华北克拉通宣龙式铁矿锆石U-Pb年龄及其对矿床成因的制约

张旭升, 杨秀清, 赵军, 梁婷, 杨云, 梁永生, 杨国威, 王晓青. 2023. 华北克拉通宣龙式铁矿锆石U-Pb年龄及其对矿床成因的制约. 地质通报, 42(1): 55-67. doi: 10.12097/j.issn.1671-2552.2023.01.005
引用本文: 张旭升, 杨秀清, 赵军, 梁婷, 杨云, 梁永生, 杨国威, 王晓青. 2023. 华北克拉通宣龙式铁矿锆石U-Pb年龄及其对矿床成因的制约. 地质通报, 42(1): 55-67. doi: 10.12097/j.issn.1671-2552.2023.01.005
ZHANG Xusheng, YANG Xiuqing, ZHAO Jun, LIANG Ting, YANG Yun, LIANG Yongsheng, YANG Guowei, WANG Xiaoqing. 2023. Zircon U-Pb age of Xuanlong-type iron deposits in North China Craton and its constraints on genesis. Geological Bulletin of China, 42(1): 55-67. doi: 10.12097/j.issn.1671-2552.2023.01.005
Citation: ZHANG Xusheng, YANG Xiuqing, ZHAO Jun, LIANG Ting, YANG Yun, LIANG Yongsheng, YANG Guowei, WANG Xiaoqing. 2023. Zircon U-Pb age of Xuanlong-type iron deposits in North China Craton and its constraints on genesis. Geological Bulletin of China, 42(1): 55-67. doi: 10.12097/j.issn.1671-2552.2023.01.005

华北克拉通宣龙式铁矿锆石U-Pb年龄及其对矿床成因的制约

  • 基金项目:
    陕西省自然科学基础研究计划项目《华北克拉通北部宣龙式铁矿成因及沉积环境研究》(编号: 2020JM-213)、国家自然科学基金《北祁连元古宙中期卡瓦条带状铁建造成因机制》(批准号: 41972075)、长安大学中央高校基本科研业务费专项资金资助(编号: 300102272203)
详细信息
    作者简介: 张旭升(1997-), 男, 在读硕士生, 矿物学、岩石学、矿床学专业。E-mail: 191545706@qq.com
    通讯作者: 杨秀清(1987-), 男, 副教授, 从事金属矿床成矿作用研究。E-mail: xiuqing2008@126.com
  • 中图分类号: P611;P597+3

Zircon U-Pb age of Xuanlong-type iron deposits in North China Craton and its constraints on genesis

More Information
  • 华北克拉通宣龙式铁矿是中国北方最重要的沉积型铁矿类型,形成于元古宙中期(1800~800Ma)。河北大岭堡地区鲕状赤铁矿石发育大量碎屑锆石,对这些碎屑锆石及庞家堡地区侵入串岭沟组的花岗岩脉进行了LA-ICP-MS锆石U-Pb年龄分析。鲕状赤铁矿石碎屑锆石获得了2组主要的峰值年龄,分别为1873Ma和2530Ma,记录了华北克拉通约1850Ma和约2500Ma两次构造热事件,结合前人研究,表明其与围岩具有基本一致的碎屑锆石源区,与北京十三陵地区串岭沟组源区略有差异,推测宣龙式铁矿可能为华北克拉通响应Columbia超大陆裂解的产物。花岗岩脉锆石U-Pb年龄为202.3±1.4Ma(n=27,MSWD=0.96),表明区内发育印支期岩浆侵入活动,暗示磁铁矿石可能并非前人认为的燕山期的产物,其成因还需要进一步深入研究。

  • 加载中
  • 图 1  宣龙式铁矿区域地质背景

    Figure 1. 

    图 图版Ⅰ   

    图 2  锆石阴极发光(CL)图像(图中白色圈为束斑大小,年龄单位为Ma)

    Figure 2. 

    图 3  锆石U-Pb年龄谐和图

    Figure 3. 

    图 4  串岭沟组锆石U-Pb年龄概率分布

    Figure 4. 

    表 1  大岭堡鲕状赤铁矿石LA-ICP-MS碎屑锆石U-Th-Pb分析结果

    Table 1.  LA-ICP-MS U-Th-Pb dating results of detrital zircons from the Dalingbu oolitic hematite ores

