• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    鞍山-本溪地区鞍山群含BIF表壳岩形成时代新证据:锆石SHRIMP U-Pb定年

    万渝生 董春艳 颉颃强 谢士稳 刘守偈 白文倩 马铭株 刘敦一

    万渝生, 董春艳, 颉颃强, 谢士稳, 刘守偈, 白文倩, 马铭株, 刘敦一, 2018. 鞍山-本溪地区鞍山群含BIF表壳岩形成时代新证据:锆石SHRIMP U-Pb定年. 地球科学, 43(1): 57-81. doi: 10.3799/dqkx.2018.004
    引用本文: 万渝生, 董春艳, 颉颃强, 谢士稳, 刘守偈, 白文倩, 马铭株, 刘敦一, 2018. 鞍山-本溪地区鞍山群含BIF表壳岩形成时代新证据:锆石SHRIMP U-Pb定年. 地球科学, 43(1): 57-81. doi: 10.3799/dqkx.2018.004
    Wan Yusheng, Dong Chunyan, Xie Hangqiang, Xie Shiwen, Liu Shoujie, Bai Wenqian, Ma Mingzhu, Liu Dunyi, 2018. Formation Age of BIF-Bearing Anshan Group Supracrustal Rocks in Anshan-Benxi Area: New Evidence from SHRIMP U-Pb Zircon Dating. Earth Science, 43(1): 57-81. doi: 10.3799/dqkx.2018.004
    Citation: Wan Yusheng, Dong Chunyan, Xie Hangqiang, Xie Shiwen, Liu Shoujie, Bai Wenqian, Ma Mingzhu, Liu Dunyi, 2018. Formation Age of BIF-Bearing Anshan Group Supracrustal Rocks in Anshan-Benxi Area: New Evidence from SHRIMP U-Pb Zircon Dating. Earth Science, 43(1): 57-81. doi: 10.3799/dqkx.2018.004

    鞍山-本溪地区鞍山群含BIF表壳岩形成时代新证据:锆石SHRIMP U-Pb定年

    doi: 10.3799/dqkx.2018.004
    基金项目: 

    科技部基础专项 2015FY31010

    中国地质调查局项目 121201102000150012

    中国地质调查局项目 DD20160121-03

    国家自然科学基金 41472169

    详细信息
      作者简介:

      万渝生(1958-), 男, 研究员, 主要从事华北克拉通早前寒武纪地质、锆石成因和SHRIMP U-Pb同位素年代学研究

    • 中图分类号: P581

    Formation Age of BIF-Bearing Anshan Group Supracrustal Rocks in Anshan-Benxi Area: New Evidence from SHRIMP U-Pb Zircon Dating

    • 摘要: 鞍本是华北克拉通最为重要的BIF铁矿集中区之一,BIF赋存于鞍山群表壳岩中.通过对广泛分布的鞍山群表壳岩的12个样品进行锆石SHRIMP U-Pb定年,大都获得2.50~2.55 Ga岩浆锆石年龄,一些岩石中存在2.7~3.5 Ga碎屑锆石或外来锆石.一些东北部(东部)岩石记录了新太古代晚期-古元古代早期变质锆石年龄.结合前人研究成果,可得出如下结论:(1)鞍本地区广泛分布的鞍山群含BIF表壳岩形成时代为新太古代晚期;(2)鞍山群表壳岩形成于陆壳基底之上.该研究进一步支持了已有认识:鞍本为东部古陆块西缘新太古代晚期巨型BIF成矿带的重要组成部分,稳定的构造环境有利于大规模BIF形成.

       

    • 图  1  鞍本地区地质简图

      图据Wan et al.(2015b);图中给出了定年样品位置.编号为斜体的样品引自文献(王守伦和张瑞华,1995代堰锫等,2012万渝生等,2012Cui et al., 2013; Han et al., 2014; Zhu et al., 2015; Li et al., 2016; Guo et al., 2017);ZK7921位置不能准确确定,但在齐大山矿带上;G02-8位置不能准确确定,但在弓长岭矿区;其他的来自本文

      Fig.  1.  Geological sketch of the Anben area

      图  2  鞍本地区鞍山群表壳岩的野外照片

      a.表壳岩露头远景,眼前山铁矿;b.黑云变粒岩(A1502),眼前山铁矿;c.二云石英片岩呈层状产出,弓长岭岭东矿区;d.二云石英片岩(A1114),弓长岭岭东矿区;e.露头远景,表壳岩包体存在于2.5 Ga正长花岗岩中,连山关北;f.黑云二长变粒岩(A1217),连山关北

      Fig.  2.  Field photos of the Anshan Group supracrustal rocks in Anben

      图  3  鞍本地区鸡冠山乡BIF铁矿区鞍山群表壳岩的野外照片

      a, b.白云片岩(A1437);c, d.黑云变粒岩(A1504);e, f.变质酸性火山岩(A1505)

      Fig.  3.  Field photos of the Anshan Group supracrustal rocks in Jiguanxiang BIF mine, Anben

      图  4  鞍本地区鞍山群表壳岩的野外照片

      a.表壳岩被2.5 Ga正长花岗岩脉切割,鸡冠山北;b.角闪变粒岩(A1225),鸡冠山北;c.表壳岩被包裹于2.5 Ga正长花岗岩中,鸡冠山北西;d.黑云变粒岩(A1230),鸡冠山北西;e~h.灯塔市八家子东,e.露头远景;f.黑云变粒岩发生皱褶变形,被包裹于深熔浅色体中,被花岗岩切割,g.黑云变粒岩被包裹于深熔浅色体中,h.黑云变粒岩(LN1333)

      Fig.  4.  Field photos of the Anshan Group supracrustal rocks in Anben

      图  5  鞍本地区鞍山群表壳岩的野外照片

      a~c.歪头山西南BIF铁矿区,a.BIF铁矿区远景,b.不同类型岩石相互关系,表壳岩被2.5 Ga正长花岗岩切割,c.斜长角闪岩(LN1331);d.黑云变粒岩(A1241),歪头山西南;e.黑云变粒岩(LN1332),歪头山西;f.黑云变粒岩被花岗岩脉切割,歪头山西

      Fig.  5.  Field photos of the Anshan Group supracrustal rocks in Anben

      图  6  鞍本地区鞍山群表壳岩的锆石阴极发光图像

      a, b.黑云变粒岩(A1502),眼前山铁矿;c, d.二云石英片岩(A1114),弓长岭岭东矿区;e, f.黑云二长变粒岩(A1217),连山关北

      Fig.  6.  Cathodoluminescence images of zircons from the Anshan Group supracrustal rocks in Anben

      图  7  鞍本地区鞍山群表壳岩的锆石U-Pb谐和图

      a.黑云变粒岩(A1502),眼前山铁矿;b.二云石英片岩(A1114),弓长岭岭东矿区;c.黑云二长变粒岩(A1217),连山关北;d~f.鸡冠山乡BIF铁矿,d.白云片岩(A1437),e.黑云变粒岩(A1504),f.变质酸性火山岩(A1505)

      Fig.  7.  Concordia diagrams for SHRIMP U-Pb zircon analyses of the Anshan Group supracrustal rocks in Anben

      图  8  鞍本地区鸡冠山乡BIF铁矿区鞍山群表壳岩的锆石阴极发光图像

      a, b.白云片岩(A1437);c, d.黑云变粒岩(A1504);e, f.变质酸性火山岩(A1505)

      Fig.  8.  Cathodoluminescence images of zircons from the Anshan Group supracrustal rocks in Jiguanxiang BIF mine, Anben

