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内蒙古狼山地区叠布斯格岩群锆石U-Pb年龄、Hf同位素特征及其对阿拉善地块构造演化的制约

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牛鹏飞, 曲军峰, 张进, 张北航, 赵衡. 内蒙古狼山地区叠布斯格岩群锆石U-Pb年龄、Hf同位素特征及其对阿拉善地块构造演化的制约[J]. 地质通报, 2022, 41(5): 754-773. doi: 10.12097/j.issn.1671-2552.2022.05.004
引用本文: 牛鹏飞, 曲军峰, 张进, 张北航, 赵衡. 内蒙古狼山地区叠布斯格岩群锆石U-Pb年龄、Hf同位素特征及其对阿拉善地块构造演化的制约[J]. 地质通报, 2022, 41(5): 754-773. doi: 10.12097/j.issn.1671-2552.2022.05.004
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NIU Pengfei, QU Junfeng, ZHANG Jin, ZHANG Beihang, ZHAO Heng. Zircon U-Pb age and Hf isotopic characteristics of the Diebusige Complex in Langshan area, Inner Mongolia, and its constraints on the tectonic evolution of the Alxa Block[J]. Geological Bulletin of China, 2022, 41(5): 754-773. doi: 10.12097/j.issn.1671-2552.2022.05.004
Citation: NIU Pengfei, QU Junfeng, ZHANG Jin, ZHANG Beihang, ZHAO Heng. Zircon U-Pb age and Hf isotopic characteristics of the Diebusige Complex in Langshan area, Inner Mongolia, and its constraints on the tectonic evolution of the Alxa Block[J]. Geological Bulletin of China, 2022, 41(5): 754-773. doi: 10.12097/j.issn.1671-2552.2022.05.004
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内蒙古狼山地区叠布斯格岩群锆石U-Pb年龄、Hf同位素特征及其对阿拉善地块构造演化的制约

  • 中国地质科学院地质研究所，北京100037

  • 基金项目:
    中国地质调查局项目《狼山尔驼庙幅1:5万构造地质填图试点》(编号: 12120115069601)、《北方山系西拉木伦与贺根山基础地质调查》(编号: DD20190004)和国家自然科学基金项目《阿拉善北部蛇绿混杂岩形成机制、变形过程与构造环境》(批准号: 41972224)
详细信息
    作者简介: 牛鹏飞(1992-)，男，在读博士生，构造地质学专业。E-mail：niupf92@163.com

  • 中图分类号: P534.3;P588.3;P597

Zircon U-Pb age and Hf isotopic characteristics of the Diebusige Complex in Langshan area, Inner Mongolia, and its constraints on the tectonic evolution of the Alxa Block

  • Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    摘要

  • 阿拉善地块位于华北克拉通西端，其早前寒武纪地质演化一直存在争议。选取阿拉善地块东北缘的叠布斯格岩群为研究对象，通过锆石U-Pb定年和Lu-Hf同位素分析，探讨阿拉善地块的性质和归属及华北克拉通早期地质演化。叠布斯格岩群主要由变质沉积岩和变质火山岩组成，包括高级变质的片麻岩、大理岩、石英岩、角闪岩，并被古元古代钾质花岗岩侵入。来自叠布斯格岩群3个副片麻岩样品的LA-ICP-MS锆石U-Pb定年结果显示，叠布斯格岩群副片麻岩中碎屑锆石的207Pb/206Pb年龄范围为2.60~2.10 Ga，变质锆石的年龄显示叠布斯格岩群经历了1.98~1.90 Ga和1.90~1.79 Ga的两组峰期变质作用，指示叠布斯格岩群原岩形成于2.10~1.98 Ga。研究区未发现有太古宙岩石出露，但不排除其下部地壳中存在太古宙基底岩石的可能。碎屑锆石的Lu-Hf同位素数据结果显示，叠布斯格岩群副片麻岩中碎屑锆石的εHf(t)均为负值，指示其成岩物质源于古—中太古代(3.42~2.79 Ga)古老地壳在新太古代晚期—古元古代早期的重熔或再造。通过对比叠布斯格岩群和阴山地块、孔兹岩带的岩浆-变质事件及Hf同位素特征，推测阿拉善地块前寒武纪基底在古元古代可能是孔兹岩带的一部分。

    The Alxa Block is located in the western part of the North China Craton (NCC), and its Precambrian geological evolution has been long controversial.In this study, the in-situ zircon U-Pb dating and the Lu-Hf isotope analysis were conducted on the Precambrian basement at the northeast margin of the Alxa Block, which called the Diebusige Complex.The Diebusige Complex consists mainly of metamorphic supracrustal rocks and metamorphic plutonic rocks, including high grade metamorphic gneiss, marble, quartzite, amphibolite and intruded K-felspar granite.LA-ICP-MS zircon U-Pb dating results of three paragneiss samples show that the detrital zircons from the Diebusige Complex yielded 207Pb/206Pb ages range from 2.60 Ga to 2.10 Ga, and the Diebusige Complex subjected to high grade metamorphic events at 1.98~1.90 Ga and 1.90~1.79 Ga, suggesting that the protoliths of the Diebusige Complex may be deposited at 2.10~1.98 Ga.There is no evidence of Archean rocks exposed in Langshan area, but the possibility of Archean rocks exist at deeper crustal levels cannot be ruled out.Zircon Lu-Hf isotopic data shows that the diagenetic material of the Diebusige Complex was originated from the reworking of Early-Middle Archean crust (3.42~2.79 Ga).Comparing the Diebusige Complex with the Yinshan Block and the Khondalite Belt in magmatic-metamorphic events and the Hf isotopic charateristics.We speculate that the Precambrian basements of the Alxa Block are probably part of the Khondalite Belt in Paleoproterozoic.

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  • 图 1  阿拉善地块构造位置(a, 据参考文献[1]修改)及地质简图(b)

    Figure 1. 

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    图 2  狼山地区叠布斯格岩群分布概况

    Figure 2. 

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    图 图版Ⅰ   

    Figure 图版Ⅰ. 

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    图 3  叠布斯格岩群四期变形

    Figure 3. 

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    图 图版Ⅱ   

    Figure 图版Ⅱ. 

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    图 4  叠布斯格岩群锆石阴极发光(CL)图像

    Figure 4. 

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    图 5  样品锆石U-Pb年龄数据谐和图

    Figure 5. 

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    图 6  叠布斯格岩群片麻岩及阴山地块、孔兹岩带基底岩石锆石εHf(t)值-年龄图

    Figure 6. 

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    图 7  叠布斯格岩群片麻岩锆石U-Pb年龄柱状图

    Figure 7. 

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    图 8  叠布斯格岩群片麻岩样品及孔兹岩带、阴山地块基底岩系锆石U-Pb年龄柱状图

    Figure 8. 

