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    兰坪盆地白秧坪铅锌铜银多金属矿床成矿流体及成矿物质来源

    王晓虎 侯增谦 宋玉财 王光辉 张洪瑞 张翀 庄天明 王哲 张天福

    王晓虎, 侯增谦, 宋玉财, 王光辉, 张洪瑞, 张翀, 庄天明, 王哲, 张天福, 2012. 兰坪盆地白秧坪铅锌铜银多金属矿床成矿流体及成矿物质来源. 地球科学, 37(5): 1015-1028. doi: 10.3799/dqkx.2012.109
    引用本文: 王晓虎, 侯增谦, 宋玉财, 王光辉, 张洪瑞, 张翀, 庄天明, 王哲, 张天福, 2012. 兰坪盆地白秧坪铅锌铜银多金属矿床成矿流体及成矿物质来源. 地球科学, 37(5): 1015-1028. doi: 10.3799/dqkx.2012.109
    WANG Xiao-hu, HOU Zeng-qian, SONG Yu-cai, WANG Guang-hui, ZHANG Hong-rui, ZHANG Chong, ZHUANG Tian-ming, WANG Zhe, ZHANG Tian-fu, 2012. Baiyangping Pb-Zn-Cu-Ag Polymetallic Deposit in Lanping Basin: A Discussion on Characteristics and Source of Ore-Forming Fluids and Source of Metallogenic Materials. Earth Science, 37(5): 1015-1028. doi: 10.3799/dqkx.2012.109
    Citation: WANG Xiao-hu, HOU Zeng-qian, SONG Yu-cai, WANG Guang-hui, ZHANG Hong-rui, ZHANG Chong, ZHUANG Tian-ming, WANG Zhe, ZHANG Tian-fu, 2012. Baiyangping Pb-Zn-Cu-Ag Polymetallic Deposit in Lanping Basin: A Discussion on Characteristics and Source of Ore-Forming Fluids and Source of Metallogenic Materials. Earth Science, 37(5): 1015-1028. doi: 10.3799/dqkx.2012.109

    兰坪盆地白秧坪铅锌铜银多金属矿床成矿流体及成矿物质来源

    doi: 10.3799/dqkx.2012.109
    基金项目: 

    中国地质科学院地质力学研究所基本科研业务费项目 DZLXJK201103

    国家自然科学基金项目 U09336051

    国家自然科学基金项目 41072071

    国家重点基础研究发展计划项目 2009CB421001

    国家重点基础研究发展计划项目 2009CB421008

    详细信息
      作者简介:

      王晓虎(1983-), 男, 博士, 助理研究员, 从事矿床学和矿田构造研究. E-mail: wangzykc@yeah.net

    • 中图分类号: P611;P618.4

    Baiyangping Pb-Zn-Cu-Ag Polymetallic Deposit in Lanping Basin: A Discussion on Characteristics and Source of Ore-Forming Fluids and Source of Metallogenic Materials

    • 摘要: 白秧坪矿床位于滇西北兰坪盆地北部, 是一沉积岩容矿的铅锌铜银多金属矿床, 矿体赋存于中生代地层中, 受断裂构造控制明显.通过成矿期方解石、石英、闪锌矿中流体包裹体研究, 以及方解石的C、O和含硫矿物的S、Pb同位素研究, 来探讨成矿流体性质及其来源和成矿物质来源.研究表明, 白秧坪矿床包裹体一般小于10 μm, 气液两相为主, 成矿流体体系为Ca2+-Na+—K+-Mg2+-Cl--F--NO3-卤水体系, 矿床矿物中冰点温度范围为-26.4~-0.2 ℃, 平均为-14.6 ℃, 均一温度集中于120~180 ℃, 盐度为0.35%~24.73%(NaCleq), 平均值16.9%(NaCleq), 成矿流体密度在0.84~1.11 g/cm3之间, 平均值1.04 g/cm3, 成矿压力为28.0~46.9 MPa, 平均37.6 MPa, 对应的成矿深度约1 058~2 452 m, 平均1 555 m, 集中于1 200~1 800 m; 碳质的来源较为均一, 矿石中热液方解石中碳源自地层中碳酸盐岩溶解, 成矿流体属于盆地流体系统, 有大气降水的加入; 成矿物质硫来自硫酸盐的热化学还原作用, 或者含硫有机质的热分解, 金属成矿物质来自沉积地层和盆地基底.