      图  9  鞍本地区鞍山群表壳岩的锆石阴极发光图像

      a, b.角闪变粒岩(A1225),鸡冠山北;c, d.黑云变粒岩(A1230),鸡冠山北西;e, f.黑云变粒岩(LN1333),灯塔八家子东

      Fig.  9.  Cathodoluminescence images of zircons from the Anshan Group supracrustal rocks in Anben

      图  10  鞍本地区鞍山群表壳岩的锆石U-Pb谐和图

      a.角闪变粒岩(A1225),鸡冠山北;b.黑云变粒岩(A1230),鸡冠山北西;c.黑云变粒岩(LN1333),灯塔八家子东;d.斜长角闪岩(LN1331),歪头山西南BIF铁矿区;e.黑云变粒岩(A1241),歪头山西南;f.黑云变粒岩(LN1332),歪头山西

      Fig.  10.  Concordia diagrams for SHRIMP U-Pb zircon analyses of the Anshan Group supracrustal rocks in Anben

      图  11  鞍本地区鞍山群表壳岩的锆石阴极发光图像

      a, b.斜长角闪岩(LN1331),歪头山西南BIF铁矿区;c, d.黑云变粒岩(A1241),歪头山西南;e, f.黑云变粒岩(LN1332),歪头山西

      Fig.  11.  Cathodoluminescence images of zircons from the Anshan Group supracrustal rocks in Anben

      图  12  华北克拉通地质简图

      Wan et al.(2016a)修改;图中给出了>2.6 Ga古陆块分布和新太古代晚期和古元古代BIF空间分布;EAT.东部古陆块;SAT.南部古陆块;CAT.中部古陆块;中国地图据1:1亿中华人民共和国地图(审图号:GS(2016)1552号,国家测绘地理信息局监制)修改

      Fig.  12.  Geological sketch of the North China Craton

      附表 1  鞍本地区鞍山群表壳岩的锆石SHRIMP U-Pb同位素年龄

      附表 1.   SHRIMP U-Pb data for zircons from the Anshan Group supracrustal rocks in Anben

