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    大兴安岭岔路口斑岩钼矿床流体成分及成矿意义

    熊索菲 何谋惷 姚书振 崔玉宝 胡新露 陈斌

    熊索菲, 何谋惷, 姚书振, 崔玉宝, 胡新露, 陈斌, 2014. 大兴安岭岔路口斑岩钼矿床流体成分及成矿意义. 地球科学, 39(7): 820-836. doi: 10.3799/dqkx.2014.077
    引用本文: 熊索菲, 何谋惷, 姚书振, 崔玉宝, 胡新露, 陈斌, 2014. 大兴安岭岔路口斑岩钼矿床流体成分及成矿意义. 地球科学, 39(7): 820-836. doi: 10.3799/dqkx.2014.077
    Xiong Suofei, He Mouchun, Yao Shuzhen, Cui Yubao, Hu Xinlu, Chen Bin, 2014. Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis. Earth Science, 39(7): 820-836. doi: 10.3799/dqkx.2014.077
    Citation: Xiong Suofei, He Mouchun, Yao Shuzhen, Cui Yubao, Hu Xinlu, Chen Bin, 2014. Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis. Earth Science, 39(7): 820-836. doi: 10.3799/dqkx.2014.077

    大兴安岭岔路口斑岩钼矿床流体成分及成矿意义

    doi: 10.3799/dqkx.2014.077
    基金项目: 

    黑龙江省国土资源厅“大兴安岭北段典型矿床剖析及成矿模式”专题研究 2012024045

    详细信息
      作者简介:

      熊索菲(1986-),女,博士生,矿物学、岩石学、矿床学专业.E-mail: sophie_0913@foxmail.com

      通讯作者:

      何谋惷, E-mail: hemch@126.com

    • 中图分类号: P588.12;P595;P597

    Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis

    • 摘要: 岔路口超大型斑岩型钼矿床位于大兴安岭北段,以网脉状和角砾岩型矿化为主.该矿床经历了4个成矿阶段:Ⅰ.石英-钾长石;Ⅱ.石英-辉钼矿;Ⅲ.石英-多金属硫化物;Ⅳ.石英-萤石-方解石.包裹体的岩相学及激光拉曼研究揭示,石英斑晶内的熔体-流体包裹体中熔体成分有更长石和钠长石,为岩浆出溶作用形成;子矿物多相包裹体(S型)中含有钾盐、石盐、赤铁矿和石膏等子矿物,显示出成矿流体为高氧逸度.第Ⅰ成矿阶段包裹体有气液两相(L+V型)、富CO2三相(C型)和含石盐、钾盐、赤铁矿及硬石膏等子矿物的多相(S型)等类型,第Ⅱ成矿阶段除了有L+V型、C型以及含钾盐、石盐、黄铜矿和辉钼矿等子矿物多相(S型)外,还可以见到S型包裹体与气相包裹体(V型)共存;第Ⅲ成矿阶段以L+V型和含方解石的S型包裹体为主;第Ⅳ成矿阶段除见到L+V型包裹体外,还可以见到液相包裹体(L型).显微测温结果显示从早到晚,流体包裹体均一温度从530 ℃变为120 ℃、盐度从66.7% NaCl equiv变为1.2% NaCl equiv,呈现逐渐降低的趋势.群体包裹体成分显示各阶段均含有气相CO2,液相成分中Na+,K+,Ca2+,SO42-,Cl-含量很高,而F-含量极少.成矿流体总体属于富含CO2的高盐度、高氧逸度的NaCl-H2O-CO2体系,在流体演化过程中温度、氧逸度、盐度和CO2含量逐渐降低.温度、盐度、CO2含量逐渐降低及绢云母化影响了矿石沉淀.