       

    • 图  1  白秧坪铅锌铜银多金属矿床矿区地质及矿体分布(据云南省地质调查院矿产调查所及宁夏有色金属地质勘查院修编①②)

      1.花开佐组下段一亚段;2.花开佐组下段二亚段;3.花开佐组上段;4.景星组下段一亚段;5.景星组下段二亚段下部;6.景星组下段二亚段上部;7.景星组下段二亚段;8.景星组下段三亚段;9.南星组下段;10.南星组上段;11.云龙组下段;12.云龙组上段;13.第四系;14.地层界线;15.断层;16矿体;17.采样点

      Fig.  1.  The geological map and distribution of ore bodies of Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      图  2  部分矿石野外产状及矿石照片

      a.呈脉状充填的细硫砷铅矿脉;b.脉状充填的闪锌矿、方解石脉

      Fig.  2.  The partial photos of ore

      图  3  白秧坪铅锌铜银多金属矿床流体包裹体显微照片

      Fig.  3.  Photomicrographs of fluid inclusions from Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      图  4  白秧坪铅锌铜银多金属矿床盐度与均一温度关系

      Fig.  4.  The homogenization temperature and salinity relation of Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      图  5  白秧坪铅锌铜银多金属矿床硫同位素组成

      Fig.  5.  S isotopic composition of Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      图  6  白秧坪铅锌铜银多金属矿床方解石氧同位素组成分布(底图据Hoefs,2009)

      Fig.  6.  δ18O values of calcite from Baiyangping Pb-Zn-Cu-Ag polymetallic deposit and important geological reservoirs

      图  7  白秧坪铅锌铜银多金属矿床方解石的C、O同位素值分布(底图据刘家军等,2004;略简化)

      Fig.  7.  C-O isotope of calcite in the Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      图  8  白秧坪铅锌铜银多金属矿床铅同位素Δβγ成因分类图解(底图据朱炳泉,1998)

      1.地幔源铅;2.上地壳铅;3.上地壳与地幔混合的俯冲带铅(3a岩浆作用,3b沉积作用);4.化学沉积型铅;5.海底热水作用铅;6.中深变质作用铅;7.深变质下地壳铅;8.造山带铅;9.古老页岩上地壳铅;10.退变质铅;Δβ=1 000×β/(βM-1),Δγ=1 000×γ/(γM-1),βγβMγM分别为样品和地幔的207Pb/204Pb和208Pb/204Pb;i.富隆厂矿段;ii.李子坪矿段;iii.吴底厂矿段;iv.白秧坪矿段;v.元古代变质岩、花岗岩;vi.寒武系片岩、白云岩;vii.二叠系凝灰岩、灰岩、玄武岩、角斑岩;viii.三叠系流纹岩、玄武岩;ix.三叠系灰岩;x.侏罗系砂岩;xi.白垩系砂岩;xii.第三系砂岩

      Fig.  8.  Δβγ genetic classification of lead isotope in Baiyangping Pb-Zn-Cu-Ag polymetallic deposits

      图  9  兰坪盆地白秧坪铅锌铜银多金属矿床Pb同位素组成与邻区地层全岩Pb同位素对比(地层岩石中Pb同位素数据陈式房等,1991; 王峰,2004)

      i.富隆厂矿段;ii.李子坪矿段;iii.吴底厂矿段;iv.白秧坪矿段;v.元古代变质岩、花岗岩;vi.寒武系片岩、白云岩;vii.二叠系凝灰岩、灰岩、玄武岩、角斑岩;viii.三叠系流纹岩、玄武岩;ix.三叠系灰岩;x.侏罗系砂岩;xi.白垩系砂岩;xii.第三系砂岩