      黑云变粒岩(A1502)
      数据点 206Pbc
      (%)
      U
      (10-6)
      Th
      (10-6)
      Th/
      U
      206Pb*
      (10-6)
      207Pb*/
      206Pb*
      ±% 207Pb*/
      235U
      ±% 206Pb*/
      238U
      ±% 误差相关系数 206Pb/
      238U年龄(Ma)
      207Pb/
      206Pb年龄(Ma)
      不谐和度
      (%)
      1.1 1.36 499 251 0.52 150 0.159 0 1.10 7.520 1.8 0.343 2 1.4 0.80 1 902 ±23 2 445 ±18 22
      2.1 2.88 725 143 0.20 159 0.152 1 1.40 5.148 1.9 0.245 6 1.4 0.74 1 416 ±18 2 369 ±22 40
      3.1 2.47 329 119 0.37 122 0.168 9 1.70 9.740 2.2 0.418 7 1.5 0.65 2 255 ±28 2 546 ±28 11
      4.1 0.38 133 16 0.12 54 0.171 6 0.86 11.190 1.8 0.473 1 1.5 0.87 2 497 ±32 2 573 ±14 3
      5.1 0.22 432 271 0.65 149 0.165 7 0.60 9.140 1.6 0.400 3 1.5 0.92 2 170 ±27 2 515 ±10 14
      6.1 1.40 371 157 0.44 153 0.166 2 1.00 10.840 1.8 0.473 3 1.5 0.83 2 498 ±31 2 519 ±17 1
      7.1 5.25 1 887 543 0.30 183 0.096 2 3.40 1.403 3.6 0.106 0 1.5 0.41 649 ± 9 1 549 ±61 58
      8.1 0.95 158 146 0.95 67 0.169 1 1.10 11.400 1.9 0.489 3 1.6 0.83 2 567 ±34 2 548 ±18 -1
      9.1 0.27 205 187 0.94 70 0.164 9 0.79 9.000 1.8 0.395 6 1.6 0.89 2 149 ±29 2 507 ±13 14
      10.1 6.74 363 429 1.22 104 0.153 8 4.20 6.450 4.5 0.305 0 2.1 0.46 1 716 ±31 2 385 ±69 28
      11.1 1.74 386 185 0.50 131 0.162 6 1.00 8.690 1.9 0.387 6 1.6 0.84 2 112 ±28 2 482 ±17 1
      12.1 2.35 682 320 0.48 172 0.152 6 1.20 6.010 1.8 0.285 6 1.5 0.80 1 620 ±21 2 374 ±19 32
      13.1 6.37 3 356 1 666 0.51 216 0.082 6 4.10 0.794 4.2 0.069 8 1.5 0.35 435 ± 6 1 259 ±78 65
      14.1 -0.01 97 79 0.84 41 0.168 5 0.76 11.460 1.7 0.492 9 1.6 0.90 2 583 ±33 2 543 ±13 -2
      15.1 0.13 288 420 1.51 105 0.168 6 0.63 9.840 1.7 0.423 4 1.6 0.93 2 276 ±30 2 544 ±11 11
      云母石英片岩(A1114)
      1.1 0.95 197 311 1.63 103 0.233 0 1.50 19.270 3.1 0.600 0 2.7 0.86 3 029 ±64 3 073 ±25 1
      2.1 0.13 663 127 0.20 331 0.232 4 0.39 18.610 2.4 0.581 0 2.4 0.99 2 952 ±56 3 069 ± 6 4
      3.1 0.58 2 803 639 0.24 380 0.103 1 10.00 2.233 2.4 0.157 1 2.2 0.91 940 ±19 1 681 ±18 44
      4.1 0.33 1 644 465 0.29 346 0.151 0 1.00 5.090 2.4 0.244 3 2.2 0.91 1 409 ±28 2 357 ±17 40
      5.1 0.28 2 805 529 0.19 381 0.099 4 0.68 2.162 2.2 0.157 7 2.1 0.95 944 ±19 1 613 ±13 41
      6.1 0.39 1 651 486 0.30 297 0.158 3 0.73 4.560 2.3 0.208 8 2.2 0.95 1 223 ±24 2 438 ±12 50
      7.1 0.35 2 281 721 0.33 337 0.103 9 0.87 2.455 2.3 0.171 4 2.1 0.93 1 020 ±20 1 694 ±16 40
      8.1 0.37 733 246 0.35 239 0.201 4 0.73 10.520 2.3 0.378 9 2.2 0.95 2 071 ±39 2 838 ±12 27
      9.1 0.35 2 192 811 0.38 386 0.120 5 0.78 3.389 2.3 0.204 0 2.2 0.94 1 197 ±23 1 964 ±14 39
      10.1 0.32 705 651 0.95 267 0.205 7 0.76 12.440 2.3 0.438 8 2.2 0.95 2 345 ±44 2 872 ±12 18
      11.1 0.34 1 467 582 0.41 342 0.162 8 0.96 6.060 2.4 0.270 1 2.2 0.92 1 541 ±30 2 485 ±16 38
      12.1 0.12 891 191 0.22 391 0.219 7 0.51 15.450 2.3 0.510 0 2.2 0.97 2 657 ±48 2 979 ± 8 11
      13.1 0.27 885 197 0.23 283 0.190 0 0.67 9.740 2.3 0.371 9 2.2 0.96 2 038 ±38 2 742 ±11 26
      黑云二长变粒岩(A1217)
      数据点 206Pbc
      (%)
      U
      (10-6)
      Th
      (10-6)
      Th/
      U
      206Pb*
      (10-6)
      207Pb*/
      206Pb*
      ±% 207Pb*/
      235U
      ±% 206Pb*/
      238U
      ±% 误差相关系数 206Pb/
      238U年龄(Ma)
      207Pb/
      206Pb年龄(Ma)
      不谐和度
      (%)
      1.1 0.00 139 53 0.39 56.9 0.163 4 1.10 10.720 3.7 0.476 0 3.5 0.95 2 509 ±72 2 492 ±19 -1
      2.1 0.04 167 71 0.44 69.6 0.161 1 0.81 10.790 3.5 0.486 0 3.4 0.97 2 553 ±72 2 467 ±14 -3
      3.1 0.00 352 151 0.44 137 0.160 2 0.57 9.970 3.3 0.451 0 3.3 0.99 2 401 ±66 2 458 ± 10 2
      4.1 0.32 181 37 0.21 78.5 0.163 5 1.00 11.360 3.6 0.504 0 3.4 0.96 2 629 ±74 2 493 ±17 -5
      5.1 0.11 276 363 1.36 84.2 0.155 5 0.74 7.590 4.0 0.354 0 3.9 0.98 1 953 ±66 2 407 ±13 19
      6.1 0.05 667 449 0.70 158 0.145 4 0.69 5.510 3.5 0.274 8 3.5 0.98 1 565 ±48 2 293 ±12 32
      7.1 0.04 434 297 0.71 144 0.154 2 0.56 8.190 3.4 0.385 0 3.4 0.99 2 101 ±60 2 393 ± 10 12
      白云片岩(A1437)
      1.1 0.64 1 329 1 277 0.99 144 0.179 4 0.63 3.106 1.2 0.125 5 1.0 0.85 762.4 ± 7 2 648 ±11 71
      2.1 0.04 474 362 0.79 204 0.296 7 0.25 20.550 1.0 0.502 4 1.0 0.97 2 624 ±22 3 453 ± 4 24
      3.1 0.40 1 012 710 0.73 165 0.145 0 0.49 3.782 1.3 0.189 2 1.2 0.92 1 117 ±12 2 287 ± 9 51
      4.1 0.82 2 341 1 379 0.61 171 0.102 8 0.78 1.195 1.2 0.084 3 1.0 0.77 522 ± 5 1 676 ±14 69
      5.1 0.25 864 189 0.23 142 0.182 6 0.86 4.815 1.3 0.191 2 1.0 0.75 1 128 ±10 2 677 ±14 58
      6.1 0.67 744 373 0.52 112 0.163 1 0.56 3.922 1.1 0.174 4 1.0 0.87 1 036 ± 9 2 488 ± 10 58
      7.1 0.03 238 138 0.60 84 0.165 2 0.58 9.330 1.3 0.409 8 1.1 0.89 2 214 ±21 2 510 ± 10 12
      8.1 0.00 197 117 0.61 105 0.316 1 0.60 27.120 1.2 0.622 2 1.1 0.88 3 119 ±27 3 551 ± 9 12
      9.1 0.14 276 435 1.63 92 0.163 5 0.46 8.750 1.2 0.388 0 1.1 0.92 2 114 ±19 2 492 ± 8 15
      10.1 0.02 244 112 0.48 111 0.186 5 0.48 13.610 1.4 0.529 5 1.3 0.94 2 739 ±29 2 711 ± 9 -1
      11.1 0.04 88 89 1.04 37 0.186 6 0.79 12.570 1.6 0.488 4 1.4 0.87 2 564 ±29 2 713 ±13 6
      12.1 - 149 118 0.82 59 0.168 1 0.65 10.710 1.4 0.462 1 1.2 0.88 2 449 ±25 2 539 ±11 4
      黑云变粒岩(A1504)