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    表 1  叠布斯格岩群角闪斜长片麻岩(17N02-5)与黑云斜长片麻岩(17N06)LA-ICP-MS锆石U-Th-Pb分析结果

    Table 1.  Zircon U-Th-Pb isotope compositions of the amphibole plagio-gneiss (17N02-5) and the biotite plagioclase gneiss samples (17N06) as measured by LA-ICP-MS technique

    样品点号 含量/10-6 Th/U 同位素比值 年龄/Ma 谐和度/%
    Pb Th U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 206Pb/238U 1σ
    17N02-5-01 207 160 302 0.53 0.1467 0.0020 8.8845 0.2597 0.4343 0.0101 2309 24.1 2325 45 99
    17N02-5-02 84.9 109 127 0.86 0.1131 0.0013 5.3817 0.0774 0.3447 0.0039 1850 22.2 1909 19 98
    17N02-5-03 375 271 634 0.43 0.1478 0.0017 8.9798 0.2106 0.4378 0.0086 2320 18.7 2341 39 99
    17N02-5-04 7.48 4.99 19.1 0.26 0.1115 0.0025 5.0624 0.1342 0.3291 0.0056 1824 40.9 1834 27 99
    17N02-5-05 77.0 53.0 141 0.38 0.1376 0.0019 7.7274 0.1362 0.4064 0.0055 2198 24.1 2199 25 99
    17N02-5-06 111 101 190 0.53 0.1310 0.0018 6.6919 0.1017 0.3693 0.0039 2122 24.1 2026 18 97
    17N02-5-07 145.7 102.2 286 0.36 0.1304 0.0019 6.7524 0.1428 0.3732 0.0057 2103 26.2 2044 27 98
    17N02-5-08 288 79.8 621 0.13 0.1576 0.0025 9.9965 0.3259 0.4563 0.0125 2431 27.0 2423 55 99
    17N02-5-09 268 216 356 0.61 0.1519 0.0022 9.4839 0.1596 0.4517 0.0057 2368 24.4 2403 25 99
    17N02-5-10 246 266 300 0.89 0.1393 0.0017 8.0217 0.1141 0.4166 0.0051 2220 20.4 2245 23 99
    17N02-5-11 118 141 207 0.68 0.1102 0.0016 4.8535 0.0796 0.3187 0.0047 1803 25.6 1783 23 99
    17N02-5-12 161 335 47.5 7.04 0.1136 0.0021 5.2974 0.1270 0.3370 0.0060 1858 28.5 1872 29 99
    17N02-5-13 62.0 110 68.5 1.61 0.1106 0.0024 4.5684 0.0865 0.3014 0.0057 1810 37.8 1698 28 97
    17N02-5-14 315 415 544 0.76 0.1122 0.0014 4.8065 0.0900 0.3087 0.0046 1836 23.0 1734 23 97
    17N02-5-15 255 356 425 0.84 0.1107 0.0020 4.6776 0.0671 0.3065 0.0037 1813 27.3 1723 18 97
    17N02-5-16 64.6 108 52.2 2.06 0.1121 0.0018 5.2443 0.1067 0.3376 0.0048 1835 29.6 1875 23 99
    17N02-5-17 541 757 784 0.97 0.1138 0.0013 5.0726 0.0728 0.3223 0.0042 1861 21.8 1801 21 98
    17N02-5-18 217 177 284 0.62 0.1509 0.0018 9.0201 0.1268 0.4326 0.0058 2367 20.4 2318 26 99
    17N02-5-19 289 250 431 0.58 0.1379 0.0025 7.7191 0.2643 0.3944 0.0085 2202 31.5 2143 39 97
    17N02-5-20 80 105 76.3 1.38 0.1330 0.0025 8.6585 0.2479 0.4712 0.0117 2139 32.4 2489 51 92
    17N02-5-21 14.4 11.1 32.7 0.34 0.1123 0.0031 5.1502 0.1250 0.3348 0.0060 1837 50.0 1861 29 99
    17N02-5-22 4.24 3.88 7.34 0.53 0.1285 0.0063 5.7801 0.2988 0.3381 0.0121 2080 87.0 1877 58 96
    17N02-5-23 224 296 309 0.96 0.1127 0.0017 5.2191 0.0869 0.3359 0.0049 1844 27.8 1867 23 99
    17N02-5-24 145 135 255 0.53 0.1207 0.0017 5.9307 0.0944 0.3550 0.0041 1966 24.5 1959 20 99
    17N02-5-25 220 178 276 0.64 0.1603 0.0019 10.3329 0.1453 0.4652 0.0049 2459 20.4 2462 21 99
    17N02-5-26 290 449 268 1.68 0.1137 0.0014 5.4906 0.0730 0.3491 0.0037 1859 22.5 1930 18 98
    17N02-5-27 185 266 188 1.41 0.1184 0.0019 5.6305 0.0939 0.3439 0.0047 1933 27.8 1905 22 99
    17N02-5-28 220 278 300 0.93 0.1208 0.0019 5.8487 0.0999 0.3495 0.0046 1968 27.8 1932 22 98
    17N02-5-29 96 160 92.3 1.73 0.1130 0.0018 5.0487 0.0832 0.3232 0.0041 1850 29.6 1806 20 98
    17N02-5-30 678 483 1695 0.28 0.1150 0.0014 5.2572 0.0736 0.3301 0.0034 1879 22.4 1839 17 98
    17N02-5-31 195 251 305 0.82 0.1184 0.0016 5.2816 0.0784 0.3230 0.0039 1933 23.9 1804 19 96
    17N02-5-32 159 186 233 0.80 0.1356 0.0025 6.8254 0.1730 0.3703 0.0112 2172 31.8 2031 53 97
    17N02-5-33 213 153 268 0.57 0.1619 0.0020 10.3748 0.1810 0.4635 0.0067 2476 21.5 2455 30 99
    17N02-5-34 26.8 39.9 22.5 1.77 0.1189 0.0043 5.7160 0.2225 0.3591 0.0130 1940 63.7 1978 61 97
    17N02-5-35 8.26 8.73 13.0 0.67 0.1175 0.0049 5.5269 0.2605 0.3494 0.0133 1920 74.5 1932 64 98
    17N02-5-36 270 214 368 0.58 0.1516 0.0022 9.1920 0.1662 0.4387 0.0052 2365 24.1 2345 23 99
    17N02-5-37 24.7 38.1 23.9 1.60 0.1125 0.0042 5.2997 0.1875 0.3490 0.0081 1839 66.7 1930 39 96
    17N02-5-38 442 383 644 0.59 0.1347 0.0017 8.3418 0.2006 0.4476 0.0088 2161 22.2 2385 39 95
    17N02-5-39 7.44 7.48 12.2 0.62 0.1113 0.0044 5.1982 0.2030 0.3508 0.0115 1820 76.4 1938 55 95
    17N02-5-40 192.8 103.2 390 0.26 0.1309 0.0018 6.8843 0.1116 0.3809 0.0042 2111 24.2 2080 19 99
    17N02-5-41 272 272 341 0.80 0.1513 0.0024 8.2140 0.2050 0.3928 0.0076 2360 27.2 2136 35 94
    17N02-5-42 468 445 549 0.81 0.1504 0.0017 8.7844 0.1307 0.4231 0.0048 2350 19.3 2275 22 98
    17N02-5-43 21.3 28.9 20.3 1.43 0.1184 0.0038 5.7602 0.2182 0.3569 0.0108 1932 57 1968 51 98
    17N02-5-44 585 558 590 0.95 0.1596 0.0019 9.8691 0.1372 0.4476 0.0041 2452 20.5 2385 18 98
    17N02-5-45 197 138 255 0.54 0.1512 0.0021 9.9800 0.2258 0.4763 0.0083 2359 23.9 2511 36 96
    17N02-5-46 245 186 309 0.60 0.1558 0.0019 9.6774 0.1416 0.4494 0.0045 2411 20.4 2393 20 99
    17N02-5-47 390 406 415 0.98 0.1421 0.0018 8.2344 0.1310 0.4191 0.0043 2253 22.4 2256 20 99
    17N02-5-48 490 426 984 0.43 0.1304 0.0018 6.1854 0.1137 0.3428 0.0040 2103 23.9 1900 19 94
    17N02-5-49 7.82 7.37 12.3 0.60 0.1185 0.0058 5.8789 0.4439 0.3639 0.0167 1944 88.7 2001 79 97
    17N02-5-50 49.5 89.0 37.5 2.37 0.1118 0.0025 4.8351 0.1100 0.3153 0.0050 1829 39.0 1767 25 98
    17N02-5-51 5.94 8.05 6.03 1.33 0.1201 0.0073 5.6777 0.3572 0.3564 0.0151 1958 108 1965 72 98
    17N02-5-52 240.7 67.3 670 0.10 0.1154 0.0016 5.8135 0.1037 0.3645 0.0047 1887 30.7 2003 22 97
    17N02-5-53 7.16 8.00 13.1 0.61 0.1107 0.0033 4.9202 0.1580 0.3264 0.0071 1813 48.9 1821 34 99
    17N02-5-54 16.8 21.3 24.1 0.88 0.1120 0.0035 4.9790 0.1369 0.3313 0.0087 1832 55.7 1845 42 98
    17N02-5-55 24.3 42.1 18.6 2.27 0.1124 0.0042 4.8887 0.1381 0.3186 0.0060 1839 67.0 1783 29 99
    17N02-5-56 8.6 11.9 9.6 1.24 0.1179 0.0047 5.3028 0.2021 0.3517 0.0275 1926 70.5 1943 131 96
    17N02-5-57 122 141 183 0.77 0.1191 0.0022 5.5495 0.1165 0.3385 0.0051 1943 33.5 1879 24 98
    17N02-5-58 237 113.0 590 0.19 0.1157 0.0016 5.8436 0.0969 0.3660 0.0047 1900 25.8 2011 22 97
    17N02-5-59 90 142 64.6 2.20 0.1194 0.0022 5.9012 0.1092 0.3610 0.0059 1947 33.3 1987 28 98
    17N02-5-60 5.13 5.22 8.46 0.62 0.1011 0.0055 4.7118 0.2337 0.3546 0.0183 1644 101.4 1957 87 89