       

    • 图  1  大兴安岭北段区域地质简图(a)及大地构造位置(b)

      1.第四系;2.光华组;3.大网子组;4.吉祥沟组;5.粗安岩;6.碱长花岗岩;7.花岗斑岩;8.中粒花岗闪长岩;9.二长花岗岩;10.花岗闪长岩;11.不整合接触;12.断层及代号;13.推测火山机构;14.矿床;15.矿化点;F1.额尔古纳断裂;F2.得尔布干深断裂;F3.大兴安岭主脊-林西深断裂;F4.头道桥-鄂伦春深断裂;F5.查干敖包-五叉沟深断裂;F6.贺根山-新开岭深断裂;F7.嫩江-林西深断裂;Fg.多布库尔河大断裂;Fg1.多布库尔河次级断裂

      Fig.  1.  Tectonic location map(a) and regional geological map (b) of the northern great Xing'an range

      图  2  岔路口钼矿床矿床地质图(河东区)

      1.第四系;2.光华组;3.大网子组;4.黑云母二长花岗岩;5.粗安岩;6.大理岩;7.隐爆角砾岩;8.钼矿(化)体;9.构造角砾;10.不整合接触;11.蚀变界线;12.勘探线及编号

      Fig.  2.  Geological map of the Chalukou porphyry Mo deposit

      图  3  不同阶段脉的穿插关系

      a.石英脉(Ⅰ)被石英-辉钼矿脉(Ⅱ)切割,而石英-萤石-方解石脉(Ⅳ)切断石英-辉钼矿脉(Ⅱ);b.石英-多金属硫化物脉(Ⅲ)穿插石英-辉钼矿脉(Ⅱ);c.石英-多金属硫化物脉(Ⅲ)被石英-萤石-方解石脉(Ⅳ)切断;Qz=石英;Clc=-方解石;Mo=钼;Fl=荧石;Q-Mo=石英-辉钼矿脉;Q-PM=石英-多金属硫化物脉;Q-Clc-F=石英-方解石脉-萤石

      Fig.  3.  Photographs showing interpenetration of Four-stage veins

      图  4  岔路口矿床流体包裹体特征

      Hem.赤铁矿,H.石盐,Syl.钾盐,Mo.辉钼矿,Cal.方解石;a.石英斑晶中熔体-流体包裹体;b.第Ⅰ阶段赤铁矿子矿物的S型包裹体;c.第Ⅰ阶段含石盐的S型包裹体;d.第Ⅰ阶段含CO2三相包裹体;e.第Ⅱ阶段含钾盐的S型包裹体;f.第Ⅱ阶段V型包裹体和S型含石盐包裹体共生;g.第Ⅱ阶段含石盐和辉钼矿的S型包裹体;h.第Ⅲ阶段含方解石的S型包裹体;i.第Ⅲ阶段V+L型包裹体;j.第Ⅳ阶段L型包裹体

      Fig.  4.  Photomicrographs of fluid inclusions in the Chalukou Deposit

      图  5  岔路口各阶段流体包裹体均一温度直方图(a)和盐度直方图(b)

      Fig.  5.  Histograms of microthermometric data (a) and salinity for mainly stages (b) in the Chalukou porphyry Mo deposit

      图  6  岔路口矿床成矿阶段均一温度-盐度关系(据Wilkinson, 2001)

      Fig.  6.  Homogenization temperature-salinity diagram between different stages in the Chalukou Porphyry Mo deposit

      图  7  花岗斑岩的石英斑晶内流体包裹体主要激光拉曼图谱

      a.熔体-流体包裹体中钠长石谱图;b.熔体-流体包裹体中更长石谱图;c.S型包裹体的石膏谱图;d.S型包裹体中子晶赤铁矿谱图;e.L+V型包裹体中H2O谱图;f.L+V型包裹体中气相CO2谱图; 箭头所指部位为激光拉曼测试点

      Fig.  7.  Raman spectra of fluid inclusions (melt-fluid inclusions) in granite porphyry

      图  8  主成矿阶段的流体包裹体激光拉曼图谱

      a.第Ⅰ成矿阶段S型包裹体中硬石膏子矿物谱图;b.第Ⅰ成矿阶段S型包裹体中赤铁矿子矿物谱图;c.第Ⅱ成矿阶段S型包裹体的辉钼矿子矿物谱图;d.第Ⅰ成矿阶段C型包裹体中气相CO2谱图;e.第Ⅱ成矿阶段S型包裹体的黄铜矿子矿物谱图;f.第Ⅲ阶段S型包裹体中方解石子矿物谱图;箭头所指部位为激光拉曼测试点