      1.1 1.11 365 262 0.74 130 0.165 1 0.83 9.300 1.6 0.408 6 1.4 0.87 2 209 ±27 2 508 ±14 12
      2.1 0.38 388 173 0.46 152 0.165 8 0.61 10.370 1.5 0.453 8 1.4 0.92 2 412 ±28 2 515 ±10 4
      3.1 0.10 150 91 0.63 64 0.166 9 0.72 11.420 1.7 0.496 1 1.5 0.90 2 597 ±33 2 527 ±12 -3
      4.1 0.00 228 105 0.48 94 0.165 8 0.65 10.930 1.6 0.477 9 1.5 0.91 2 518 ±31 2 516 ±11 0
      5.1 0.28 168 141 0.87 60 0.167 0 0.82 9.480 1.7 0.411 8 1.5 0.87 2 223 ±27 2 528 ±14 12
      6.1 0.07 292 172 0.61 130 0.168 0 0.57 11.970 1.5 0.516 8 1.4 0.93 2 685 ±30 2 538 ± 10 -6
      9.1 1.30 423 317 0.77 131 0.164 9 1.50 8.020 2.1 0.352 9 1.4 0.68 1 949 ±24 2 506 ±25 22
      7.1 0.58 79 61 0.80 33 0.168 6 1.10 11.230 1.9 0.483 0 1.6 0.82 2 540 ±33 2 544 ±19 0
      8.1 0.39 293 224 0.79 98 0.162 0 0.69 8.620 1.6 0.385 9 1.4 0.90 2 104 ±25 2 476 ±12 15
      10.1 0.81 358 238 0.69 116 0.163 9 0.76 8.390 1.6 0.371 6 1.4 0.88 2 037 ±25 2 496 ±13 18
      11.1 3.95 312 140 0.46 112 0.180 5 1.90 9.840 2.3 0.396 1 1.6 0.67 2 151 ±29 2 655 ±29 19
      12.1 0.23 257 200 0.81 94 0.165 5 0.65 9.740 1.6 0.427 0 1.4 0.91 2 292 ±28 2 513 ±11 9
      13.1 0.33 381 302 0.82 119 0.1682 0.64 8.420 1.6 0.363 1 1.4 0.91 1 997 ±24 2 540 ±11 21
      14.1 0.10 187 114 0.63 78 0.166 2 0.68 11.130 1.6 0.485 6 1.5 0.91 2 551 ±31 2 520 ±11 -1
      15.1 0.05 238 140 0.61 98 0.167 0 0.61 11.060 1.6 0.480 5 1.4 0.92 2 530 ±30 2 527 ±10 0
      16.1 0.03 104 88 0.87 44 0.166 8 0.88 11.320 1.8 0.492 0 1.6 0.87 2 579 ±34 2 526 ±15 -2
      变质酸性火山岩(A1505)
      数据点 206Pbc
      (%)
      U
      (10-6)
      Th
      (10-6)
      Th/
      U
      206Pb*
      (10-6)
      207Pb*/
      206Pb*
      ±% 207Pb*/
      235U
      ±% 206Pb*/
      238U
      ±% 误差相关系数 206Pb/
      238U年龄(Ma)
      207Pb/
      206Pb年龄(Ma)
      不谐和度
      (%)
      1.1 0.86 644 425 0.68 121 0.154 6 1.30 4.600 1.9 0.215 9 1.4 0.72 1 260 ±16 2 396 ±23 47
      2.1 0.04 233 195 0.86 93 0.164 7 0.64 10.520 1.6 0.463 1 1.5 0.91 2 453 ±30 2 504 ±11 2
      3.1 0.31 287 190 0.68 93 0.160 9 0.81 8.290 1.8 0.374 0 1.6 0.89 2 048 ±28 2 465 ±14 17
      4.1 1.77 325 222 0.70 126 0.166 1 1.00 10.130 1.8 0.442 7 1.5 0.83 2 363 ±30 2 518 ±17 6
      5.1 10.95 612 612 1.03 156 0.154 3 5.00 5.430 4.9 0.256 4 1.7 0.35 1 471 ±23 2 387 ±79 38
      6.1 1.86 176 140 0.82 45 0.159 5 2.10 6.400 2.9 0.291 1 2.1 0.71 1 647 ±31 2 449 ±35 33
      7.1 1.10 552 548 1.03 132 0.156 7 0.89 5.930 1.7 0.274 7 1.5 0.86 1 565 ±21 2 419 ±15 35
      8.1 2.30 596 387 0.67 147 0.155 3 1.20 5.960 1.9 0.278 6 1.5 0.79 1 584 ±21 2 404 ±19 34
      9.1 1.58 573 328 0.59 146 0.157 6 0.99 6.310 1.8 0.290 5 1.5 0.85 1 644 ±22 2 429 ±16 32
      10.1 0.16 118 68 0.59 44 0.168 0 0.91 10.140 1.9 0.437 6 1.7 0.88 2 340 ±33 2 538 ±15 8
      11.1 0.05 283 315 1.15 105 0.166 4 0.65 9.920 1.7 0.432 5 1.6 0.92 2 317 ±31 2 521 ±11 8
      12.1 2.14 584 510 0.90 100 0.153 6 1.40 4.124 2.0 0.194 9 1.6 0.77 1 148 ±16 2 385 ±22 52
      13.1 0.65 509 324 0.66 122 0.156 1 0.79 5.970 1.7 0.277 4 1.5 0.89 1 578 ±22 2 414 ±13 35
      14.1 0.09 163 138 0.87 62 0.166 4 0.67 10.070 3.6 0.439 0 3.5 0.98 2 347 ±69 2 521 ±11 7
      15.1 0.05 291 190 0.68 111 0.164 5 0.54 10.050 1.5 0.442 9 1.4 0.93 2 364 ±28 2 503 ± 9 6
      角闪变粒岩(A1225)
      1.1 0.07 197 110 0.58 82 0.165 2 0.76 11.000 3.5 0.483 0 3.4 0.98 2 541 ±71 2 510 ±13 -1
      2.1 0.33 133 104 0.81 70 0.197 7 0.90 16.650 3.9 0.611 0 3.8 0.97 3 073 ±94 2 808 ±15 -9
      2.2 0.07 217 20 0.09 99 0.191 5 0.56 14.090 3.3 0.533 0 3.2 0.99 2 756 ±72 2 756 ± 9 0
      3.1 0.08 636 292 0.48 134 0.150 0 0.64 5.080 3.3 0.245 6 3.2 0.98 1 416 ±41 2 346 ±11 40
      4.1 0.96 915 808 0.91 110 0.130 5 2.50 2.483 4.0 0.137 8 3.2 0.80 832 ±25 2 107 ±43 61
      5.1 0.10 131 76 0.60 51 0.163 0 0.76 10.230 3.3 0.455 0 3.3 0.97 2 418 ±66 2 487 ±13 3
      6.1 0.07 89 104 1.20 37 0.163 4 0.96 10.750 3.5 0.477 0 3.3 0.96 2 514 ±69 2 491 ±16 -1
      7.1 0.03 377 58 0.16 77 0.156 2 0.68 5.120 3.3 0.237 5 3.2 0.98 1 374 ±40 2 415 ±12 43
      8.1 0.08 73 38 0.53 32 0.167 2 1.30 11.800 3.7 0.512 0 3.5 0.94 2 664 ±76 2 530 ±22 -5
      9.1 0.07 182 124 0.70 74 0.165 0 0.81 10.760 3.4 0.473 0 3.3 0.97 2 497 ±69 2 508 ±14 0
      黑云变粒岩(A1230)
      1.1 0.00 33 17 0.54 15 0.168 1 1.70 12.240 4.6 0.528 0 4.3 0.93 2 733 ±95 2 539 ±28 -8
      1.2 0.28 316 193 0.63 92 0.156 6 0.72 7.280 3.9 0.337 0 3.9 0.98 1 873 ±63 2 420 ±12 23
      2.1 0.15 126 134 1.10 57 0.165 7 1.10 11.910 4.1 0.521 0 4.0 0.97 2 704 ±88 2 515 ±18 -7
      3.1 0.79 548 312 0.59 124 0.150 3 1.30 5.390 4.1 0.260 0 3.9 0.95 1 488 ±52 2 351 ±23 37
      4.1 0.96 291 180 0.64 105 0.168 2 1.50 9.650 4.3 0.416 0 4.1 0.94 2 241 ±77 2 541 ±24 12
      5.1 0.30 222 167 0.78 55 0.150 9 1.30 6.020 4.2 0.289 0 3.9 0.95 1 638 ±57 2 357 ±22 31
      6.1 0.87 282 371 1.36 76 0.157 8 1.40 6.750 4.2 0.310 0 3.9 0.95 1 741 ±60 2 434 ±23 28
      7.1 0.41 250 149 0.62 81 0.157 2 1.20 8.140 4.1 0.375 0 4.0 0.96 2 054 ±70 2 427 ±20 15
      8.1 0.13 113 153 1.40 46 0.165 2 1.60 10.840 4.4 0.476 0 4.2 0.94 2 508 ±86 2 510 ±26 0
      9.1 0.56 346 513 1.53 106 0.161 1 1.30 7.870 4.1 0.354 0 3.9 0.95 1 954 ±66 2 469 ±22 21
      10.1 0.38 56 48 0.88 24 0.165 9 1.70 11.520 4.5 0.503 0 4.2 0.93 2 628 ±91 2 517 ±28 -4