    点号 含量/10-6 Th/U 同位素比值 年龄/Ma
    204Pb 232Th 238U 207Pb/206Pb± 207Pb/235 206Pb/U238± 208Pb/232Th± 207Pb/206Pb± 207Pb/235 206Pb/238 208/Pb/232Th±
    DLB-1-01 7.54 207.2 981.61 0.21 0.1297 0.00263 6.10367 0.06389 0.34125 0.00344 0.10113 0.00103 2093.9 35.22 1990.8 9.13 1892.7 16.53 1947.2 18.87
    DLB-1-02 < 1.02 187.57 146.69 1.28 0.11375 0.00233 5.24236 0.05689 0.3342 0.00339 0.10167 0.00093 1860.1 36.55 1859.5 9.25 1858.7 16.4 1957.1 17.1
    DLB-1-03 1.87 113.7 174.51 0.65 0.12187 0.00252 5.4377 0.06063 0.32355 0.00331 0.1148 0.00111 1983.7 36.28 1890.8 9.56 1807.1 16.14 2196.6 20.07
    DLB-1-04 2.28 202.01 234.71 0.86 0.11312 0.00232 3.20294 0.03451 0.20531 0.00207 0.06005 0.00056 1850.2 36.58 1457.9 8.34 1203.8 11.1 1178.7 10.6
    DLB-1-05 1.25 16.78 21.21 0.79 0.10855 0.00254 4.7444 0.0744 0.31694 0.0036 0.09834 0.00123 1775.2 42.08 1775.1 13.15 1774.8 17.64 1895.9 22.65
    DLB-1-06 < 1.12 25.48 74.77 0.34 0.16948 0.00347 11.35351 0.12294 0.48579 0.00499 0.14573 0.00155 2552.5 33.86 2552.6 10.1 2552.4 21.66 2749.7 27.29
    DLB-1-07 < 1.48 50.59 135.49 0.37 0.11499 0.00237 5.34251 0.05848 0.33692 0.00343 0.10075 0.00102 1879.7 36.62 1875.7 9.36 1871.9 16.55 1940.3 18.67
    DLB-1-08 < 1.29 22.77 36.77 0.62 0.11108 0.0025 4.96974 0.07112 0.32442 0.00358 0.10135 0.00124 1817.2 40.3 1814.2 12.1 1811.3 17.41 1951.2 22.8
    DLB-1-09 < 1.15 101.5 146.3 0.69 0.17009 0.00347 11.42612 0.12166 0.48713 0.00497 0.15722 0.00148 2558.5 33.76 2558.6 9.94 2558.2 21.55 2951.5 25.92
    DLB-1-10 < 1.16 48.69 37.88 1.29 0.12817 0.00276 6.59203 0.08365 0.37295 0.004 0.11182 0.00113 2073.1 37.41 2058.3 11.19 2043.3 18.8 2142.4 20.51
    DLB-1-11 1.01 74.17 143.79 0.52 0.11661 0.0024 5.51865 0.06017 0.34319 0.0035 0.10427 0.00101 1904.9 36.51 1903.5 9.37 1902 16.77 2004.7 18.46
    DLB-1-12 1.03 70.79 78.35 0.9 0.16783 0.00345 11.21694 0.12237 0.48467 0.00499 0.14094 0.00134 2536.1 34.06 2541.3 10.17 2547.6 21.68 2665 23.79
    DLB-1-13 < 0.98 84.52 83.64 1.01 0.12485 0.0026 6.28619 0.07124 0.36511 0.00377 0.10725 0.00102 2026.7 36.39 2016.5 9.93 2006.3 17.8 2059.2 18.67
    DLB-1-14 < 1.04 80.15 93.54 0.86 0.16816 0.00344 11.22525 0.12056 0.48407 0.00495 0.13924 0.00131 2539.4 33.95 2542 10.01 2545 21.52 2634.9 23.2
    DLB-1-15 1.24 189.88 161.56 1.18 0.11526 0.00237 5.39789 0.05862 0.3396 0.00346 0.10225 0.00093 1884 36.61 1884.5 9.3 1884.7 16.63 1967.7 17.13
    DLB-1-16 1.78 100.55 69.15 1.45 0.16112 0.00334 10.30068 0.1149 0.4636 0.00481 0.13626 0.00127 2467.4 34.54 2462.2 10.32 2455.4 21.19 2582 22.64
    DLB-1-17 1.42 117.95 251 0.47 0.16409 0.00334 9.73452 0.10159 0.4302 0.00435 0.13647 0.00127 2498.2 33.89 2410 9.61 2306.6 19.6 2585.6 22.52
    DLB-1-18 < 1.08 111.9 127.06 0.88 0.11437 0.00237 5.28981 0.05848 0.3354 0.00343 0.10069 0.00094 1869.9 36.88 1867.2 9.44 1864.5 16.55 1939 17.29
    DLB-1-19 3.76 200.74 806.72 0.25 0.15831 0.00324 3.54981 0.03724 0.16259 0.00164 0.03092 0.00031 2437.7 34.23 1538.4 8.31 971.2 9.1 615.6 6.09
