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    赣东北东乡铜矿侵入岩与成矿年龄的确定及意义

    蔡逸涛 倪培 王国光 陈辉 张洁

    蔡逸涛, 倪培, 王国光, 陈辉, 张洁, 2017. 赣东北东乡铜矿侵入岩与成矿年龄的确定及意义. 地球科学, 42(9): 1495-1507. doi: 10.3799/dqkx.2017.500
    引用本文: 蔡逸涛, 倪培, 王国光, 陈辉, 张洁, 2017. 赣东北东乡铜矿侵入岩与成矿年龄的确定及意义. 地球科学, 42(9): 1495-1507. doi: 10.3799/dqkx.2017.500
    Cai Yitao, Ni Pei, Wang Guoguang, Chen Hui, Zhang Jie, 2017. Determination of Diagenetic and Metallogenic Age and Their Significance in Dongxiang Copper Deposit, Northeast Jiangxi Province, China. Earth Science, 42(9): 1495-1507. doi: 10.3799/dqkx.2017.500
    Citation: Cai Yitao, Ni Pei, Wang Guoguang, Chen Hui, Zhang Jie, 2017. Determination of Diagenetic and Metallogenic Age and Their Significance in Dongxiang Copper Deposit, Northeast Jiangxi Province, China. Earth Science, 42(9): 1495-1507. doi: 10.3799/dqkx.2017.500

    赣东北东乡铜矿侵入岩与成矿年龄的确定及意义

    doi: 10.3799/dqkx.2017.500
    基金项目: 

    国家重点研发计划 2016YFC0600206

    中国地质调查局项目 20089935

    详细信息
      作者简介:

      蔡逸涛(1982-), 男, 助理研究员, 研究方向为内生金属矿床成矿规律及流体包裹体研究

      通讯作者:

      倪培, E-mail:peini@nju.edu.cn

    • 中图分类号: P597

    Determination of Diagenetic and Metallogenic Age and Their Significance in Dongxiang Copper Deposit, Northeast Jiangxi Province, China

    • 摘要: 对于赣东北地区东乡铜矿床的成因机制,一直存在着海西期海底喷流沉积成矿作用与燕山期岩浆热液成矿作用的成因争议,获得精确的成矿年龄是解决这一成因争议的关键.利用LA-ICP-MS技术对矿区中与矿体伴生的花岗闪长斑岩进行了锆石U-Pb同位素定年,两个花岗闪长斑岩样品的形成年龄分别为164±2 Ma、160±1 Ma.同时对东乡铜矿床块状硫化物矿石中的石英,开展了流体包裹体Rb-Sr同位素定年研究,获得一条等时线年龄为161.8±9.6 Ma(MSDW=1.3).结合对流体包裹体以及区域成矿作用的研究,认为该年龄可以代表东乡铜矿的形成时代.这些定年结果表明,东乡铜矿的形成可能与该区燕山期花岗闪长斑岩侵入活动带来的岩浆流体成矿作用有关.

       

    • 图  1  赣东北区域地质及矿区地质简图

      图a据杨明桂和梅勇文(1997);图b据李培铮等(1999);图c据张国林和何国朝(2002).1.钦杭结合带;2.深大断裂;3.一般断裂;4.倒转背斜;5.中生代火山岩;6.燕山期侵入岩;7.第四系;8.上白垩统南雄组;9.上石炭统壶天群;10.石炭系梓山组;11.上泥盆统-下石炭统中棚组;12.新元古界双桥山群;13.矿体平面投影位置

      Fig.  1.  Geological sketch of northeast Jiangxi Province and geological sketch of the Dongxiang copper deposit

      图  2  东乡铜矿矿石样品及流体包裹体照片

      a.黄铁黄铜矿矿石,可见金属硫化物矿物之间石英,黄铁矿晶粒较大,碎裂现象明显(DT656);b.黄铜矿,他形;c.成矿阶段石英中含子晶三相流体包裹体;d.富气相包裹体;e.富液相包裹体.Ccp.黄铜矿;Q.石英;Py.黄铁矿;S.子晶;L.液相;V.气相