    17N02-5-61 30.7 47.5 30.2 1.57 0.1129 0.0028 5.2048 0.1202 0.3362 0.0060 1847 43.8 1868 29 99
    17N02-5-62 86.1 85.7 109 0.79 0.1311 0.0019 7.5003 0.1198 0.4147 0.0046 2122 25.9 2236 21 97
    17N02-5-63 248 264 443 0.60 0.1133 0.0014 5.3005 0.0826 0.3390 0.0040 1854 21.1 1882 19 99
    17N06-01 281.1 30.2 715 0.04 0.1167 0.0013 5.3431 0.0653 0.3320 0.0036 1906 21.5 1848 17 98
    17N06-02 96 107 75.6 1.41 0.1138 0.0022 5.2810 0.0839 0.3366 0.0041 1861 35.2 1870 20 99
    17N06-03 148.3 114.2 224 0.51 0.1167 0.0012 5.2621 0.0737 0.3264 0.0038 1906 17.9 1821 18 97
    17N06-04 126.2 74.5 234 0.32 0.1103 0.0011 4.8762 0.0660 0.3204 0.0038 1803 17.4 1791 19 99
    17N06-05 1234 1768 394 4.48 0.1137 0.0012 5.2407 0.0675 0.3337 0.0035 1861 18.5 1856 17 99
    17N06-06 152 179 85.1 2.10 0.1172 0.0019 5.5624 0.1045 0.3436 0.0041 1914 29.6 1904 20 99
    17N06-07 76 92 52.2 1.77 0.1110 0.0018 5.0485 0.1027 0.3301 0.0053 1816 29.8 1839 26 99
    17N06-08 501 624 217 2.88 0.1124 0.0013 5.4620 0.0782 0.3521 0.0039 1839 22.1 1944 19 97
    17N06-09 51.5 55.8 37.5 1.49 0.1183 0.0027 5.5348 0.1188 0.3416 0.0055 1931 41.8 1894 27 99
    17N06-10 652 883 264 3.34 0.1118 0.0014 5.1301 0.0843 0.3329 0.0049 1828 22.7 1852 24 99
    17N06-11 22.94 2.51 55.5 0.05 0.1142 0.0016 5.3784 0.1097 0.3403 0.0049 1933 24.8 1888 24 99
    17N06-12 583 351 583 0.60 0.1503 0.0017 8.8199 0.1328 0.4245 0.0048 2350 18.7 2281 22 98
    17N06-13 319 393 199 1.98 0.1101 0.0014 5.2721 0.0687 0.3472 0.0038 1811 17.4 1921 18 96
    17N06-14 268 348 134 2.60 0.1123 0.0017 5.2036 0.1091 0.3360 0.0066 1839 27.3 1867 32 99
    17N06-15 333 274 250 1.10 0.1350 0.0022 7.7429 0.2731 0.4095 0.0107 2165 27.8 2212 49 99
    17N06-16 555 707 250 2.83 0.1125 0.0015 5.3520 0.0946 0.3451 0.0057 1840 24.1 1911 27 98
    17N06-17 95 92.1 104 0.89 0.1117 0.0018 5.1625 0.1159 0.3342 0.0056 1828 29.5 1858 27 99
    17N06-18 58.8 38.6 87.7 0.44 0.1099 0.0016 5.2142 0.1101 0.3434 0.0059 1798 26.1 1903 28 97
    17N06-19 537 432 478 0.90 0.1360 0.0015 7.7200 0.1006 0.4114 0.0050 2177 19.1 2221 23 98
    17N06-20 1365 1166 750 1.55 0.1546 0.0016 9.6428 0.1530 0.4511 0.0060 2398 17.3 2400 27 99
    17N06-21 575 740 263 2.82 0.1134 0.0015 5.3855 0.1003 0.3443 0.0059 1855 23.9 1907 28 98
    17N06-22 366 389 276 1.41 0.1187 0.0022 5.4203 0.1801 0.3285 0.0075 1939 34.7 1831 37 96
    17N06-23 263 334 147 2.27 0.1114 0.0016 5.1507 0.1005 0.3349 0.0054 1833 25.9 1862 26 99
    17N06-24 129 135 114 1.18 0.1104 0.0016 5.1934 0.0964 0.3410 0.0052 1806 26.5 1892 25 97
    17N06-25 1012 719 721 1.00 0.1555 0.0017 9.7653 0.1423 0.4547 0.0051 2407 18.2 2416 23 99
    17N06-26 63.7 44.8 85.1 0.53 0.1105 0.0021 5.4114 0.1089 0.3555 0.0046 1809 35.0 1961 22 96
    17N06-27 496 317 330 0.96 0.1605 0.0022 11.0972 0.1768 0.5012 0.0053 2461 22.7 2619 23 96
    17N06-28 315 403 168 2.40 0.1118 0.0020 5.1454 0.1087 0.3338 0.0052 1829 31.5 1857 25 99
    17N06-29 84 95.8 59.7 1.61 0.1126 0.0024 5.0889 0.1227 0.3281 0.0057 1843 38.1 1829 28 99
    17N06-30 239 186 164 1.14 0.1423 0.0023 8.4100 0.1486 0.4284 0.0047 2255 27.6 2299 21 99
    17N06-31 326 403 159 2.53 0.1094 0.0016 5.3380 0.0858 0.3539 0.0041 1791 25.9 1953 19 95
    17N06-32 463 330 374 0.88 0.1473 0.0021 8.7042 0.1659 0.4278 0.0065 2317 24.4 2296 30 99
    17N06-33 137 171 120 1.43 0.1105 0.0022 4.6046 0.1162 0.3026 0.0074 1807 36.4 1704 37 97
    17N06-34 429 343 262 1.31 0.1592 0.0026 9.9024 0.2072 0.4505 0.0079 2447 27.8 2397 35 98
    17N06-35 294 226 253 0.90 0.1433 0.0024 8.0462 0.1480 0.4059 0.0044 2333 28.4 2196 20 98
    17N06-36 77 85.4 58.3 1.47 0.1131 0.0024 5.3096 0.1233 0.3396 0.0043 1850 38.3 1885 21 99
    17N06-37 375 312 315 0.99 0.1317 0.0023 7.3577 0.2426 0.4000 0.0094 2121 25.8 2169 43 99
    17N06-38 731 877 546 1.61 0.1099 0.0015 4.9920 0.0882 0.3286 0.0046 1798 24.1 1831 22 99
    17N06-39 70.9 72.3 51.4 1.41 0.1192 0.0023 5.8569 0.1377 0.3556 0.0058 1944 33.9 1961 28 99
    17N06-40 266 208 230 0.90 0.1357 0.0023 7.8621 0.2677 0.4123 0.0093 2173 29.9 2226 42 99
    17N06-41 197 254 103.0 2.46 0.1120 0.0017 5.1642 0.1070 0.3347 0.0070 1831 26.1 1861 34 99
    17N06-42 104 129 89.6 1.44 0.1097 0.0024 4.4874 0.1216 0.2962 0.0064 1794 40.7 1673 32 96
    17N06-43 145 161 107 1.51 0.1141 0.0019 5.2957 0.1159 0.3360 0.0061 1865 29.5 1868 29 99
    17N06-44 207 230 136 1.69 0.1176 0.0018 5.8917 0.1418 0.3623 0.0075 1920 27.8 1993 35 98
    17N06-45 106 122 70.5 1.73 0.1134 0.0019 5.3549 0.1168 0.3411 0.0054 1855 26.9 1892 26 99
    17N06-46 90 100 67.9 1.48 0.1116 0.0022 5.1575 0.1118 0.3341 0.0046 1826 35.0 1858 22 99
    17N06-47 268 179 238 0.76 0.1478 0.0017 8.7657 0.1119 0.4286 0.0042 2321 20.4 2299 19 99
    17N06-48 200 236 131 1.81 0.1114 0.0016 5.1811 0.1107 0.3358 0.0060 1833 27.3 1867 29 99
    17N06-49 281 360 135 2.67 0.1126 0.0018 5.1927 0.0925 0.3332 0.0044 1843 29.8 1854 21 99
    17N06-50 481 625 226 2.77 0.1114 0.0016 5.1309 0.0865 0.3328 0.0045 1822 25.3 1852 22 99
    17N06-51 303 225 355 0.63 0.1179 0.0017 5.8905 0.0963 0.3603 0.0034 1924 25.8 1983 16 98
    17N06-52 386 255 346 0.74 0.1477 0.0016 8.6909 0.1096 0.4250 0.0041 2320 18.4 2283 19 99
    17N06-53 116 121 112 1.08 0.1107 0.0014 4.9282 0.0683 0.3219 0.0030 1810 24.1 1799 14 99
    17N06-54 146 175 94.6 1.85 0.1137 0.0023 5.1900 0.1284 0.3303 0.0065 1861 31.0 1840 31 99
    17N06-55 275 219 242 0.90 0.1330 0.0016 7.2153 0.0850 0.3933 0.0041 2139 21.0 2138 19 99
    17N06-56 492 347 317 1.10 0.1511 0.0023 8.9095 0.1966 0.4251 0.0067 2358 25.3 2284 30 98
    17N06-57 278 186 373 0.50 0.1170 0.0014 5.8369 0.0867 0.3606 0.0042 1922 16.2 1985 20 98
    17N06-58 249 305 150 2.03 0.1124 0.0017 5.1933 0.0927 0.3343 0.0044 1839 25.8 1859 21 99
    17N06-59 211 233 129 1.80 0.1185 0.0014 5.8686 0.1162 0.3584 0.0062 1944 16.5 1975 30 99
    17N06-60 442 324 301 1.07 0.1544 0.0017 9.5808 0.1187 0.4490 0.0038 2395 18.5 2391 17 99
    17N06-61 271 352 134 2.62 0.1118 0.0018 5.1183 0.1039 0.3319 0.0055 1828 29.2 1848 27 99
    17N06-62 493 629 242 2.60 0.1144 0.0014 5.2800 0.0907 0.3338 0.0042 1870 23.6 1857 20 99
    17N06-63 319 291 345 0.84 0.1200 0.0014 5.7629 0.0936 0.3471 0.0040 1967 26.7 1921 19 98
    下载: 导出CSV