      黑云变粒岩(LN1333)
      数据点 206Pbc
      (%)
      U
      (10-6)
      Th
      (10-6)
      Th/
      U
      206Pb*
      (10-6)
      207Pb*/
      206Pb*
      ±% 207Pb*/
      235U
      ±% 206Pb*/
      238U
      ±% 误差相关系数 206Pb/
      238U年龄(Ma)
      207Pb/
      206Pb年龄(Ma)
      不谐和度
      (%)
      1.1 0.02 200 152 0.78 82 0.165 9 0.55 10.890 1.2 0.475 9 1.1 0.89 2 510 ±22 2 517 ±9 0
      2.1 0.17 214 142 0.68 81 0.165 3 0.38 10.030 1.1 0.440 0 1.0 0.94 2 351 ±21 2 511 ±6 6
      3.1 0.06 268 225 0.87 97 0.163 9 0.33 9.460 1.2 0.418 7 1.2 0.96 2 255 ±22 2 496 ±6 10
      4.1 0.05 257 121 0.49 101 0.168 6 0.31 10.670 1.2 0.458 8 1.1 0.96 2 434 ±23 2 544 ± 5 4
      6.1 0.10 173 98 0.59 72 0.166 7 0.42 11.200 1.2 0.487 2 1.1 0.93 2 559 ±23 2 525 ± 7 -1
      7.1 0.09 168 64 0.40 71 0.167 8 0.40 11.400 1.2 0.492 9 1.1 0.94 2 583 ±23 2 536 ± 7 -2
      8.1 0.08 170 76 0.46 71 0.167 5 0.42 11.240 1.2 0.486 9 1.1 0.93 2 557 ±23 2 533 ± 7 -1
      5.1 0.07 257 286 1.15 99 0.166 0 0.32 10.280 1.1 0.449 1 1.1 0.96 2 391 ±21 2 518 ± 5 5
      9.1 0.07 125 55 0.46 52 0.167 3 0.46 11.060 1.2 0.479 4 1.1 0.93 2 525 ±24 2 531 ± 8 0
      10.1 0.03 219 417 1.96 76 0.166 3 0.36 9.290 1.2 0.405 0 1.2 0.96 2 192 ±22 2 521 ±6 13
      11.1 0.10 229 145 0.66 86 0.163 8 0.37 9.890 1.1 0.438 2 1.0 0.94 2 342 ±21 2 495 ±6 6
      12.1 0.05 185 70 0.39 78 0.168 0 0.38 11.340 1.1 0.489 6 1.1 0.94 2 569 ±23 2 538 ±6 -1
      斜长角闪岩(LN1331)
      1.1 0.21 158 63 0.42 65 0.164 8 0.45 10.800 1.3 0.475 3 1.2 0.93 2 507 ±25 2 506 ± 8 0
      2.1 0.12 162 80 0.51 67 0.163 8 0.40 10.930 1.2 0.483 9 1.1 0.94 2 544 ±23 2 496 ± 7 -2
      3.1 0.03 207 53 0.26 85 0.164 5 0.36 10.840 1.1 0.478 0 1.1 0.95 2 519 ±22 2 502 ±6 -1
      4.1 0.03 259 69 0.28 109 0.165 6 0.30 11.170 1.1 0.489 1 1.0 0.96 2 567 ±22 2 514 ± 5 -2
      5.1 0.09 591 250 0.44 156 0.159 4 0.33 6.761 1.0 0.307 6 1.0 0.95 1 729 ±15 2 449 ±6 29
      6.1 0.04 322 159 0.51 133 0.163 8 0.29 10.870 1.1 0.481 3 1.0 0.96 2 533 ±21 2 496 ± 5 -1
      7.1 0.06 184 81 0.45 79 0.164 8 0.37 11.300 1.1 0.497 4 1.1 0.95 2 602 ±23 2 506 ±6 -4
      8.1 0.09 126 50 0.41 51 0.164 9 0.47 10.580 1.2 0.465 4 1.1 0.92 2 463 ±23 2 506 ± 8 2
      9.1 0.05 164 139 0.88 71 0.166 1 0.39 11.550 1.5 0.504 5 1.4 0.96 2 633 ±31 2 518 ± 7 -5
      10.1 0.34 192 239 1.29 80 0.165 0 0.55 10.930 1.3 0.480 6 1.2 0.91 2 530 ±25 2 507 ± 9 -1
      11.1 0.16 135 43 0.33 56 0.164 8 0.47 10.980 1.2 0.483 0 1.1 0.92 2 540 ±23 2 506 ± 8 -1
      12.1 0.10 57 68 1.23 23 0.164 4 0.79 10.400 1.5 0.458 5 1.3 0.86 2 433 ±26 2 502 ±13 3
      黑云变粒岩(A1241)
      数据点 206Pbc
      (%)
      U
      (10-6)
      Th
      (10-6)
      Th/
      U
      206Pb*
      (10-6)
      207Pb*/
      206Pb*
      ±% 207Pb*/
      235U
      ±% 206Pb*/
      238U
      ±% 误差相关系数 206Pb/
      238U年龄(Ma)
      207Pb/
      206Pb年龄(Ma)
      不谐和度
      (%)
      1.1 0.20 901 692 0.79 221 0.244 4 0.71 9.590 3.3 0.284 5 3.2 0.98 1 614 ±46 3 149 ±11 49
      2.1 0.06 822 530 0.67 113 0.207 7 0.44 4.560 3.2 0.159 3 3.2 0.99 953 ±28 2 888 ± 7 67
      3.1 0.21 823 510 0.64 164 0.207 4 1.20 6.600 3.4 0.230 8 3.2 0.94 1 339 ±38 2 886 ±19 54
      4.1 0.94 866 663 0.79 192 0.238 9 0.51 8.380 3.2 0.254 3 3.2 0.99 1 461 ±42 3 114 ± 8 53
      5.1 0.16 682 476 0.72 208 0.274 5 0.33 13.390 3.2 0.354 0 3.2 0.99 1 952 ±54 3 332 ± 5 41
      6.1 0.87 697 477 0.71 167 0.236 6 1.60 9.010 3.6 0.276 0 3.2 0.89 1 571 ±45 3 098 ±25 49
      7.1 0.34 674 456 0.70 182 0.260 6 0.36 11.200 3.2 0.311 8 3.2 0.99 1 750 ±49 3 251 ± 6 46
      8.1 0.03 938 614 0.68 248 0.262 4 0.35 11.110 3.2 0.307 0 3.2 0.99 1 726 ±48 3 261 ± 6 47
      9.1 0.13 864 546 0.65 146 0.210 3 0.44 5.690 3.2 0.196 4 3.2 0.99 1 156 ±34 2 908 ± 7 60
      10.1 0.53 811 397 0.51 165 0.218 9 0.63 7.100 3.2 0.235 3 3.2 0.98 1 362 ±39 2 973 ± 10 54
      11.1 3.71 1 156 947 0.85 174 0.185 4 1.60 4.270 3.5 0.166 5 3.2 0.91 993 ±30 2 709 ±24 63
      12.1 0.18 915 702 0.79 258 0.254 8 0.45 11.490 3.2 0.327 0 3.2 0.99 1 824 ±50 3 215 ± 7 43
      黑云变粒岩(LN1332)
      1.1 0.16 274 233 0.88 102 0.166 3 0.41 9.980 1.1 0.435 2 1.0 0.93 2 329 ±20 2 521 ±7 8
      2.1 2.54 337 71 0.22 94 0.149 8 1.30 6.480 1.6 0.314 1 1.1 0.67 1 761 ±16 2 343 ± 20 25
      3.1 0.08 163 108 0.68 68 0.164 8 0.50 11.070 1.2 0.487 4 1.1 0.91 2 559 ±24 2 505 ±9 -2
      4.1 0.17 173 109 0.65 71 0.166 2 0.44 10.880 1.2 0.474 7 1.1 0.93 2 504 ±22 2 520 ±7 1
      5.1 10.70 321 321 1.03 95 0.158 0 10.00 6.440 10.0 0.296 8 1.5 0.15 1 676 ±22 2 428 ±170 31
      6.1 0.17 83 48 0.60 34 0.165 7 0.68 10.930 1.4 0.478 4 1.2 0.88 2 520 ±26 2 514 ±11 0
      7.1 0.17 193 113 0.61 81 0.167 3 0.43 11.290 1.2 0.489 6 1.1 0.93 2 569 ±23 2 531 ±7 -2
      8.2 1.11 343 327 0.99 78 0.158 4 5.80 5.690 5.9 0.260 9 1.1 0.18 1 494 ±14 2 438 ±98 39
      8.1 0.24 162 188 1.20 58 0.163 9 0.65 9.320 1.3 0.412 3 1.1 0.86 2 225 ±20 2 497 ±11 11
      9.1 3.09 160 170 1.09 44 0.163 1 1.90 6.920 2.2 0.308 1 1.2 0.53 1 732 ±18 2 487 ± 32 30
      10.1 0.46 122 53 0.45 51 0.167 4 0.64 11.180 1.3 0.484 4 1.1 0.88 2 546 ±24 2 532 ±11 -1
      11.1 0.09 155 132 0.88 64 0.166 3 0.44 11.090 1.2 0.483 7 1.1 0.93 2 543 ±23 2 521 ±7 -1
      下载: 导出CSV