    DLB-1-20 < 1.38 128.69 129.15 1 0.12022 0.00249 5.81465 0.06395 0.35073 0.00359 0.10307 0.00095 1959.4 36.48 1948.6 9.53 1938.1 17.12 1982.7 17.5
    DLB-1-21 1.76 34.79 61.83 0.56 0.16808 0.00349 11.21597 0.12579 0.48387 0.00504 0.13987 0.00143 2538.6 34.41 2541.2 10.46 2544.1 21.9 2646.1 25.42
    DLB-1-22 1.47 104.61 141.96 0.74 0.11507 0.00238 5.3613 0.05883 0.33783 0.00345 0.10167 0.00095 1881 36.82 1878.7 9.39 1876.2 16.62 1957.2 17.47
    DLB-1-23 < 1.19 96.62 87.06 1.11 0.16967 0.0035 11.389 0.12421 0.48674 0.00501 0.13786 0.00128 2554.4 34.14 2555.5 10.18 2556.6 21.73 2610.4 22.8
    DLB-1-24 1.4 81.64 105.12 0.78 0.11573 0.00242 5.40938 0.06128 0.33892 0.00349 0.0998 0.00096 1891.3 37.12 1886.3 9.71 1881.5 16.81 1922.7 17.59
    DLB-1-25 < 1.35 79.79 67.22 1.19 0.11439 0.00243 5.33418 0.06369 0.33813 0.00353 0.0995 0.00095 1870.3 37.81 1874.4 10.21 1877.7 17.02 1917.3 17.54
    DLB-1-26 < 1.21 120.35 75.76 1.59 0.12444 0.00264 6.24731 0.07417 0.36402 0.00382 0.10637 0.001 2020.8 37.11 2011.1 10.39 2001.2 18.03 2043.2 18.3
    DLB-1-27 < 1.12 197.75 201.52 0.98 0.11493 0.00237 5.38027 0.05823 0.33943 0.00345 0.1003 0.00091 1878.8 36.76 1881.7 9.27 1883.9 16.63 1931.9 16.78
    DLB-1-28 < 1.22 21.8 36.28 0.6 0.10952 0.00244 4.77402 0.06536 0.31607 0.00343 0.09624 0.00113 1791.4 40.02 1780.3 11.49 1770.5 16.81 1857.2 20.75
    DLB-1-29 < 1.21 36 87.87 0.41 0.17649 0.00365 12.2693 0.13418 0.50407 0.0052 0.14401 0.00147 2620.1 34 2625.2 10.27 2631.3 22.3 2719.3 25.9
    DLB-1-30 < 1.21 26.49 52.93 0.5 0.11076 0.00239 4.98142 0.06238 0.3261 0.00345 0.09504 0.00106 1811.9 38.7 1816.2 10.59 1819.5 16.77 1835.2 19.57
    DLB-1-31 1.24 21.26 57.39 0.37 0.11383 0.00246 5.25841 0.06562 0.33494 0.00355 0.09731 0.00116 1861.5 38.46 1862.1 10.65 1862.3 17.13 1876.9 21.34
    DLB-1-32 < 1.14 63.19 77.98 0.81 0.11335 0.00241 5.07907 0.0605 0.32488 0.00339 0.0951 0.00094 1853.8 37.96 1832.6 10.11 1813.5 16.51 1836.1 17.31
    DLB-1-33 < 0.97 82.14 43.96 1.87 0.11483 0.00252 5.31308 0.06977 0.33548 0.00361 0.09783 0.00094 1877.2 39.06 1871 11.22 1864.9 17.44 1886.5 17.39
    DLB-1-34 1.26 93.97 129.75 0.72 0.11673 0.00244 5.55652 0.062 0.34514 0.00354 0.10015 0.00094 1906.7 37.03 1909.4 9.6 1911.3 16.99 1929.2 17.36
    DLB-1-35 < 1.33 45.41 46.01 0.99 0.11245 0.00249 4.87211 0.06502 0.31413 0.00339 0.09082 0.00095 1839.4 39.5 1797.4 11.24 1761 16.63 1757.1 17.65
    DLB-1-36 < 1.10 74.63 166.91 0.45 0.11985 0.0025 5.839 0.06468 0.35324 0.00362 0.10275 0.001 1953.9 36.75 1952.2 9.6 1950.1 17.26 1976.9 18.35
    DLB-1-37 < 1.12 191.41 49.28 3.88 0.16401 0.00339 10.42798 0.12004 0.46128 0.00493 0.11817 0.001 2497.4 34.38 2473.5 10.67 2445.2 21.77 2257.6 18.07
    DLB-1-38 < 0.78 25.78 31.67 0.81 0.10908 0.00241 4.78065 0.0665 0.31795 0.00353 0.08693 0.00093 1784.1 39.8 1781.5 11.68 1779.7 17.26 1684.9 17.3
    DLB-1-39 < 1.03 118.89 104.08 1.14 0.16645 0.00339 11.12306 0.12116 0.48479 0.00508 0.12562 0.00109 2522.3 33.79 2533.5 10.15 2548.1 22.04 2391.9 19.57