    表 2  叠布斯格岩群黑云钾长片麻岩(D791-1)SHRIMP锆石U-Th-Pb分析结果

    Table 2.  SHRIMP zircon U-Th-Pb data of the biotite K-feldspar gneiss (D791-1) from the Diebusige Complex

    样品点号 含量/10-6 Th/U 同位素比值 年龄/Ma
    Pb Th U 207Pb/206Pb 1σ/% 207Pb/235U 1σ/% 206Pb/238U 1σ/% 207Pb/206Pb 1σ
    D791-1-1 71.2 148 246 0.62 0.1139 1.40 5.253 1.90 0.3346 1.20 1862 25
    D791-1-2 154 35 487 0.07 0.12170 0.57 6.185 1.30 0.3686 1.10 1981 10
    D791-1-3 15.1 62 53 1.22 0.1088 8.90 4.89 9.20 0.3261 2.00 1778 160
    D791-1-4 102 120 232 0.53 0.1744 0.64 12.26 1.40 0.5100 1.20 2601 11
    D791-1-5 13.2 3 42 0.07 0.1284 4.20 6.39 4.60 0.3611 1.80 2076 74
    D791-1-6 24.9 94 86 1.14 0.1094 2.60 5.04 3.00 0.3343 1.50 1789 48
    D791-1-7 122 123 309 0.41 0.16307 0.54 10.33 1.30 0.4595 1.20 2488 9.1
    D791-1-8 62.7 26 172 0.16 0.1453 1.20 8.41 1.80 0.4197 1.30 2291 21
    D791-1-9 174 88 565 0.16 0.1201 0.86 5.884 1.50 0.3555 1.20 1957 15
    D791-1-10 37.1 159 124 1.32 0.1134 2.00 5.36 2.40 0.3433 1.50 1853 36
    D791-1-11 173 220 405 0.56 0.17257 0.50 11.79 1.30 0.4953 1.20 2583 8.4
    D791-1-12 39.3 70 139 0.52 0.1159 1.20 5.227 1.90 0.3270 1.50 1895 22
    D791-1-13 64.8 2 201 0.01 0.1215 1.10 6.24 1.70 0.3728 1.30 1978 20
    D791-1-14 16.2 51 54 0.98 0.1097 5.10 5.04 5.40 0.3334 1.80 1792 93
    D791-1-15 35.6 64 116 0.57 0.1200 3.10 5.81 3.40 0.3511 1.40 1956 56
    下载: 导出CSV

    表 3  叠布斯格岩群角闪斜长片麻岩(17N02-5)与黑云斜长片麻岩(17N06)锆石原位Lu-Hf同位素组成

    Table 3.  Zircon in-situ Lu-Hf isotopic compositions of the amphibole plagio-gneiss (17N02-5) and the biotite plagioclase gneiss (17N06) from the Diebusige Complex

