滇东富乐铅锌矿区及外围闪锌矿流体包裹体特征
发布时间：2018-07-25 07:49
【摘要】：云南罗平富乐铅锌矿是川滇黔铅锌成矿域内赋矿层位最新的大型铅锌矿床,成矿流体研究薄弱,铅锌成矿作用过程的认识缺少实际地球化学依据。对该矿床及邻近矿点中闪锌矿流体包裹体的研究表明,该区矿床(点)闪锌矿中流体包裹体以气液相包裹体为主,其次为含子矿物多相包裹体,显微测温获得闪锌矿流体包裹体均一温度主要分布在120~160℃和180~210℃两个区间,盐度分布在4%~10%和16%~22%两个区间,矿区存在低温和中温两类成矿流体,该类流体属于少量油田水混入的Na~+-Mg~(2+)-SO_4~(2-)-Cl~-型流体,结合富乐矿区矿体及矿石组构特征分析,该区成矿流体具有低温和中温流体混合特征,在成矿流体混合部位形成富厚矿体。该成果为认识该区铅锌成矿作用提供了新的地球化学证据。
[Abstract]:The Luo Ping Fule lead-zinc deposit in Yunnan Province is the latest large-scale lead-zinc deposit in the lead-zinc metallogenic region of Sichuan Yunnan and Guizhou Province. The study of ore-forming fluids is weak and the understanding of the process of lead-zinc mineralization is lack of practical geochemical basis. The study of sphalerite fluid inclusions in the ore deposit and adjacent ore points shows that the fluid inclusions in the sphalerite are mainly gas-liquid inclusions, followed by the multi-phase inclusions of sub-bearing minerals. The results of microthermometry show that the homogenization temperature of sphalerite fluid inclusions is mainly distributed between 120 ~ 160 鈩，
本文编号：2143130
[Abstract]:The Luo Ping Fule lead-zinc deposit in Yunnan Province is the latest large-scale lead-zinc deposit in the lead-zinc metallogenic region of Sichuan Yunnan and Guizhou Province. The study of ore-forming fluids is weak and the understanding of the process of lead-zinc mineralization is lack of practical geochemical basis. The study of sphalerite fluid inclusions in the ore deposit and adjacent ore points shows that the fluid inclusions in the sphalerite are mainly gas-liquid inclusions, followed by the multi-phase inclusions of sub-bearing minerals. The results of microthermometry show that the homogenization temperature of sphalerite fluid inclusions is mainly distributed between 120 ~ 160 鈩，
本文编号：2143130
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