    DLB-1-40 < 1.00 24.35 98.69 0.25 0.12411 0.00256 6.25036 0.07137 0.36537 0.00385 0.09708 0.00107 2016.1 36.2 2011.5 10 2007.6 18.19 1872.7 19.67
    DLB-1-41 < 1.48 175.61 184.86 0.95 0.16759 0.00343 9.04396 0.10056 0.39149 0.00412 0.11794 0.00105 2533.8 33.96 2342.5 10.17 2129.7 19.1 2253.4 19.03
    DLB-1-42 1.65 102.28 127.77 0.8 0.16579 0.00336 10.86621 0.11689 0.47548 0.00495 0.12611 0.00111 2515.6 33.71 2511.7 10 2507.6 21.64 2400.6 19.84
    DLB-1-43 < 1.01 22.24 39.59 0.56 0.15998 0.00334 9.55104 0.11348 0.4331 0.00468 0.10843 0.00115 2455.5 34.86 2392.5 10.92 2319.7 21.04 2080.7 21.01
    DLB-1-44 < 1.14 21.46 67.1 0.32 0.12318 0.00257 6.19409 0.07327 0.36479 0.00388 0.09624 0.00108 2002.8 36.61 2003.6 10.34 2004.8 18.34 1857.2 19.95
    DLB-1-45 < 1.00 51.72 113.96 0.45 0.1137 0.00235 5.28537 0.06014 0.33722 0.00354 0.09162 0.00089 1859.4 36.83 1866.5 9.72 1873.3 17.06 1771.9 16.46
    DLB-1-46 < 1.09 33.62 43.05 0.78 0.10833 0.00236 4.69926 0.06266 0.31467 0.00344 0.08328 0.00088 1771.5 39.27 1767.1 11.16 1763.7 16.87 1616.8 16.4
    DLB-1-47 < 1.28 162.97 180.67 0.9 0.16718 0.00338 11.22795 0.11919 0.4872 0.00505 0.12781 0.00111 2529.6 33.56 2542.2 9.9 2558.5 21.87 2431.1 19.87
    DLB-1-48 < 1.06 210.38 138.43 1.52 0.12347 0.00253 6.14923 0.06852 0.36128 0.00378 0.09698 0.00085 2007 35.97 1997.3 9.73 1988.2 17.88 1870.8 15.59
    DLB-1-49 1.35 89.01 89.23 1 0.16164 0.00332 10.4559 0.117 0.46923 0.00495 0.12438 0.00114 2472.9 34.21 2476 10.37 2480.2 21.73 2369.5 20.56
    DLB-1-50 < 1.00 47.83 130.36 0.37 0.12184 0.0025 6.09739 0.06802 0.36301 0.00379 0.10106 0.001 1983.3 36.07 1989.9 9.73 1996.4 17.93 1945.9 18.38
    DLB-1-51 < 0.92 23.48 39.9 0.59 0.109 0.00274 4.59411 0.08477 0.30572 0.00379 0.08435 0.00134 1782.8 45.24 1748.2 15.39 1719.6 18.71 1636.8 24.95
    DLB-1-52 < 1.08 133.07 130.61 1.02 0.16788 0.00342 11.12641 0.12122 0.48074 0.00502 0.12935 0.00116 2536.6 33.76 2533.8 10.15 2530.5 21.87 2458.7 20.83
    DLB-1-53 < 1.02 65.5 142.96 0.46 0.11647 0.00238 5.43957 0.05993 0.33878 0.00352 0.09695 0.00091 1902.7 36.31 1891.1 9.45 1880.8 16.95 1870.4 16.85
    DLB-1-54 < 1.13 137.38 154.1 0.89 0.11816 0.00242 5.67031 0.06318 0.34808 0.00363 0.09709 0.00088 1928.6 36.31 1926.9 9.62 1925.4 17.35 1872.9 16.25
    DLB-1-55 < 0.99 36.57 59.02 0.62 0.11387 0.0024 5.26728 0.06367 0.33551 0.00357 0.09329 0.00095 1862.1 37.51 1863.6 10.32 1865 17.24 1802.8 17.61
    DLB-1-56 1.29 8.71 213.01 0.04 0.11535 0.00235 5.41295 0.05898 0.34039 0.00352 0.07511 0.00127 1885.3 36.28 1886.9 9.34 1888.5 16.95 1463.9 23.78
    DLB-1-57 0.97 60.36 145.36 0.42 0.18056 0.00366 12.66076 0.13492 0.50859 0.00527 0.12603 0.0012 2658 33.18 2654.7 10.03 2650.6 22.53 2399.2 21.51
    DLB-1-58 < 1.04 72.71 162.26 0.45 0.16161 0.00328 10.26112 0.10966 0.46051 0.00477 0.13281 0.00124 2472.6 33.82 2458.6 9.89 2441.8 21.05 2520.5 22.17