    点号 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf 2σ 年龄/Ma (176Hf/177Hf)i εHf(0) εHf(t) 2σ TDM/Ma TDM2/Ma fLu/Hf
    角闪斜长片麻岩
    17N02-5-01 0.03660 0.00078 0.28131 0.000041 2350 0.281277 -51.6 -0.22 1.46 2691 2898 -0.97645
    17N02-5-02 0.00942 0.00020 0.28132 0.000043 1847 0.281311 -51.4 -10.52 1.53 2643 3146 -0.99386
    17N02-5-03 0.08220 0.00165 0.28124 0.000051 2327 0.281166 -54.2 -4.68 1.81 2853 3153 -0.95042
    17N02-5-04 0.01656 0.00035 0.28132 0.000044 1843 0.281305 -51.5 -10.84 1.56 2654 3162 -0.98951
    17N02-5-05 0.01780 0.00040 0.28116 0.000052 2202 0.281142 -57.0 -8.39 1.85 2869 3285 -0.98810
    17N02-5-06 0.04940 0.00099 0.28121 0.000051 2085 0.281173 -55.2 -10.00 1.81 2841 3294 -0.97032
    17N02-5-08 0.06600 0.00136 0.28126 0.000057 2478 0.281190 -53.6 -0.34 2.03 2810 3004 -0.95892
    17N02-5-10 0.05890 0.00125 0.28121 0.000056 2224 0.281153 -55.4 -7.52 1.99 2869 3248 -0.96226
    17N02-5-11 0.08219 0.00167 0.28124 0.000064 1798 0.281184 -54.1 -16.14 2.27 2853 3453 -0.94958
    17N02-5-14 0.04155 0.00084 0.28126 0.000057 1902 0.281227 -53.6 -12.27 2.02 2769 3294 -0.97466
    17N02-5-12 0.04456 0.00102 0.28136 0.000040 1835 0.281320 -50.1 -10.45 1.42 2648 3133 -0.96921
    17N02-5-13 0.01867 0.00039 0.28135 0.000035 1828 0.281332 -50.4 -10.19 1.24 2618 3111 -0.98821
    17N02-5-15 0.04661 0.00097 0.28122 0.000044 1833 0.281182 -55.0 -15.40 1.56 2834 3434 -0.97087
    17N02-5-16 0.00355 0.00007 0.28136 0.000044 1840 0.281354 -50.1 -9.17 1.56 2583 3058 -0.99798
    17N02-5-19 0.04200 0.00089 0.28132 0.000046 2310 0.281279 -51.4 -1.08 1.64 2690 2920 -0.97310
    17N02-5-21 0.01939 0.00042 0.28140 0.000044 1847 0.281384 -48.6 -7.91 1.56 2549 2986 -0.98746
    17N02-5-20 0.03576 0.00078 0.28124 0.000044 2128 0.281212 -54.0 -7.62 1.56 2783 3181 -0.97639
    17N02-5-22 0.00969 0.00019 0.28136 0.000051 2052 0.281356 -49.8 -4.24 1.81 2581 2916 -0.99419
    17N02-5-23 0.01823 0.00043 0.28136 0.000049 1851 0.281344 -50.0 -9.26 1.74 2603 3071 -0.98711
    17N02-5-25 0.06659 0.00144 0.28127 0.000055 2454 0.281198 -53.3 -0.64 1.96 2802 3004 -0.95669
    17N02-5-26 0.03189 0.00062 0.28138 0.000044 1869 0.281356 -49.3 -8.41 1.56 2591 3034 -0.98120
    17N02-5-27 0.02602 0.00058 0.28139 0.000044 1933 0.281364 -49.1 -6.69 1.56 2578 2976 -0.98250
    17N02-5-29 0.01861 0.00043 0.28144 0.000045 1850 0.281422 -47.2 -6.51 1.60 2498 2902 -0.98702
    17N02-5-33 0.04526 0.00101 0.28124 0.000064 2474 0.281189 -54.3 -0.48 2.28 2809 3009 -0.96957
    17N02-5-35 0.02140 0.00046 0.28133 0.000044 1835 0.281310 -51.1 -10.82 1.56 2649 3155 -0.98626
    17N02-5-36 0.02710 0.00057 0.28118 0.000056 2381 0.281154 -56.3 -3.87 1.99 2853 3145 -0.98292
    17N02-5-37 0.01430 0.00031 0.28129 0.000039 1883 0.281282 -52.3 -10.73 1.39 2683 3186 -0.99073
    17N02-5-38 0.03497 0.00075 0.28122 0.000042 2161 0.281184 -55.1 -7.84 1.49 2819 3220 -0.97747
    17N02-5-39 0.01789 0.00040 0.28141 0.000044 1858 0.281394 -48.2 -7.32 1.56 2535 2958 -0.98793
    17N02-5-41 0.04594 0.00102 0.28126 0.000055 2551 0.281210 -53.5 2.05 1.96 2778 2914 -0.96922
    17N02-5-42 0.06232 0.00126 0.28124 0.000047 2351 0.281184 -54.1 -3.49 1.67 2822 3098 -0.96192
    17N02-5-43 0.02065 0.00048 0.28132 0.000042 2106 0.281302 -51.3 -4.93 1.49 2658 3000 -0.98560
    17N02-5-44 0.12680 0.00249 0.28135 0.000066 2429 0.281231 -50.4 -0.01 2.35 2766 2946 -0.92494
    17N02-5-45 0.03560 0.00079 0.28131 0.000056 2228 0.281274 -51.8 -3.12 1.99 2697 2982 -0.97611
    17N02-5-46 0.05033 0.00106 0.28123 0.000056 2409 0.281178 -54.6 -2.35 1.99 2826 3074 -0.96819
    17N02-5-47 0.04008 0.00093 0.28122 0.000049 2265 0.281181 -54.8 -5.58 1.74 2825 3161 -0.97199
    17N02-5-49 0.01497 0.00035 0.28132 0.000050 1850 0.281311 -51.2 -10.45 1.78 2646 3144 -0.98953
    17N02-5-51 0.01748 0.00038 0.28133 0.000052 1987 0.281312 -51.1 -7.30 1.85 2644 3054 -0.98867
    17N02-5-50 0.00150 0.00003 0.28125 0.000049 1832 0.281249 -53.8 -13.05 1.74 2722 3290 -0.99910
    17N02-5-52 0.03630 0.00077 0.28149 0.000043 1894 0.281464 -45.3 -4.00 1.53 2446 2781 -0.97672
    17N02-5-53 0.01692 0.00041 0.28135 0.000043 1856 0.281336 -50.3 -9.44 1.53 2614 3086 -0.98780
    17N02-5-54 0.01414 0.00033 0.28131 0.000040 1872 0.281300 -51.6 -10.33 1.42 2660 3153 -0.98997
    17N02-5-55 0.01317 0.00031 0.28138 0.000040 1958 0.281363 -49.4 -6.12 1.42 2574 2960 -0.99065
    17N02-5-57 0.03294 0.00076 0.28123 0.000052 1911 0.281200 -54.6 -12.99 1.85 2803 3346 -0.97708
    17N02-5-58 0.01439 0.00033 0.28143 0.000043 1884 0.281415 -47.6 -5.96 1.53 2505 2894 -0.99017
    17N02-5-59 0.02605 0.00065 0.28137 0.000041 1937 0.281343 -49.7 -7.34 1.46 2607 3019 -0.98038