      Fig.  9.  Comparison of Pb isotope composition of sulfides from Baiyangping Pb-Zn-Cu-Ag polymetallic deposit and whole-rock Pb isotope composition of strata from adjacent areas

      表  1  白秧坪铅锌银铜多金属矿床流体包裹体特征及参数

      Table  1.   Microthermometric data and characteristics of fluid inclusion in Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      序号 矿段 样品号 寄主矿物 包裹体特征 冰点温度(℃) 均一温度(℃) 盐度(NaCleq%) 密度ρ(g/cm3) 深度估算(m) 资料来源
      类型 大小(μm) 气液比估算(%)
      1 富隆厂 FLC054-2 石英 富液两相 4~10 5~10 -17.6~-5.6 137~214.6 8.7~20.67 0.975~1.02 1 780.4~2 272.0 实测
      2 富隆厂 FLC2-5 闪锌矿 富液两相 4~5 5 138~181.6 实测
      3 富隆厂 FLC2-8 闪锌矿 富液两相 10 5 -21 143.9 23.05 1.09 1 525.9 实测
      4 富隆厂 FLC2-21 闪锌矿 富液两相 5~7 5~10 -20.6~-9 118.2~138.2 12.85~22.78 1.025~1.11 1 253.2~1 463.6 实测
      5 富隆厂 FLC054-7 闪锌矿 富液两相 5~10 5 123~188.1 实测
      6 吴底厂 2WDC2-4 闪锌矿 富液两相 6~10 5~10 -20~-15.6 120~206.1 19.13~22.38 1.07~1.105 1 270.6~1 449.0 实测
      7 吴底厂 2WDC2-9 闪锌矿 富液两相 10~13 5 -21 130~134 23.05 1.1 1 420.9 实测
      8 吴底厂 LP08-43 闪锌矿 富液两相 8 5 -16.6 120 19.92 1.08 1 269.7 实测
      9 吴底厂 LP08-44 闪锌矿 富液两相 11~12 5~10 -20.8~-16.2 130~137 19.6~22.91 1.07~1.1 1 375.8~1 449.2 实测
      10 吴底厂 WDC022-1 闪锌矿 富液两相 7~8 5~10 -21.6~-16.9 100~138 20.15~22.38 1.08~1.105 1 058.3~1 461.7 实测
      11 吴底厂 WDC022-8 闪锌矿 富液两相 4~10 5~10 -20.5~-19 120~139 21.68~22.71 1.08~1.095 1 271.4~1 440.9 实测
      12 李子坪 LZP2-2 方解石 富液两相 5 10 -2.5 153.2 4.18 0.94 1531.2 实测
      13 李子坪 LZP2-2 闪锌矿 富液两相 5~20 5~10 -24~-20.1 130~167 22.44~24.02 1.07~1.11 1 379.0~1 771.6 实测
      14 李子坪 LZP2-3-1 方解石 富液两相 4~10 10~20 -5.5~-1.4 122~238 2.57~8.55 0.84~0.96 1 169.4~2 365.7 实测
      15 李子坪 LZP2-4 方解石 富液两相 7~8 5~10 -19.3~-2 129~153 3.39~21.89 0.945~1.07 1 363.8~1 621.2 实测
      16 李子坪 LZP2-6-1 方解石 富液两相 4~12 5~20 -19.1~-5.1 111~233 8~21.75 0.925~1.105 1 176.0~2 452.6 实测
      17 李子坪 LZP2-6-1 闪锌矿 富液两相 8~10 5~20 -24.5~-20 145~150 22.38~24.17 1.08~1.095 1 538.2~1 591.3 实测
      18 李子坪 LZP2-9-2 方解石 富液两相 20 10 -0.3 0.53 实测
      19 李子坪 LZP021-1 方解石 富液两相 6~17 5~20 -26.4~-5 143~189 7.86~24.73 0.93~1.1 1 517.5~1 977.9 实测
      20 李子坪 LZP021-2 闪锌矿 富液两相 9 10 -20.8 130 22.91 1.1 1 378.4 实测
      21 白秧坪 B29 重晶石 -0.2 179 0.35 0.9 1 103.0 曾荣,2007
      22 白秧坪 B29 方解石 -7.6~-2.1 165~238 曾荣,2007
      23 白秧坪 B28 天青石 -3.1~-0.9 183~284 曾荣,2007
      24 白秧坪 BYP29 方解石 -3.0~-0.9 122~181 曾荣,2007
      25 白秧坪 B33 天青石 -4.1~-0.8 123~258 曾荣,2007
      26 白秧坪 B20 方解石 -0.7 140 1.22 0.94 1206.4 曾荣,2007
      27 白秧坪 BYP 闪锌矿 105~155 杨伟光等,2003
      28 白秧坪 ss97066 石英脉 富液两相 -3.3 189 5.3 0.91 1917.1 徐启东和李建威,2003
      下载: 导出CSV