      Fig.  8.  Raman spectra of fluid inclusions in the mainly stage

      图  9  主成矿阶段群体包裹体成分变化趋势

      Fig.  9.  The change of Aqueous and Gaseous contents of fluid inclusions in the mainly stage

      表  1  岔路口钼矿床的流体包裹体特征及显微测温结果

      Table  1.   The characteristics of fluid inclusions and microthermal measurement in Chalukou Porphyry deposit

      包裹体类型 形态和大小 冰点(℃) CO2笼形化合物熔化温度(℃) CO2部分均一温度(℃) 完全均一温度(℃) 子晶熔化温度(℃) 盐度(% NaCl equiv) 分布情况及特征
      M型 熔体-流体包裹体 不规则和负晶型为主一般8~15 μm 升至500 ℃测均一温度,熔体-流体包裹体无显著变化 在花岗斑岩的石英斑晶中较为发育,包裹体中可见到明显的熔体相存在,无晶形,但其消光位与主矿物石英存在差异
      V型 气相包裹体 负晶型、椭圆形为主,大小一般小于10 μm -8.9~-1.2 302~530 2.1~12.7 在石英斑晶中及第Ⅱ成矿阶段出现较多
      L+V型 富气相的气液两相包裹体 不规则和负晶型为主,一般3~15 μm -8.9~-1.2 302~530 2.1~12.7 最主要的包裹体类型,第Ⅰ、Ⅱ、Ⅲ和Ⅳ阶段均有分布,主要呈群状、带状或线状产出,少数呈孤立状产出
      富气相的气液两相包裹体 椭圆形、不规则和负晶型为主,一般4~20 μm -13.1~-0.3 121~474 0.5~17.0
      L型 液相包裹体 椭圆形、圆形为主大小一般小于10 μm -13.1~-0.3 121~474 0.5~17.0 在第Ⅳ阶段该类包裹体呈线状或带状产出,一般为次生包裹体
      C型 含CO2三相包裹体 圆形、椭圆形和不规则形为主,气相CO2位于中央,外侧依次是液相CO2、液相H2O,大小一般6~20 μm 0.9~9.2 15.6~30.8 254~470 1.6~14.5 该类型包裹体第Ⅰ和Ⅱ成矿阶段较为常见,往往呈孤立状产出,少数群状、线状出现
      含CO2两相包裹体 负晶型为主,存在液相CO2和气相CO2,一般4~12 μm 28.1~30.1
      S型 含子矿物多相包裹体 椭圆和不规则为主,一般子矿物数量为1~2个,少数3~4个,大小通常为6~22 μm 324~551 324~551 39.8~66.7 第Ⅰ阶段有含石盐、钾盐、赤铁矿和硬石膏的S型包裹体
      292~466 292~466 37.4~55.8 第Ⅱ阶段有含石盐、黄铜矿和辉钼矿的S型包裹体
      -2.7~-1.8 253~316 3.0~4.5 第Ⅲ阶段可见含方解石的S型包裹体
      第Ⅳ阶段未见S型包裹体
      下载: 导出CSV

      表  2  包裹体激光拉曼测试结果

      Table  2.   Raman spectra of fluid inclusions

      主矿物(阶段) 包裹体类型 测试对象 成分(个数) 拉曼特征峰值(cm-1)
      石英斑晶 L+V型包裹体 气相 CO2(10) 1 387, 1 283.9
      L+V型包裹体 液相 水(10) 3 440
      S型包裹体 子矿物 石膏(4) 1 008
      C型包裹体 气相 CO2(2) 1 385, 1 281
      熔体-流体包裹体 熔体 钠长石(2) 506.9, 479.2
      熔体-流体包裹体 熔体 更长石(3) 508.8, 477.6
      石英(Ⅰ) L+V型包裹体 液相 水(8) 3 465
      C型包裹体 气相 CO2(8) 1 388.8, 1 285.8
      S型包裹体 子矿物 赤铁矿(7) 1 311.1, 408
      S型包裹体 子矿物 硬石膏 1 015.9, 1 127.5, 674.7
      石英(Ⅱ) L+V型包裹体 气相 CO2(5) 1 388.8, 1 285.8
      S型包裹体 子矿物 黄铜矿(2) 291.1, 349.3
      S型包裹体 子矿物 辉钼矿(3) 408.8, 464.9
      石英(Ⅲ) C型包裹体 气相 CO2(3) 1 387, 1 283
      L+V型包裹体 液相 水(8) 3 443
      S型包裹体 子矿物 方解石(4) 1 086.19
      石英(Ⅳ) L+V型包裹体 液相 水(6) 3 441
      下载: 导出CSV