    17N02-5-60 0.01471 0.00035 0.28137 0.000045 1740 0.281359 -49.6 -11.26 1.60 2583 3111 -0.98961
    17N02-5-61 0.02151 0.00053 0.28137 0.000044 1861 0.281347 -49.7 -8.90 1.56 2601 3058 -0.98401
    17N02-5-62 0.04824 0.00108 0.28130 0.000047 2047 0.281253 -52.2 -8.01 1.67 2735 3143 -0.96759
    17N02-5-63 0.02751 0.00064 0.28144 0.000041 1855 0.281413 -47.3 -6.72 1.46 2514 2919 -0.98078
    黑云斜长片麻岩
    17N06-01 0.01069 0.00022 0.28139 0.000037 1909 0.281385 -48.8 -6.47 1.31 2544 2944 -0.99346
    17N06-02 0.00327 0.00007 0.28131 0.000042 1854 0.281303 -51.9 -10.67 1.49 2651 3160 -0.99788
    17N06-03 0.02824 0.00066 0.28121 0.000044 1922 0.281186 -55.2 -13.24 1.56 2819 3369 -0.98027
    17N06-04 0.01253 0.00033 0.28123 0.000041 1806 0.281215 -54.7 -14.89 1.46 2775 3382 -0.98991
    17N06-05 0.04100 0.00086 0.28142 0.000069 1865 0.281391 -47.7 -7.26 2.45 2547 2959 -0.97402
    17N06-06 0.01344 0.00032 0.28133 0.000049 1916 0.281317 -51.0 -8.72 1.74 2636 3088 -0.99022
    17N06-07 0.00772 0.00018 0.28136 0.000045 1833 0.281352 -50.0 -9.39 1.60 2588 3066 -0.99465
    17N06-08 0.02691 0.00057 0.28137 0.000067 1831 0.281353 -49.5 -9.38 2.38 2594 3064 -0.98277
    17N06-09 0.01812 0.00043 0.28129 0.000047 1917 0.281275 -52.4 -10.19 1.67 2694 3179 -0.98717
    17N06-11 0.00284 0.00006 0.28143 0.000031 1896 0.281428 -47.5 -5.25 1.10 2484 2860 -0.99813
    17N06-12 0.03923 0.00084 0.28121 0.000042 2327 0.281169 -55.4 -4.58 1.49 2838 3148 -0.97461
    17N06-13 0.04580 0.00095 0.28138 0.000078 1803 0.281344 -49.3 -10.33 2.77 2614 3101 -0.97127
    17N06-14 0.03034 0.00069 0.28128 0.000070 1829 0.281257 -52.7 -12.83 2.49 2726 3274 -0.97928
    17N06-15 0.00862 0.00021 0.28136 0.000037 2231 0.281348 -50.0 -0.41 1.32 2591 2819 -0.99360
    17N06-16 0.04066 0.00085 0.28140 0.000067 1836 0.281372 -48.4 -8.59 2.38 2573 3019 -0.97441
    17N06-17 0.00150 0.00003 0.28128 0.000045 1818 0.281278 -52.8 -12.36 1.60 2683 3237 -0.99911
    17N06-18 0.02394 0.00050 0.28127 0.000041 1800 0.281251 -53.2 -13.72 1.46 2730 3307 -0.98500
    17N06-19 0.02926 0.00067 0.28117 0.000051 2183 0.281141 -56.7 -8.87 1.81 2876 3300 -0.97978
    17N06-20 0.06732 0.00151 0.28122 0.000054 2415 0.281151 -54.8 -3.19 1.92 2868 3129 -0.95452
    17N06-21 0.04337 0.00084 0.28138 0.000055 1857 0.281349 -49.3 -8.92 1.95 2604 3056 -0.97466
    17N06-22 0.05267 0.00119 0.28120 0.000048 2021 0.281158 -55.5 -11.98 1.71 2867 3366 -0.96404
    17N06-23 0.01515 0.00031 0.28137 0.000048 1831 0.281356 -49.7 -9.27 1.70 2585 3058 -0.99054
    17N06-24 0.01454 0.00034 0.28128 0.000046 1840 0.281268 -52.8 -12.19 1.63 2703 3244 -0.98965
    17N06-26 0.02728 0.00062 0.28123 0.000052 1769 0.281207 -54.6 -15.99 1.85 2793 3422 -0.98120
    17N06-25 0.03798 0.00079 0.28115 0.000044 2406 0.281115 -57.3 -4.70 1.56 2909 3214 -0.97630
    17N06-29 0.01909 0.00044 0.28128 0.000047 1835 0.281266 -52.7 -12.40 1.67 2709 3252 -0.98672
    17N06-32 0.03405 0.00072 0.28116 0.000040 2320 0.281131 -56.9 -6.08 1.42 2887 3233 -0.97843
    17N06-33 0.00682 0.00015 0.28130 0.000055 1744 0.281291 -52.2 -13.57 1.95 2669 3256 -0.99537
    17N06-35 0.03206 0.00072 0.28115 0.000057 2280 0.281119 -57.4 -7.45 2.03 2905 3286 -0.97836
    17N06-36 0.01323 0.00028 0.28138 0.000054 1854 0.281365 -49.4 -8.44 1.92 2571 3023 -0.99171
    17N06-40 0.03034 0.00071 0.28120 0.000047 2221 0.281168 -55.7 -7.06 1.67 2839 3217 -0.97866
    17N06-42 0.00893 0.00019 0.28136 0.000051 1754 0.281356 -49.9 -11.05 1.81 2583 3108 -0.99441
    17N06-44 0.03469 0.00087 0.28138 0.000056 1939 0.281344 -49.4 -7.24 1.99 2610 3015 -0.97392
    17N06-45 0.01350 0.00028 0.28130 0.000044 1854 0.281285 -52.2 -11.28 1.56 2679 3198 -0.99164
    17N06-47 0.01887 0.00042 0.28114 0.000044 2317 0.281124 -57.6 -6.43 1.56 2893 3252 -0.98740
    17N06-49 0.02670 0.00049 0.28132 0.000052 1856 0.281305 -51.3 -10.55 1.85 2657 3154 -0.98524
    17N06-50 0.04541 0.00089 0.28139 0.000072 1817 0.281361 -48.8 -9.42 2.56 2590 3056 -0.97312
    17N06-51 0.03030 0.00062 0.28125 0.000047 1947 0.281231 -53.7 -11.08 1.67 2757 3256 -0.98139
    17N06-55 0.03314 0.00072 0.28114 0.000053 2135 0.281115 -57.6 -10.92 1.88 2913 3388 -0.97836
    17N06-57 0.01227 0.00029 0.28135 0.000039 1902 0.281344 -50.1 -8.12 1.39 2600 3040 -0.99133
    17N06-59 0.03053 0.00061 0.28120 0.000049 1928 0.281180 -55.5 -13.33 1.74 2827 3379 -0.98175
    17N06-61 0.01982 0.00038 0.28135 0.000047 1822 0.281336 -50.3 -10.21 1.67 2613 3108 -0.98850
    17N06-62 0.03170 0.00057 0.28136 0.000072 1887 0.281337 -50.0 -8.70 2.56 2615 3064 -0.98283
    下载: 导出CSV
    • 参考文献(73)
  • [1]