      表  2  流体包裹体气相液相成分分析结果(μg/g)

      Table  2.   Gas and liquid compositions of fluid inclusions from Baiyangping Pb-Zn-Cu-Ag polymetallic deposit

      样号 矿物名称 CH4 C2H2+C2H4 C2H6 CO2 H2O O2 N2 CO Li+
      LZP2-1 方解石 0.223 0.065 微量 167.509 195.102 5.316 33.188 0
      LZP2-6-1 方解石 0.356 0.082 微量 468.483 198.428 39.196 171.563 0
      FLC2-3-3 方解石 0.577 0.106 0.027 203.815 210.382 3.088 28.287 0.437
      WDC022-4 方解石 0.505 0.126 0.018 184.049 177.565 4.247 30.514 0.195
      FLC2-8 闪锌矿 0
      FLC2-21 闪锌矿 0
      LZP021-2 闪锌矿 0
      LZP2-6-1 闪锌矿 0
      2WDC2-7 闪锌矿 0
      2WDC2-15 闪锌矿 0
      WDC022-4 闪锌矿 0
      LP08-45 闪锌矿 0
      样号 矿物名称 Na+ K+ Mg2+ Ca2+ F- Cl- NO2- Br- NO3- SO42-
      LZP2-1 方解石 15.939 5.817 224.675 9.814 19.839 0 0.276 0.634
      LZP2-6-1 方解石 14.667 1.658 9.225 1.417 39.652 0 0.859 0.264
      FLC2-3-3 方解石 8.488 10.360 104.774 5.903 10.688 0 0.071 0.174
      WDC022-4 方解石 2.072 0.622 2.474 1.078 2.431 0 0 0.140
      FLC2-8 闪锌矿 14.447 6.385 4.941 28.253 0.244 5.226 0 0.153 0.254
      FLC2-21 闪锌矿 21.732 3.284 8.840 67.825 0.278 11.479 0 0 0.267
      LZP021-2 闪锌矿 7.485 1.180 1.498 24.699 0.251 4.983 0 0 0.115
      LZP2-6-1 闪锌矿 13.151 2.197 0.713 125.827 0.264 9.080 0 0 0.195
      2WDC2-7 闪锌矿 12.227 1.217 0 4.393 0.095 4.767 0 0 0.102
      2WDC2-15 闪锌矿 3.663 0.958 1.116 131.645 0.103 1.294 0 0 0.089
      WDC022-4 闪锌矿 7.459 1.504 0.561 25.270 0.160 6.550 0 0 0.488
      LP08-45 闪锌矿 8.569 3.642 1.737 12.580 0.200 7.569 0 0 0.768
      注:“—”表未检出.
      下载: 导出CSV
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