      附表 2  鞍本地区表壳岩锆石年龄总结

      附表 2.   Summary of zircon U-Pb ages for the Anshan Group supracrustal rocks in Anben

      顺序号 样品编号 岩石名称 位置 外来或碎屑锆石年龄(Ma) 岩浆锆石年龄
      (Ma)
      变质锆石年龄
      (Ma)
      定年方法 经纬度 数据来源
      1 A1114 二云石英片岩 弓长岭岭东矿区 3 069±12 SHRIMP N41°05′49″/E123°32′6″ 本文
      2 A1217 黑云二长变粒岩 连山关北 2 469±13 SHRIMP N41°00′11″/E123°44′51″ 本文
      3 A1225 角闪变粒岩 鸡冠山乡北 2 756 2 502±13 SHRIMP N41°22′24″/E123°34′56″ 本文
      4 A1230 黑云变粒岩 鸡冠山北西 2 519±23 SHRIMP N41°23′41″/E123°31′03″ 本文
      5 A1241 黑云变粒岩 歪头山西南 3 490±110 SHRIMP N41°28′05″/E123°35′48″ 本文
      6 LN1331 斜长角闪岩 歪头山西南 2 505±4 SHRIMP N41°28′04″/E123°35′57″ 本文
      7 LN1332 黑云变粒岩 歪头山西 2 521±7 SHRIMP N41°29′51″/E123°32′22″ 本文
      8 LN1333 黑云变粒岩 灯塔市八家子东 2 531±6 SHRIMP N41°26′36″/E123°33′58″ 本文
      9 A1437 白云片岩 鸡冠山 2 711, 2 539 SHRIMP N41°18′11″/E123°35′22″ 本文
      10 A1502 黑云变粒岩 眼前山 2 538±17 SHRIMP N41°04′23″/E123°08′07″ 本文
      11 A1504 黑云变粒岩 鸡冠山 2 528±9 SHRIMP N41°18′07″/E123°35′16″ 本文
      12 A1505 变质酸性火山岩 鸡冠山 2 514±9 SHRIMP N41°18′07″/E123°35′16″ 本文
      13 WTS1-15 斜长角闪岩(变质基性岩脉) 歪头山 2 523±12 2 481±19 LA-ICP-MS Cui et al., 2013
      14 CTG-7 片麻状绿泥石化黑云片
      麻岩(绿泥石英片岩)
      陈台沟
      (ZK26钻孔的负815m)
      2 608~2 733 2 551±10 2 469±23 LA-ICP-MS 代堰锫等,2013
      15 G02-8 斜长角闪片岩 弓长岭 2 554±12 SHRIMP Han et al., 2014
      16 A0420 黑云变粒岩 弓长岭 2 705, 2 911 2 528±10 SHRIMP 万渝生等,2012
      17 ZK7921 黑云变粒岩 齐大山
      (ZK7921钻孔的负207m)
      2 533±53 同位素稀释法 王守伦和张瑞华,1995
      18 WTS-11 斜长角闪岩 歪头山 2 611±5,2 530±7 CAMECA 代堰锫等,2012
      19 15YK30-1 绿泥片岩(变质英安岩) 鸡冠山东南 2 756±11 2 574±13 LA-ICP-MS Guo et al., 2017
      20 15YK24-2 绿泥片岩(变质英安岩) 东鞍山 3 009, 2 609~2 612 2 560±7 LA-ICP-MS Guo et al., 2017
      21 石英片岩,黑云变粒岩 齐大山 2 700~3 000 2 530~2 560 1 840~1 880 LA-ICP-MS Li et al., 2016
      22 DNF4-3 绿泥角闪片岩 南芬铁矿区 2 552±18 2 482 LA-ICP-MS Zhu et al., 2015
      下载: 导出CSV
    • [1] Black, L.P., Kamo, S.L., Allen, C.M., et al., 2003.TEMORA 1:A New Zircon Standard for Phanerozoic U-Pb Geochronology.Chemical Geology, 200(1-2):155-170. https://doi.org/10.1016/S0009-2541(03)00165-7
      [2] Chen, Y.W., Zhong, F.D., Liu, J.Y., et al., 1981.Pb Isotopic Age Determinations of Some Precambrian Rocks from North China (Additional Discussion on Precambrian Geochronological Scale of China).Geochimica, 10(3):209-219 (in Chinese with English abstract). doi: 10.1360/03yd0163
      [3] Cheng, Y.Q., 1957.Problems on the Genesis of the High-Grade Ore in the Pre-Sinian (Pre-Cambrian) Banded Iron Ore Deposits of the Anshan-Type of Liaoning and Shantung Provinces.Acta Geologica Sinica, 31(2):153-180, 241-250.(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE195702001.htm
      [4] Cui, P.L., Sun, J.G., Sha, D.M., et al., 2013.Oldest Zircon Xenocryst (4.17 Ga) from the North China Craton.International Geology Review, 55(15):1902-1908. https://doi.org/10.1080/00206814.2013.805925
      [5] Dai, Y.P., Zhang, L.C., Wang, C.L., et al., 2012.Genetic Type, Formation Age and Tectonic Setting of the Waitoushan Banded Iron Formation, Benxi, Liaoning Province.Acta Petrologica Sinica, 28(11):3574-3594 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201211013.htm
      [6] Dai, Y.P., Zhang, L.C., Zhu, M.T., et al., 2013.Chentaigou BIF-Type Iron Deposit, Anshan Area Associated with Archean Crustal Growth:Constraints from Zircon U-Pb Dating and Hf Isotope.Acta Petrologica Sinica, 29(7):2537-2550 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201307020.htm
      [7] Dai, Y.P., Zhang, L.C., Zhu, M.T., et al., 2014.The Composition and Genesis of the Mesoarchean Dagushan Banded Iron Formation (BIF) in the Anshan Area of the North China Craton.Ore Geology Reviews, 63:353-373. https://doi.org/10.1016/j.oregeorev.2014.04.013
      [8] Dong, C.Y., Wan, Y.S., Xie, H.Q., et al., 2017a.The Mesoarchean Tiejiashan-Gongchangling Potassic Granite in the Anshan-Benxi Area, North China Craton:Origin by Recycling of Paleo-to Eoarchean Crust from U-Pb-Nd-Hf-O Isotopic Studies.Lithos, 290-291:116-135. https://doi.org/10.1016/j.lithos.2017.08.009
      [9] Dong, C.Y., Xie, H.Q., Kröner, A., et al., 2017b.The Complexities of Zircon Crystllazition and Overprinting during Metamorphism and Anatexis:An Example from the Late Archean TTG Terrane of Western Shandong Province, China.Precambrian Research, 300:181-200. https://doi.org/10.1016/j.precamres.2017.07.034
      [10] Eriksson, P.G., Altermann, W., Hartzer, F.J., 2006.The Transvaal Supergroup and Its Precursors.In:Johnson, M.R., Anhaecusser, C.R., Thomas, R.J., eds., The Geology of South Africa.Johannesburg, 237-260.
      [11] Guo, R.R., Liu, S.W., Gong, E.P., et al., 2017.Arc-Generated Metavolcanic Rocks in the Anshan-Benxi Greenstone Belt, North China Craton:Constraints from Geochemistry and Zircon U-Pb-Hf Isotoic Systematics.Precambrian Research, in Press.https://doi.org/10.1016/j.precamres.2017.03.028
      [12] Han, C.M., Xiao, W.J., Su, B.X., et al., 2014.Formation Age and Genesis of the Gongchangling Neoarchean Banded Iron Deposit in Eastern Liaoning Province:Constraints from Geochemistry and SHRIMP Zircon U-Pb Dating.Precambrian Research, 254:306-322. https://doi.org/10.1016/j.precamres.2014.09.007
      [13] Li, H.M., Liu, M.J., Li, L.X., et al., 2014.SHRIMP U-Pb Geochronology of Zircons from the Garnet-Rich Altered Rocks in the Mining Area Ⅱ of the Gongchangling Iron Deposit:Constraints on the Ages of the High-Grade Iron Deposit.Acta Petrologica Sinica, 30(5):1205-1217 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0301926816305927