    DLB-1-59 < 1.14 15.33 25.92 0.59 0.11312 0.00263 5.09366 0.08026 0.32661 0.0038 0.09111 0.00125 1850.1 41.53 1835 13.37 1821.9 18.46 1762.3 23.2
    DLB-1-60 < 1.07 31.34 62.89 0.5 0.11015 0.00235 4.94568 0.06265 0.32566 0.00351 0.09211 0.00103 1801.8 38.38 1810.1 10.7 1817.3 17.05 1780.9 19.11
    DLB-1-61 1.24 48.78 130.45 0.37 0.11775 0.00244 5.43015 0.06205 0.33447 0.0035 0.0971 0.00101 1922.4 36.62 1889.6 9.8 1860 16.93 1873 18.66
    DLB-1-62 < 1.46 42.07 51.26 0.82 0.11577 0.00249 5.39378 0.06996 0.3379 0.00367 0.09565 0.00102 1891.9 38.27 1883.9 11.11 1876.6 17.7 1846.4 18.73
    DLB-1-63 < 0.99 23.88 54.18 0.44 0.10772 0.00231 4.70383 0.05992 0.31671 0.00341 0.0914 0.00106 1761.2 38.64 1767.9 10.67 1773.6 16.67 1767.8 19.59
    DLB-1-64 < 1.01 146.46 135.22 1.08 0.16714 0.00339 11.27171 0.12048 0.48911 0.00506 0.13152 0.00119 2529.2 33.63 2545.9 9.97 2566.8 21.92 2497.5 21.31
    DLB-1-65 < 1.05 13.18 16.07 0.82 0.11262 0.0027 5.07427 0.08494 0.32676 0.00386 0.09234 0.00122 1842.2 42.75 1831.8 14.2 1822.6 18.77 1785.3 22.52
    DLB-1-66 2.89 243.93 400.87 0.61 0.15736 0.00318 6.34601 0.06643 0.29248 0.003 0.09847 0.00089 2427.5 33.83 2024.8 9.18 1653.9 14.94 1898.4 16.33
    DLB-1-67 3.23 91.92 681.34 0.13 0.11435 0.00232 2.09822 0.02227 0.13308 0.00136 0.05801 0.00057 1869.6 36.14 1148.2 7.3 805.4 7.75 1139.7 10.89
    DLB-1-68 < 0.80 85.52 166.34 0.51 0.11829 0.00241 5.61018 0.06048 0.34395 0.00354 0.09992 0.00094 1930.6 35.99 1917.7 9.29 1905.7 17 1924.9 17.3
    DLB-1-69 < 1.00 28.59 43.48 0.66 0.16445 0.00343 10.74174 0.12791 0.47371 0.00512 0.13611 0.00147 2501.9 34.72 2501 11.06 2499.8 22.39 2579.3 26.17
    DLB-1-70 < 1.19 62.39 210.58 0.3 0.11281 0.00229 5.19131 0.05571 0.33373 0.00343 0.10019 0.00098 1845.1 36.33 1851.2 9.14 1856.5 16.58 1929.8 17.98
    DLB-1-71 0.85 95.54 206.62 0.46 0.11372 0.00232 5.31421 0.05747 0.33888 0.00349 0.10073 0.00096 1859.7 36.34 1871.2 9.24 1881.3 16.81 1939.8 17.67
    DLB-1-72 0.89 127.6 103.71 1.23 0.11405 0.00234 5.26654 0.05884 0.33487 0.00348 0.09919 0.00092 1864.9 36.65 1863.5 9.53 1861.9 16.79 1911.5 16.92
    DLB-1-73 < 0.62 52.17 106.45 0.49 0.11515 0.0024 5.23115 0.06158 0.32945 0.00347 0.09852 0.00105 1882.2 37.14 1857.7 10.03 1835.7 16.82 1899.2 19.28
    DLB-1-74 < 1.13 56.77 63.32 0.9 0.16757 0.00354 10.97485 0.13543 0.47494 0.00522 0.1404 0.00152 2533.5 34.97 2521 11.48 2505.2 22.8 2655.4 26.91
    DLB-1-75 < 0.79 93 101.71 0.91 0.11757 0.00242 5.60564 0.06281 0.34574 0.00359 0.1029 0.00098 1919.6 36.44 1917 9.65 1914.2 17.21 1979.7 18.05
    DLB-1-76 < 1.30 68.51 217.93 0.31 0.11611 0.00239 4.08081 0.04589 0.25486 0.00264 0.08478 0.0009 1897.2 36.61 1650.5 9.17 1463.5 13.57 1644.8 16.68
    DLB-1-77 < 0.80 163.03 201.74 0.81 0.11441 0.00234 5.36104 0.05847 0.3398 0.0035 0.10052 0.00095 1870.6 36.39 1878.7 9.33 1885.7 16.85 1936 17.48
    DLB-1-78 < 0.97 78.61 94.78 0.83 0.12239 0.00252 6.11826 0.06907 0.36249 0.00378 0.10728 0.00105 1991.3 36.21 1992.9 9.85 1994 17.88 2059.7 19.15
    下载: 导出CSV