      Fig.  2.  Photos of mineral in the Dongxiang copper deposit and fluid inclusions in the ore stage of quartz veins

      图  3  东乡铜矿区67线勘探线剖面采样点示意

      1.白云质灰岩;2.细砂岩;3.花岗闪长斑岩;4.铜矿体;5.采样点.C1-2z.下-上石炭统梓山组;C2H.中石炭统壶天群;K2n.上白垩纪南雄组

      Fig.  3.  Profile sketch of prospecting line 67 of Dongxiang copper deposit

      图  4  东乡铜矿矿石中石英流体包裹体中Rb-Sr同位素等时线

      Fig.  4.  Rb-Sr isotope data and isochron ages of fluid inclusion in quiz from Dongxiang mineral

      图  5  样品的锆石的CL图像

      实线圆为年龄分析点

      Fig.  5.  CL images of zircon grains from Samples of Dongxiang

      图  6  花岗闪长斑岩的锆石207Pb/235U-206Pb/238U同位素年龄谐和图

      样品DT050、DT086为花岗闪长斑岩

      Fig.  6.  The 207Pb/235U-206Pb/238U ages of zircon grains from granodiorite-porphyries and quartz porphyry

      表  1  东乡铜矿矿石中石英流体包裹体中Rb-Sr同位素组成

      Table  1.   Rb-Sr isotope data of fluid inclusion in quiz from Dongxiang mineral

      样品 Rb(10-6) Sr(10-6) 87Rb/86Sr 87Sr/86Sr 2σ
      DT365 0.785 6 0.569 7 3.98 0.724 01 0.000 04
      DT366-2 0.990 2 0.646 4 4.43 0.724 97 0.000 06
      DT366-3 1.642 0 1.227 0 3.86 0.723 80 0.000 09
      DT367 2.080 0 1.254 0 4.79 0.726 02 0.000 01
      DT368 0.867 9 0.734 1 3.41 0.722 78 0.000 01
      下载: 导出CSV

      表  2  东乡铜矿侵入岩LA-ICP-MS锆石分析结果

      Table  2.   Zircon LA-ICP-MS U-Pb results for intrusion of Dongxiang copper deposit