      [14] Li, L.X., Li, H.M., Liu, M.J., et al., 2016.Timing of Deposition and Tectonothermal Events of Banded Iron Formations in the Anshan-Benxi Area, Liaoning Province, China:Evidence from SHRIMP U-Pb Zircon Geochronology of the Wall Rocks.Journal of Asian Earth Sciences, 129:276-293. https://doi.org/10.1016/j.jseaes.2016.08.022
      [15] Liu, D.Y., Nutman, A.P., Compston, W., et al., 1992.Remnants of ≥ 3 800 Ma Crust in the Chinese Part of the Sino-Korean Craton.Geology, 20(4):339-342.https://doi.org/10.1130/0091-7613(1992)020<0339:romcit>2.3.co;2 doi: 10.1130/0091-7613(1992)020<0339:romcit>2.3.co;2
      [16] Liu, D.Y., Wilde, S.A., Wan, Y.S., et al., 2008.New U-Pb and Hf Isotopic Data Confirm Anshan as the Oldest Preserved Segment of the North China Craton.American Journal of Science, 308(3):200-231. https://doi.org/10.2475/03.2008.02
      [17] Liu, S.W., Wang, M.J., Wan, Y.S., et al., 2017.A Reworked~3.45 Ga Continental Microblock of the North China Craton:Constraints from Zircon U-Pb-Lu-Hf Isotopic Systematics of the Archean Beitai-Waitoushan Migmatite-Syenogranite Complex.Precambrian Research, in Press.https://doi.org/10.1016/j.precamres.2017.04.003
      [18] Ludwig, K.R., 2001.Squid 1.02:A User's Manual.Berkeley Geochronology Centre, Berkeley.
      [19] Qiao, G.S., Zhai, M.G., Yan, Y.H., 1990.Geochronological Study of Archaean Rocks in Anshan, Liaoning Province.Scientia Geologica Sinica, 25(2):158-165 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0024493799000821
      [20] Shen, B.F., Zhai, A.M., Yang, C.L., et al., 2005.Temporal-Spatial Distribution and Evolutional Characters of Precambrian Iron Deposits in China.Geological Survey and Research, 28(4):196-206 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-QHWJ200504002.htm
      [21] Song, B., Nutman, A.P., Liu, D.Y., et al., 1996.3 800 to 2 500 Ma Crustal Evolution in the Anshan Area of Liaoning Province, Northeastern China.Precambrian Research, 78(1-3):79-94. https://doi.org/10.1016/0301-9268(95)00070-4
      [22] Sun, X.H., Zhu, X.Q., Tang, H.S., et al., 2014.The Gongchangling BIFs from the Anshan-Benxi Area, NE China:Petrological-Geochemical Characteristics and Genesis of High-Grade Iron Ores.Ore Geology Reviews, 60:112-125. https://doi.org/10.1016/j.oregeorev.2013.12.017
      [23] Van Kranendonk, M.J., Altermann, W., Beard, B.L., et al., 2012.A Chronostratigraphic Division of the Precambrian:A Chronostratigraphic Division of the Precambrian:Possibilities and Challenges.In:Gradstein, F.M., Ogg, J.G., Schmitz, M., et al., eds., The Geologic Time Scale.Elsevier, New York, 299-392.
      [24] Wan, Y.S., 1993.Formation and Evolution of Liaoning Gongchangling Iron Rocks.Beijing Science and Technology Press, Beijing (in Chinese).
      [25] Wan, Y.S., Dong, C.Y., Ren, P., et al., 2017.Spatial and Temporal Distribution, Compositional Characteristics and Formation and Evolution of Archean TTG Rocks in North China Craton:A Synthesis.Acta Petrologica Sinica, 33(5):1405-1419 (in Chinese with English abstract).
      [26] Wan, Y.S., Dong, C.Y., Xie, H.Q., et al., 2012.Formation Ages of Early Precambrian BIFs in the North China Craton:SHRIMP Zircon U-Pb Dating.Acta Geologica Sinica, 86(9):1447-1478 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201209010.htm
      [27] Wan, Y.S., Geng, Y.S., Shen, Q.H., et al., 2002.Geochemical Characteristics of Supracrustal Enclaves in Mesoarchean Tiejiashan Granite in Anshan Area and Its Geological Significance.Chinese Journal of Geology, 37(2):143-151, 164 (in Chinese with English abstract). doi: 10.3321/j.issn:0563-5020.2002.02.002
      [28] Wan, Y.S., Liu, D.Y., 1993.Ages of Zircons from Mid-Archaean Gneissic Granite and Fuchsite Quartzite in the Gongchangling Area, Liaoning.Geological Review, 39(2):124-129 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0024493717302876
      [29] Wan, Y.S., Liu, D.Y., Dong, C.Y., et al., 2015a.Formation and Evolution of Archean Continental Crust of the North China Craton.In:Zhai, M.G., ed., Precambrian Geology of China.Springer, Berlin, 59-136.https://doi.org/10.1007/978-3-662-47885-1_2
      [30] Wan, Y.S., Ma, M., Dong, C.Y., et al., 2015b.Widespread Late Neoarchean Reworking of Meso-to Paleoarchean Continental Crust in the Anshan-Benxi Area, North China Craton, as Documented by U-Pb-Nd-Hf-O Isotopes.American Journal of Science, 315(7):620-670. https://doi.org/10.2475/07.2015.02
      [31] Wan, Y.S., Liu, D.Y., Nutman, A., et al., 2012a.Multiple 3.8-3.1 Ga Tectono-Magmatic Events in a Newly Discovered Area of Ancient Rocks (the Shengousi Complex), Anshan, North China Craton.Journal of Asian Earth Sciences, 54-55:18-30. https://doi.org/10.1016/j.jseaes.2012.03.007
      [32] Wan, Y.S., Wang, S.J., Liu, D.Y., et al., 2012b.Redefinition of Depositional Ages of Neoarchean Supracrustal Rocks in Western Shandong Province, China:SHRIMP U-Pb Zircon Dating.Gondwana Research, 21(4):768-784. https://doi.org/10.1016/j.gr.2011.05.017
      [33] Wan, Y.S., Liu, D.Y., Song, B., et al., 2005.Geochemical and Nd Isotopic Compositions of 3.8 Ga Meta-Quartz Dioritic and Trondhjemitic Rocks from the Anshan Area and Their Geological Significance.Journal of Asian Earth Sciences, 24(5):563-575. https://doi.org/10.1016/j.jseaes.2004.02.009
      [34] Wan, Y.S., Liu, D.Y., Xie, H.Q., et al., 2016a.Formation Ages and Environments of Early Precambrian Banded Iron Formation in the North China Craton.In:Zhai, M.G., ed., Main Tectonic Events and Metallogeny of the North China Craton.Springer, Berlin, 65-83.https://doi.org/10.1007/978-981-10-1064-4_4
      [35] Wan, Y.S., Liu, S.J., Kröner, A., et al., 2016b.Eastern Ancient Terrane of the North China Craton.Acta Geologica Sinica (English Edition), 90(4):1082-1096. https://doi.org/10.1111/1755-6724.12763