    表 2  庞家堡地区花岗岩脉锆石LA-ICP-MS U-Th-Pb分析结果

    Table 2.  LA-ICP-MS U-Th-Pb analysed results of zircons from the granite vein in the Pangjiabu area

    点号 含量/10-6 Th/U 同位素比值 年龄/Ma
    204Pb 232Th 238U 207Pb/206Pb± 207Pb/235 206Pb/U238± 208Pb/232Th± 207Pb/206Pb± 207Pb/235 206Pb/238 208/Pb/232Th±
    PJB-11-01 < 1.05 567.8 295.55 1.92 0.0507 0.00141 0.21821 0.0046 0.03122 0.00033 0.0094 0.00009 227.2 63.12 200.4 3.83 198.2 2.07 189.2 1.87
    PJB-11-02 1.26 343.14 231.08 1.48 0.05115 0.00141 0.2208 0.00455 0.03131 0.00033 0.00969 0.0001 247.8 62.08 202.6 3.79 198.7 2.06 195 1.98
    PJB-11-03 < 1.05 149.67 126.44 1.18 0.04846 0.0016 0.20771 0.00567 0.03109 0.00034 0.00978 0.00012 121.7 75.79 191.6 4.77 197.3 2.14 196.8 2.31
    PJB-11-04 < 1.07 231.34 185.21 1.25 0.05178 0.00153 0.22634 0.00527 0.0317 0.00034 0.0108 0.00012 275.8 66.41 207.2 4.36 201.2 2.15 217.1 2.39
    PJB-11-05 2.3 323.13 251.59 1.28 0.05181 0.00148 0.22781 0.00502 0.03189 0.00034 0.00989 0.00011 277.2 64.15 208.4 4.15 202.3 2.13 198.9 2.14
    PJB-11-06 < 1.21 324.53 213.02 1.52 0.05217 0.00138 0.22932 0.00441 0.03188 0.00033 0.01003 0.0001 292.9 59.1 209.6 3.64 202.3 2.08 201.7 2
    PJB-11-07 < 1.19 227.83 176.64 1.29 0.05208 0.00165 0.22832 0.00591 0.03179 0.00036 0.01013 0.00012 289.1 70.89 208.8 4.88 201.8 2.23 203.7 2.41
    PJB-11-08 < 1.51 451.22 252.42 1.79 0.05112 0.00198 0.21908 0.00742 0.03108 0.00038 0.00935 0.00012 246.4 86.96 201.1 6.18 197.3 2.38 188.1 2.4
    PJB-11-09 3.07 61.96 79.66 0.78 0.05098 0.00268 0.22806 0.0111 0.03244 0.00047 0.01119 0.00024 239.9 116.88 208.6 9.18 205.8 2.91 224.9 4.85
    PJB-11-10 < 1.23 149.63 138.11 1.08 0.05146 0.00167 0.22413 0.00598 0.03159 0.00035 0.01032 0.00013 261.4 72.71 205.3 4.96 200.5 2.21 207.5 2.55
    PJB-11-12 < 0.81 249.67 121.49 2.06 0.05103 0.00214 0.21936 0.00819 0.03117 0.0004 0.01041 0.00013 242.1 93.9 201.4 6.82 197.9 2.48 209.4 2.64
    PJB-11-13 < 1.35 177.09 161.58 1.1 0.05029 0.00161 0.2205 0.0058 0.03179 0.00036 0.01054 0.00013 208.6 72.69 202.3 4.83 201.7 2.22 212 2.57
    PJB-11-14 < 0.89 153.63 128.62 1.19 0.05023 0.00211 0.21786 0.00814 0.03145 0.0004 0.01053 0.00016 205.5 94.52 200.1 6.79 199.6 2.5 211.8 3.16
    PJB-11-15 < 0.93 122.91 107.14 1.15 0.0529 0.0018 0.23343 0.00668 0.03199 0.00037 0.0104 0.00013 324.6 75.51 213 5.5 203 2.31 209.2 2.7
    PJB-11-17 < 1.10 149.92 118.35 1.27 0.05153 0.00192 0.22824 0.00736 0.03212 0.00038 0.0103 0.00014 264.5 83.29 208.7 6.09 203.8 2.4 207.2 2.78
    PJB-11-18 < 1.18 300.95 185.05 1.63 0.05112 0.00142 0.22268 0.00468 0.03159 0.00034 0.00981 0.0001 246 62.53 204.1 3.89 200.5 2.1 197.2 2.02
    PJB-11-19 < 1.34 208.47 147.41 1.41 0.05121 0.00159 0.22347 0.00564 0.03164 0.00035 0.01037 0.00012 250.1 70.08 204.8 4.68 200.8 2.2 208.5 2.35
    PJB-11-21 1.4 252.74 151.37 1.67 0.05141 0.00155 0.22398 0.00539 0.03159 0.00035 0.01003 0.00011 259.4 67.78 205.2 4.47 200.5 2.18 201.8 2.18
    PJB-11-22 < 1.28 108.3 102.94 1.05 0.05007 0.00169 0.22155 0.00628 0.03208 0.00036 0.01019 0.00013 198.2 76.53 203.2 5.22 203.6 2.26 204.9 2.59
    PJB-11-23 < 1.17 171.06 128.47 1.33 0.05435 0.00188 0.23549 0.00689 0.03141 0.00037 0.0101 0.00013 385.6 75.17 214.7 5.66 199.4 2.29 203.1 2.56
    PJB-11-24 < 1.11 162.15 124.21 1.31 0.04894 0.00157 0.21716 0.00573 0.03217 0.00036 0.00999 0.00012 144.7 73.4 199.5 4.78 204.1 2.23 200.8 2.32
    PJB-11-25 < 1.13 207.02 179.36 1.15 0.05089 0.00143 0.22109 0.00478 0.0315 0.00034 0.01027 0.00011 235.8 63.58 202.8 3.97 199.9 2.12 206.6 2.28
    PJB-11-26 < 0.98 215.6 162.16 1.33 0.05068 0.00144 0.22441 0.00492 0.0321 0.00035 0.01047 0.00011 226.2 64.22 205.6 4.08 203.7 2.16 210.6 2.27
    PJB-11-27 < 1.17 407.42 236.34 1.72 0.05115 0.00136 0.22547 0.00446 0.03196 0.00034 0.01019 0.0001 247.5 60.23 206.5 3.69 202.8 2.12 205 2.06
    PJB-11-28 < 1.25 164.77 132.17 1.25 0.05127 0.00155 0.22553 0.00545 0.03189 0.00035 0.0103 0.00012 253 67.9 206.5 4.51 202.4 2.21 207.1 2.4
    PJB-11-29 < 1.29 251.28 192.2 1.31 0.04879 0.00133 0.21626 0.00447 0.03213 0.00034 0.01039 0.00011 137.8 62.92 198.8 3.73 203.9 2.14 209 2.18
    PJB-11-30 1.08 444.53 253.99 1.75 0.05202 0.00139 0.22615 0.00451 0.03152 0.00034 0.00996 0.0001 286.5 60.04 207 3.73 200 2.11 200.4 2.06
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  • [1]

    Bekker A, Planavsky N, Krapež B, et al. Iron formations: their origins and implications for ancient seawater chemistry[J]. Elsevier, 2014, 9: 561-628.