    Zhao G C, Sun M, Wilde S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited[J]. Precambrian Research, 2005, 136(2): 177-202. doi: 10.1016/j.precamres.2004.10.002

    [2]

    耿元生, 王新社, 沈其韩, 等. 内蒙古阿拉善地区前寒武纪变质基底阿拉善群的再厘定[J]. 中国地质, 2006, 33(1): 138-145. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200601014.htm

    [3]

    耿元生, 王新社, 沈其韩, 等. 内蒙古阿拉善地区前寒武纪变质岩系形成时代的初步研究[J]. 中国地质, 2007, 34(2): 251-261. doi: 10.3969/j.issn.1000-3657.2007.02.006

    [4]

    耿元生, 王新社, 吴春明, 等. 阿拉善变质基底古元古代晚期的构造热事件[J]. 岩石学报, 2010, 26(4): 1159-1170. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201004014.htm

    [5]

    李江海, 牛向龙, 程素华, 等. 大陆克拉通早期构造演化历史探讨——以华北为例[J]. 地质科学: 中国地质大学学报, 2006, 31(3): 285-293. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200603000.htm

    [6]

    耿元生, 周喜文. 阿拉善地区新元古代岩浆事件及其地质意义[J]. 岩石矿物学杂志, 2010, 29(6): 779-795. doi: 10.3969/j.issn.1000-6524.2010.06.014

    [7]

    宫江华, 张建新, 于胜尧. 阿拉善地块南缘龙首山岩群及相关岩石的起源和归属——来自LA-ICP-MS锆石U-Pb年龄的制约[J]. 岩石矿物学杂志, 2011, 30(5): 795-818. doi: 10.3969/j.issn.1000-6524.2011.05.005

    [8]

    Dan W, Li X H, Guo J H, et al. Paleoproterozoic evolution of the eastern Alxa Block, westernmost North China: Evidence from in situ zircon U-Pb dating and Hf-O isotopes[J]. Gondwana Research, 2012, 21(4): 838-864. doi: 10.1016/j.gr.2011.09.004

    [9]

    Dan W, Li X H, Guo J H, et al. Integrated in situ zircon U-Pb age and Hf-O isotopes for the Helanshan khondalites in North China Craton: Juvenile crustal materials deposited in or passive continental margin?[J]. Precambrian Research, 2012, 222/223: 143-158. doi: 10.1016/j.precamres.2011.07.016

    [10]

    Dan W, Li X H, Wang Q, et al. Phanerozoic amalgamation of the Alxa Block and North China Craton: evidence from Paleozoic granitoids, U-Pb geochronology and Sr-Nd-Pb-Hf-O isotope geochemistry[J]. Gondwana Research, 2016, 32: 105-121. doi: 10.1016/j.gr.2015.02.011

    [11]

    Zhang J X, Gong J H, Yu S Y, et al. Neoarchean-Paleoproterozoic multiple tectono thermal events in the western Alxa block, North China Craton and their geological implication: Evidence from zircon U-Pb ages and Hf isotopic composition[J]. Precambrian Research, 2013, 235: 36-57. doi: 10.1016/j.precamres.2013.05.002

    [12]

    Wu S J, Hu J M, Ren M H, et al. Petrography and zircon U-Pb isotopic study of the Bayanwulashan Complex: Constrains on the Paleoproterozoic evolution of the Alxa Block, westernmost North China Craton[J]. Journal of Asian Earth Sciences, 2014, 94: 226-239. doi: 10.1016/j.jseaes.2014.05.011

    [13]

    Zhao G C, Wilde S A, Cawood P A, et al. Archean blocks and their boundaries in the North China Craton: Lithological, geochemical, structural and P-T path constrains and tectonic evolution[J]. Precambrian Research, 2001, 107: 45-73. doi: 10.1016/S0301-9268(00)00154-6

    [14]

    Yin, C Q, Zhao G C, Sun M, et al. LA-ICP-MS U-Pb zircon ages of theQianlishan Complex: Constrains on the evolution of the Khondalite Beltin the Western Block of the North China Craton[J]. Precambrian Research, 2009, 174(1/2): 78-94.