      表  3  岔路口矿床流体包裹体(群体)气相成分特征摩尔分数(%)

      Table  3.   Gaseous composition of mass fluid inclusions of the Sawayardun deposit

      样品 矿物成矿阶段 CH4 C2H2+C2H4 C2H6 CO2 H2O O2 N2 CO CO2/CH4 H2O/CO2
      1606-2 石英(I) 0.01 0.01 b.d. 12.36 66.45 2.84 18.33 b.d. 1236.00 5.38
      1114-2 石英(I) 0.03 b.d. b.d. 9.76 70.65 2.89 16.67 b.d. 325.33 7.24
      1606-1 石英(I) 0.01 b.d. b.d. 6.66 71.45 3.22 18.50 0.60 666.00 10.73
      1102-6 石英(П) 0.01 b.d. b.d. 8.64 55.95 5.34 29.85 0.53 864.00 6.48
      1102-9 石英(П) 0.01 b.d. b.d. 8.37 81.95 1.18 8.33 0.74 837.00 9.79
      DB-14 石英(Ш) 0.01 b.d. b.d. 7.97 70.67 3.12 18.23 b.d. 797.00 8.87
      DB-12 石英(Ш) 0.01 b.d. b.d. 10.71 59.98 4.31 24.99 b.d. 1071.00 5.60
      注: “b.d.”表示低于检测限; 单位为摩尔百分含量.
      下载: 导出CSV

      表  4  岔路口矿床流体包裹体(群体)液相成分特征(10-6)

      Table  4.   Aqueous composition(10-6) of mass fluid inclusions of the Chalukou deposit

      样品 矿物成矿阶段 Li+ Na+ K+ Mg2+ Ca2+ F- Cl- Br- NO2- NO3- SO42- ∑M+ ∑M- Na+/K+ K+/Na+ Na+/(Mg2++Ca2+) C1-/S042- F-/C1-
      1606-1 石英(I) b.d. 4.76 12.87 0.57 5.82 0.34 8.27 b.d. b.d. 1.44 19.64 24.02 29.69 0.37 2.70 0.74 0.42 0.04
      1114-2 石英(I) b.d. 0.83 0.55 0.63 6.76 0.25 1.22 b.d. b.d. 0.94 6.93 8.76 9.34 1.52 0.66 0.11 0.18 0.20
      1606-2 石英(I) b.d. 0.81 b.d. 0.51 9.61 0.20 2.52 b.d. b.d. 1.80 4.06 10.92 8.58 0.08 0.62 0.08
      1102-6 石英(Ⅱ) b.d. 1.31 1.26 0.41 13.18 0.22 8.45 b.d. b.d. 1.41 4.39 16.16 14.47 1.04 0.96 0.10 1.92 0.03
      1102-9 石英(Ⅱ) b.d. 5.15 22.21 0.80 5.81 0.52 3.50 b.d. b.d. 1.19 33.73 33.97 38.94 0.23 4.31 0.78 0.10 0.15
      DB-14 石英(Ⅲ) b.d. 1.77 3.81 0.29 4.22 0.21 2.84 b.d. b.d. 1.63 14.58 10.08 19.26 0.46 2.15 0.39 0.19 0.07
      DB-12 石英(Ⅲ) b.d. 1.94 3.89 0.70 6.90 0.14 1.67 b.d. b.d. 1.46 8.34 13.43 11.61 0.50 2.00 0.26 0.20 0.08
      注:∑M+和∑M-分别为阳离子(团)和阴离子(团);“b. d. ”表示低于检测限.
      下载: 导出CSV
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