    [2]

    Canfield D E. A new model for Proterozoic ocean chemistry[J]. Nature, 1998, 396: 450-453. doi: 10.1038/24839

    [3]

    Cox G M, Halverson G P, Minarik W G, et al. Neoproterozoic iron formation: An evaluation of its temporal, environmental and tectonic significance[J]. Chemical Geology, 2013, 362: 232-249. doi: 10.1016/j.chemgeo.2013.08.002

    [4]

    Ding J, Shi Y, Kröner A, et al. Constraints on sedimentary ages of the Chuanlinggou formation in the Ming Tombs, Beijing, North China Craton: LA-ICP-MS and SHRIMP U-Pb dating of detrital zircons[J]. Acta Geochimica, 2018, 37: 1-24. doi: 10.1007/s11631-017-0179-x

    [5]

    Duan C, Li Y H, Yang Y, et al. U-Pb ages and Hf isotopes of detrital zircon grains from the Mesoproterozoic Chuanlinggou Formation in North China Craton: Implications for the geochronology of sedimentary iron deposits and crustal evolution[J]. Minerals, 2018, 8: 547.

    [6]

    Holland H. The chemical evolution of the atmosphere and oceans[M]. New York, Princeton University Press, 1984: 582.

    [7]

    Hoskin P W, Schaltegger U. The composition of zircon and ignous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochenistry, 2003, 53(1): 27-62. doi: 10.2113/0530027

    [8]

    Johnson C M, Beard B L, Klein C, et al. Iron isotopes constrain biologic and abiologic processes in banded iron formation genesis[J]. Geochimica et Cosmochimica Acta, 2008, 72: 151-169. doi: 10.1016/j.gca.2007.10.013

    [9]

    Konhauser K O, Planavsky N J, Hardisty D S, et al. Iron formations: a global record of Neoarchaean to Palaeoproterozoic environmental history[J]. Earth-Science Reviews, 2017, 172: 140-177. doi: 10.1016/j.earscirev.2017.06.012

    [10]

    Kusky T M, Li J. Paleoproterozoic tectonic evolution of the North China Craton[J]. Journal of Asian Earth Science, 2003, 22(4): 383-397. doi: 10.1016/S1367-9120(03)00071-3

    [11]

    Kusky T M, Santosh M. The Columbia connection in North China[J]. Geological Society London Special Publications, 2009, 323(1): 49-71. doi: 10.1144/SP323.3

    [12]

    Lin Y T, Tang D J, Shi X Y, et al. Shallow-marine ironstones formed by microaerophilic iron-oxidizing bacteria in terminal Paleoproterozoic[J]. Gondwana Research, 2019, 76: 1-18. doi: 10.1016/j.gr.2019.06.004

    [13]

    Lu S N, Zhao G C, Wang H M, et al. Precambrian metamorphic basement and sedimentary cover of the North China Craton: A review[J]. Precambrian Research, 2008, 160(1/2): 77-93.

    [14]

    Rahiminejad A H, Zand-Moghadam H. Synsedimentary formation of ooidal iron stone: An example from the Jurassic deposits of SE central Iran[J]. Ore Geology Reviews, 2018, 95: 238-257. doi: 10.1016/j.oregeorev.2018.02.028

    [15]

    Ramanaidou E R, Wells M A. 13.13-sedimentary hosted iron ores[J]. Treatise on Geochemistry, 2014, 13: 313-355.

    [16]

    Van Houten F B, Arthur M A. Temporal patterns among Phanerozoic oolitic ironstones and oceanic anoxia[J]. Geological Society Special Publication, 1989, 46: 33-49. doi: 10.1144/GSL.SP.1989.046.01.06

    [17]

    Xu D R, Wang Z L, Chen H Y, et al. Petrography and geochemistry of the Shilu Fe-Co-Cu ore district, South China: Implications for the origin of a Neoproterozoic BIF system[J]. Ore Geology Reviews, 2014, 57: 322-350. doi: 10.1016/j.oregeorev.2013.08.011

    [18]

    Young T P. Phanerozoic ironstones: an introduction and review[C]//Young T P, Taylor W E G. Phanerozoic Ironstones. Special Publication, Geological Society of London, 1989, 46: ix-xxv.

    [19]

    Yuan H L, Gao S, Dai M N et al. Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon by excimer laser ablation quadrupole and multiple collector ICP-MS[J]. Chemical Geology, 2008, 247: 100-117. doi: 10.1016/j.chemgeo.2007.10.003

    [20]

    Zhai M G, Bian A G, Zhao T P. The amalgamation of the supercontinent of North China Craton at the end of Neo-Archaean and its breakup during late Palaeoproterozoic and Meso-Proterozoic[J]. Science in China(Series D), 2000, 30(S1): 219-232.

    [21]

    陈志明, 于洁, 侯奎. 冀西北宣龙地区菱铁矿的成因[J]. 地质科学, 1982, 4: 395-420. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198204006.htm

    [22]

    戴永定, 宋海明, 沈继英. 河北宣龙铁矿化石细菌[J]. 中国科学(D辑), 2003, 33(8): 751-759. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200308005.htm

    [23]

    杜汝霖, 胡华斌, 刘志礼, 等. 冀西北长城系宣龙式铁矿生物成矿作用[M]. 北京: 科学出版社, 1999: 1-160.

