWW to SEE exist the longitudinal distribution of Ag-Cu-Sn-Pb-Zn mixed mineralization → Cu-Sn-Ag mineralization → Pb-Zn-Ag mineralization. The stages of metallogenetic geochemistry can be divided into four phases: Sn + As + Co, Cu + Sn + Ag ± Au ± Co, Ag + Cu ± Au, Zn + Pb + Ag ± Cu. It is inferred that the NE-trending F2-1 and F2 may be ore-bearing structures. F1 may be another similar to F2 -1 guide structure.