      样品Th UTh/U同位素比值 同位素年龄(Ma)
      (10-6)207Pb/206Pb error 207Pb/235U error 206Pb/238U error 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ
      DT050
      1 381 436 0.87 0.053 89 0.001 44 0.189 02 0.004 97 0.025 47 0.000 33 366 62 176 4 162 2
      2 870 789 1.10 0.052 61 0.001 16 0.184 32 0.004 10 0.025 44 0.000 33 312 51 172 4 162 2
      3 567 434 1.31 0.051 80 0.001 97 0.182 74 0.006 75 0.025 63 0.000 40 277 89 170 6 163 3
      4 666 579 1.15 0.057 50 0.001 85 0.202 11 0.006 35 0.025 52 0.000 36 511 72 187 5 162 2
      5 536 499 1.07 0.048 93 0.001 52 0.170 76 0.005 17 0.025 34 0.000 35 144 74 160 4 161 2
      6 1 139 877 1.30 0.050 78 0.001 61 0.179 62 0.005 67 0.025 67 0.000 40 231 75 168 5 163 3
      7 635 521 1.22 0.051 27 0.002 36 0.182 15 0.008 25 0.025 78 0.000 42 253 108 170 7 164 3
      9 705 734 0.96 0.052 32 0.001 31 0.189 67 0.004 76 0.026 30 0.000 37 299 58 176 4 167 2
      12 553 527 1.05 0.049 15 0.001 33 0.172 24 0.004 67 0.025 42 0.000 36 155 65 161 4 162 2
      14 927 532 1.74 0.046 46 0.001 24 0.166 57 0.004 44 0.026 01 0.000 36 22 56 156 4 166 2
      15 3 572 1 146 3.12 0.053 33 0.001 14 0.195 11 0.004 25 0.026 54 0.000 36 343 50 181 4 169 2
      16 713 954 0.75 0.056 27 0.001 47 0.199 42 0.005 24 0.025 71 0.000 39 463 59 185 4 164 2
      17 1 180 830 1.42 0.048 95 0.001 10 0.179 41 0.004 06 0.026 59 0.000 36 145 54 168 3 169 2
      18 449 353 1.27 0.071 76 0.001 88 0.256 01 0.006 60 0.025 88 0.000 37 979 55 231 5 165 2
      DT086
      1 238 223 1.06 0.046 53 0.001 58 0.161 37 0.005 43 0.025 15 0.000 38 25 72 152 5 160 2
      2 540 489 1.10 0.049 68 0.001 57 0.170 22 0.005 33 0.024 85 0.000 39 180 75 160 5 158 2
      3 563 439 1.28 0.048 00 0.001 41 0.170 27 0.005 08 0.025 73 0.000 42 99 68 160 4 164 3
      4 441 341 1.30 0.049 61 0.001 32 0.170 99 0.004 61 0.025 00 0.000 38 177 64 160 4 159 2
      6 242 229 1.06 0.047 83 0.001 27 0.167 63 0.004 45 0.02 542 0.000 36 91 62 157 4 162 2
      7 327 250 1.31 0.058 74 0.001 97 0.204 44 0.006 77 0.025 24 0.000 42 557 75 189 6 161 3
      8 623 425 1.47 0.049 01 0.001 12 0.155 44 0.003 55 0.023 00 0.000 30 148 55 147 3 147 2
      9 171 146 1.17 0.049 63 0.004 37 0.172 06 0.014 70 0.025 15 0.000 72 178 200 161 13 160 5
      10 447 292 1.53 0.048 97 0.001 51 0.170 63 0.005 26 0.025 27 0.000 40 146 74 160 5 161 3
      12 867 867 1.00 0.048 69 0.001 06 0.168 61 0.003 74 0.025 12 0.000 35 133 52 158 3 160 2
      13 808 635 1.27 0.049 28 0.000 98 0.171 37 0.003 53 0.025 23 0.000 34 161 48 161 3 161 2
      14 701 732 0.96 0.049 01 0.000 88 0.218 98 0.004 25 0.032 41 0.000 47 148 43 201 4 206 3
      16 363 906 0.40 0.051 06 0.001 56 0.178 35 0.005 27 0.025 35 0.000 36 244 72 167 5 161 2
      17 889 740 1.20 0.048 67 0.001 07 0.167 30 0.003 79 0.024 94 0.000 36 132 53 157 3 159 2
      18 256 289 0.89 0.049 51 0.001 46 0.191 45 0.005 67 0.028 05 0.000 43 172 70 178 5 178 3
      19 376 246 1.53 0.050 52 0.001 64 0.173 70 0.005 54 0.024 94 0.000 38 219 77 163 5 159 2
      20 670 453 1.48 0.048 80 0.003 18 0.169 21 0.010 74 0.025 16 0.000 62 138 147 159 9 160 4
      21 297 249 1.19 0.049 42 0.001 88 0.170 79 0.006 34 0.025 07 0.000 40 168 90 160 5 160 3
      22 298 300 0.99 0.045 77 0.002 90 0.165 22 0.010 22 0.026 17 0.000 63 -14 139 155 9 167 4
      23 626 545 1.15 0.050 59 0.003 34 0.177 58 0.011 35 0.025 50 0.000 66 222 151 166 10 162 4
      24 1092 663 1.65 0.048 96 0.001 25 0.174 51 0.004 49 0.025 87 0.000 39 146 61 163 4 165 2
      25 247 252 0.98 0.051 99 0.001 39 0.176 55 0.004 75 0.024 65 0.000 37 285 63 165 4 157 2
      下载: 导出CSV
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