    [24]

    段超, 李延河, 魏明辉, 等. 河北宣化姜家寨铁矿床串岭沟组底部碎屑锆石LA-MC-ICP-MS U-Pb年龄及其地质意义[J]. 岩石学报, 2014, 30(1): 35-48. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201401003.htm

    [25]

    高林志, 张传恒, 刘鹏举, 等. 华北-江南地区中、新元古代地层格架的再认识[J]. 地球学报, 2009, 30(4): 433-446. doi: 10.3321/j.issn:1006-3021.2009.04.004

    [26]

    高维, 张传恒, 高林志, 等. 北京密云环斑花岗岩的锆石SHRIMP U-Pb年龄及其构造意义[J]. 地质通报, 2008, 27(6): 793-798. doi: 10.3969/j.issn.1671-2552.2008.06.007 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20080607&flag=1

    [27]

    和政军, 牛宝贵, 张新元, 等. 北京密云元古宙常州沟组之下环斑花岗岩古风化壳岩石的发现及其碎屑锆石年龄[J]. 地质通报, 2011, 30(5): 798-802. doi: 10.3969/j.issn.1671-2552.2011.05.020 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20110520&flag=1

    [28]

    李厚民, 陈毓川, 李立兴, 等. 中国铁矿成矿规律[M]. 北京: 地质出版社, 2012: 1-246.

    [29]

    李怀坤, 苏文博, 周红英, 等. 华北克拉通北部长城系底界年龄小于1670Ma: 来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMS U-Pb年龄的约束[J]. 地学前缘, 2011, 18(3): 108-120. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103013.htm

    [30]

    李延河, 侯可军, 万德芳, 等. Algoma型和Superior型硅铁建造地球化学对比研究[J]. 岩石学报, 2012, 28(11): 3513-3519. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201211008.htm

    [31]

    李志红, 朱祥坤. 河北省宣龙式铁矿的地球化学特征及其地质意义[J]. 岩石学报, 2012, 28(9): 2903-2911. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201209020.htm

    [32]

    梁永生. 冀西北宣龙式铁矿中磁铁矿特征及成生机制[D]. 中国地质大学(北京)硕士学位论文, 2019: 1-71.

    [33]

    廖士范, 魏梁鸿, 刘成德, 等. 中国泥盆纪鲕铁石沉积环境、成因[J]. 沉积学报, 1993, 11(1): 93-102. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB199301010.htm

    [34]

    刘成维, 杨云, 谷振飞, 等. 河北陈家窑磁铁矿成因探讨[J]. 矿产勘查, 2013, 4(5): 519-524. doi: 10.3969/j.issn.1674-7801.2013.05.008

    [35]

    刘敏. 宣龙铁矿地质地球化学特征及成因探讨[D]. 中国科学院地质研究所博士学位论文, 1995: 1-104.

    [36]

    陆松年, 李惠民. 蓟县长城系大红峪组火山岩的单颗粒锆石U-Pb法准确定年[J]. 中国地质科学院院报, 1991, 22(1): 137-146. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB199101010.htm

    [37]

    乔秀夫. 中朝板块元古宙板内地震带与盆地格局[J]. 地学前缘, 2002, (3): 141-149. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200203024.htm

    [38]

    宋瑞先, 魏明辉, 王金锁, 等. 张家口地质矿产[M]. 北京: 地质出版社, 2012: 218-221.

    [39]

    孙会一, 高林志, 包创, 等. 河北宽城中元古代串岭沟组凝灰岩SHRIMP锆石U-Pb年龄及其地质意义[J]. 地质学报, 2013, 87(4): 591-596. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201304013.htm

    [40]

    汤冬杰, 史晓颖, 刘典波, 等. 华北古元古代末鲕铁岩: Columbia超大陆裂解初期的沉积响应[J]. 地球科学——中国地质大学学报, 2015, 40(2): 290-304. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201502009.htm

    [41]

    万渝生, 董春艳, 颉颃强, 等. 华北克拉通太古宙研究若干进展[J]. 地球学报, 2015, 36(6): 685-700. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201506001.htm

    [42]

    阎玉忠, 刘志礼. 中国北方燕山盆地长城纪生物群落和古环境关系探讨[J]. 微体古生物学报, 1998, 3: 29-46. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT803.002.htm

    [43]

    杨秀清, 毛景文, 张作衡, 等. 条带状铁建造: 特征、成因及其对地球环境的制约[J]. 矿床地质, 2020, 39(4): 697-727. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ202004011.htm

    [44]

    翟明国. 华北克拉通2.1~1.7Ga地质事件群的分解和构造意义探讨[J]. 岩石学报, 2004, 20(6): 1343-1354. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200406003.htm

    [45]

    翟明国, 彭澎. 华北克拉通古元古代构造事件[J]. 岩石学报, 2007, 11: 2665-2682. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200711002.htm

    [46]

    翟明国. 克拉通化与华北陆块的形成[J]. 中国科学: 地球科学, 2011, 41(8): 1037-1046. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201108001.htm

    [47]

    翟明国. 华北克拉通的形成以及早期板块构造[J]. 地质学报, 2012, 86(9): 1335-1349. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201209004.htm

    [48]

    翟裕生, 姚书振, 蔡克勤. 矿床学[M]. 北京: 地质出版社, 2011: 248-290.

    [49]

    张连昌, 翟明国, 万渝生, 等. 华北克拉通前寒武纪铁建造铁矿研究: 进展与问题[J]. 岩石学报, 2012, 28(11): 3431-3445. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201211002.htm

    [50]

    张拴宏, 赵越, 叶浩, 等. 燕辽地区长城系串岭沟组及团山子组沉积时代的新制约[J]. 岩石学报, 2013, 29(7): 2481-2490. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201307017.htm

    [51]

    赵一鸣, 毕承思. 宁乡式沉积铁矿床的时空分布和演化[J]. 矿床地质, 2020, 19(4): 350-362. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200004007.htm

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