      [36] Wan, Y.S., Xie, S.W., Yang, C.H., et al., 2014.Early Neoarchean (~2.7 Ga) Tectono-Thermal Events in the North China Craton:A Synthesis.Precambrian Research, 247:45-63. https://doi.org/10.1016/j.precamres.2014.03.019
      [37] Wang, S.L., Zhang, R.H., 1995.U-Pb Isotope Age of Individual Zircon from Biotite Leptynite in the Qidashan Iron Deposit and Its Significance.Mineral Deposits, 14(3):216-219 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ503.002.htm
      [38] Williams, I.S., 1998.U-Th-Pb Geochronology by Ion Microprobe.In:Mickibben, M.A., Shanks Ⅲ, W.C., Ridley, W.I., eds., Applications of Microanalytical Techniques to Understanding Mineralizing Processes.Review Econonic Geology, 7:1-35.https://doi.org/10.1080/00241160410006483
      [39] Wu, J.S., Geng, Y.S., Shen, Q.H., et al., 1989.Geological Characteristics and Tectonic Evolution of the Sino Korean Continent.Geological Publishing House, Beijing (in Chinese).
      [40] Yang, F.C., Sun, J.G., Song, Y.H., et al., 2016.SHRIMP U-Pb Age, Hf Isotope Composition and Geochemical Characteristics of Neoarchean Granitic Complex in Liaodong Lianshanguan Area, NE China.Earth Science, 41(12):2008-2018 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.140
      [41] Yang, X.Q., Li, H.M., Xue, C.J., et al., 2013.Geochemical Characteristics of Two Iron Ores from the Waitoushan Iron Deposit, Liaoning Province:Constraints on Ore-Forming Mechanism.Acta Geologica Sinica, 87(10):1580-1592 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201310008.htm
      [42] Zhai, M.G., Santosh, M., 2011.The Early Precambrian Odyssey of the North China Craton:A Synoptic Overview.Gondwana Research, 20(1):6-25. https://doi.org/10.1016/j.gr.2011.02.005
      [43] Zhai, M.G., Windley, B.F., Sills, J.D., 1990.Archaean Gneisses, Amphibolites and Banded Iron-Formations from the Anshan Area of Liaoning Province, NE China:Their Geochemistry, Metamorphism and Petrogenesis.Precambrian Research, 46(3):195-216. https://doi.org/10.1016/0301-9268(90)90002-8
      [44] Zhang, L.C., Dai, Y.P., Wang, C.L., et al., 2014.Age, Material Sources and Formation Setting of Precambrian BIFs Iron Deposits in Anshan-Benxi Area.Journal of Earth Sciences and Environment, 36(4):1-15 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_xagcxyxb201404001
      [45] Zhong, F.D., 1984.Geochronological Study of Archaean Granite-Gneisses in Anshan Area, Northeast China.Geochimica, 13(3):195-205 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX198403000.htm
      [46] Zhu, M.T., Dai, Y.P., Zhang, L.C., et al., 2015.Geochronology and Geochemistry of the Nanfen Iron Deposit in the Anshan-Benxi Area, North China Craton:Implications for~2.55 Ga Crustal Growth and the Genesis of High-Grade Iron Ores.Precambrian Research, 260:23-38. https://doi.org/10.1016/j.precamres.2015.01.001
      [47] 陈毓蔚, 钟富道, 刘菊英, 等, 1981.我国北方前寒武岩石铅同位素年龄测定——兼论中国前寒武地质年表.地球化学, 10(3):209-219. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199500006009.htm
      [48] 程裕淇, 1957.中国东北部辽宁山东等省前震旦纪鞍山式条带状铁矿中富矿的成因问题.地质学报, 31(2):153-180, 241-250. https://www.wenkuxiazai.com/doc/a1a6bb91767f5acfa0c7cd95.html
      [49] 代堰锫, 张连昌, 王长乐, 等, 2012.辽宁本溪歪头山条带状铁矿的成因类型、形成时代及构造背景.岩石学报, 28(11):3574-3594. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201211013&dbname=CJFD&dbcode=CJFQ
      [50] 代堰锫, 张连昌, 朱明田, 等, 2013.鞍山陈台沟BIF铁矿与太古代地壳增生:锆石U-Pb年龄与Hf同位素约束.岩石学报, 29(7):2537-2550. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201307020&dbname=CJFD&dbcode=CJFQ
      [51] 李厚民, 刘明军, 李立兴, 等, 2014.弓长岭铁矿二矿区蚀变岩中锆石SHRIMP U-Pb年龄及地质意义.岩石学报, 30(5):1205-1217. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201405002&dbname=CJFD&dbcode=CJFQ
      [52] 乔广生, 翟明国, 阎月华, 1990.鞍山地区太古代岩石同位素地质年代学研究.地质科学, 25(2):158-165. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkx199002005&dbname=CJFD&dbcode=CJFQ
      [53] 沈保丰, 翟安民, 杨春亮, 等, 2005.中国前寒武纪铁矿床时空分布和演化特征.地质调查与研究, 28(4):196-206. https://www.wenkuxiazai.com/doc/e7292d93f90f76c660371a59.html
      [54] 万渝生, 1993.辽宁弓长岭含铁岩系的形成与演化.北京:北京科学技术出版社.
      [55] 万渝生, 董春艳, 任鹏, 等, 2017.华北克拉通太古宙TTG岩石的时空分布、组成特征及形成演化:综述.岩石学报, 33(5):1405-1419. http://mall.cnki.net/magazine/Article/YSXB201705003.htm
      [56] 万渝生, 董春艳, 颉颃强, 等, 2012.华北克拉通早前寒武纪条带状铁建造形成时代:SHRIMP锆石U-Pb定年.地质学报, 86(9):1447-1478. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzxe201209010&dbname=CJFD&dbcode=CJFQ
      [57] 万渝生, 耿元生, 沈其韩, 等, 2002.鞍山中太古代铁架山花岗岩中表壳岩包体的地球化学特征及地质意义.地质科学, 37(2):143-151, 164. doi: 10.3321/j.issn:0563-5020.2002.02.002
      [58] 万渝生, 刘敦一, 1993.辽宁弓长岭中太古代片麻岩和铬云母石英岩的锆石年龄.地质论评, 39(2):124-129. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzlp199302004&dbname=CJFD&dbcode=CJFQ
      [59] 王守伦, 张瑞华, 1995.齐大山铁矿黑云母变粒岩单锆石年龄及意义.矿床地质, 14(3):216-219. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ201301005014.htm
      [60] 伍家善, 耿元生, 沈其韩, 等, 1989.中朝古大陆的地质特征及构造演化.北京:地质出版社.
      [61] 杨凤超, 孙景贵, 宋运红, 等, 2016.辽东连山关地区新太古代花岗杂岩SHRIMP U-Pb年龄、Hf同位素组成及地质意义.地球科学, 41(12):2008-2018. http://www.earth-science.net/WebPage/Article.aspx?id=3397
      [62] 杨秀清, 李厚民, 薛春纪, 等, 2013.辽宁歪头山铁矿两类矿石地球化学特征及其对成矿作用的制约.地质学报, 87(10):1580-1592. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzxe201310008&dbname=CJFD&dbcode=CJFQ
      [63] 张连昌, 代堰锫, 王长乐, 等, 2014.鞍山-本溪地区前寒武纪条带状铁建造铁矿时代、物质来源与形成环境.地球科学与环境学报, 36(4):1-15. https://www.wenkuxiazai.com/doc/d07a7a588bd63186bdebbc58.html
      [64] 钟富道, 1984.鞍山铁甲山花岗片麻岩同位素年代学研究.地球化学, 13(3):195-205. http://www.cnki.com.cn/Article/CJFDTotal-HSDZ200004000.htm
    • 加载中
    图(12) / 表(2)
    计量
    • 文章访问数:  5075
    • HTML全文浏览量:  1661
    • PDF下载量:  64
    • 被引次数: 0
    出版历程
    • 收稿日期:  2017-06-28
    • 刊出日期:  2018-01-15

    目录

      /

      返回文章
      返回