    [15]

    Yin C Q, Zhao G C, Guo J H, et al. U-Pb and Hf isotopic study of zircons of the Helanshan Complex: Constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton[J]. Lithos, 2011, 122(1/2): 25-38. https://www.sciencedirect.com/science/article/pii/S0024493710003233

    [16]

    Santosh M, Tsunogae T, Li J H. Discovery of sapphirine-bearing Mg-Al granulites in the North China Craton: Implications for Paleoproterozoic ultrahigh temperature metamorphism[J]. Gondwana Research, 2007, 11(3): 263-285. doi: 10.1016/j.gr.2006.10.009

    [17]

    董春艳, 刘敦一, 李俊健, 等. 华北克拉通西部孔兹岩带形成时代新证据: 巴彦乌拉—贺兰山地区锆石SHRIMP定年和Hf同位素组成[J]. 科学通报, 2007, 39(12): 1744-1752. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200716012.htm

    [18]

    段瑞涵, 刘超辉, 施建荣. 华北克拉通孔兹岩带磴口和佘太地区花岗片麻岩和斜长角闪岩变质锆石对其北界位置的再约束[J]. 地球科学, 2020, 45(9): 3386-3402. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202009017.htm

    [19]

    Dong X P, Hu J M, Li Z H, et al. Provenance of Ediacaran (Sinian) sediments in the Helanshan area, North China Craton: Constraints from U-Pb geochronology and Hf isotopes of detrital zircons[J]. Precambrian Research, 2017, 298: 490-511. doi: 10.1016/j.precamres.2017.06.022

    [20]

    葛肖虹, 刘俊来. 被肢解的"西域克拉通"[J]. 岩石学报, 2000, 16(1): 59-66. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200001006.htm

    [21]

    Li X H, Su L, Song B, et al. SHRIMP U-Pb zircon age of the Jinchuan ultramafic intrusion and its geological significance[J]. Chinese Science Bulletin, 2004, 49 (4): 420-42. doi: 10.1007/BF02900329

    [22]

    段吉业, 葛肖虹. 中国西北地区各构造单元之间地层和生物古地理的亲缘关系——兼论西北地区构造格局[J]. 地质通报, 2005, 24(6): 558-563. doi: 10.3969/j.issn.1671-2552.2005.06.013

    [23]

    Yuan W, Yang Z Y. The Alashan Terrane did not amalgamate with North China block by the Late Permian: evidence from Carboniferous and Permian paleomagnetic results[J]. Asian Earth Sciences, 2015, 104: 145-159. doi: 10.1016/j.jseaes.2014.02.010

    [24]

    Zhang B H, Zhang J, Zhang Y P, et al. Tectonic affinity of the Alxa Block, Northwest China: Constrained by detrital zircon U-Pb ages from the early Paleozoic strata on its southern and eastern margins[J]. Sedimentary Geology, 2016, 339: 289-303. doi: 10.1016/j.sedgeo.2016.02.017

    [25]

    Zhang S H, Zhao Y, Ye H, et al. Early Neoproterozoic emplacement of the diabase sill swarms in the Liaodong Peninsula and pre-magmatic uplift of the southeastern North China Craton[J]. Precambrian Research, 2016, 272: 203-225. doi: 10.1016/j.precamres.2015.11.005

    [26]

    Zhang W, Pease V, Meng Q P, et al. Discovery of a Neoproterozoic granite in the Northern Alxa region, NW China: its age, petrogenesis and tectonic significance[J]. Geological Magazine, 2016, 153(3): 512-523. doi: 10.1017/S0016756815000631

    [27]

    Song D F, Xiao W J, Collins A S, et al. New chronological constrains on the tectonic affinity of theAlxa Block, NW China[J]. Precambrian Research, 2017, 299: 230-243. doi: 10.1016/j.precamres.2017.07.015

    [28]

    Yuan W, Yang Z Y. The Alashan Terrane was not part of North China by the Late Devonian: evidence from detrital zircon U-Pb geochronology and Hf isotopes[J]. Gondwana Research, 2015, 27(3): 1270-1282. doi: 10.1016/j.gr.2013.12.009

    [29]

    李锦轶, 张进, 曲军峰. 华北与阿拉善两个古陆在早古生代晚期拼合: 来自宁夏牛首山沉积岩系的证据[J]. 地质论评, 2012, 58(2): 208-214. doi: 10.3969/j.issn.0371-5736.2012.02.002

    [30]

    Dan W, Li X H, Wang Q, et al. Phanerozoic amalgamation of the Alxa Block and North China Craton: evidence from Paleozoic granitoids, U-Pb geochronology and Sr-Nd-Pb-Hf-O isotope geochemistry[J]. Gondwana Research, 2016, 32: 105-121. doi: 10.1016/j.gr.2015.02.011

    [31]

    霍福臣, 曹景轩, 董燕生, 等. 贺兰山—阿拉善地区下、中前寒武系的划分对比及其变质、成矿作用特征[J]. 长春地质学院学报, 1987, 17(1): 35-46. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ198701004.htm

    [32]

    沈其韩, 耿元生, 王新社, 等. 阿拉善地区前寒武纪斜长角闪岩的岩石学、地球化学、形成环境和年代学[J]. 岩石矿物学杂志, 2005, 24(1): 21-31. doi: 10.3969/j.issn.1000-6524.2005.01.003

    [33]

    牛鹏飞, 曲军峰, 张进, 等. 狼山地区叠布斯格岩群变形研究及其构造意义[J]. 地质学报, 2019, 93(8): 1867-1884. doi: 10.3969/j.issn.0001-5717.2019.08.005

    [34]

    Ludwig K R. User's Manual forIsoplot 3.0: A geochronological, toolkit for Microsoft Excel[J]. Berkeley Geochronology Center Special Publication, 2003, 4: 1-71.

    [35]

    Anderson T, Griffin W L, Pearson N J. Crustal evolution in the SW part of the Baltic Shield: the Hf isotope evidence[J]. Journal of Petrology, 2002, 43(9), 1725-1747. doi: 10.1093/petrology/43.9.1725

    [36]

    Williams I S. U-Th-Pb geochronology by ion microprobe[J]. Applications of Microanalytical Techniques to Understanding Mineralizing Processes, 1998, 7: 1-35. https://pubs.geoscienceworld.org/segweb/books/book/1220/chapter/107020745/U-Th-Pb-Geochronology-by-Ion-Microprobe

    [37]

    Nasdala L, Gigler A M, Wildner M, et al. Alpha-radiation damage in diamond[C]// Geochimica et Cosmochimica Acta Supplement. 2008: 72.

    [38]

    Black L P, Kamo S L, Allen C M, et al. TEMORA 1: a new zircon standard for Phanerozoic U-Pb geochronology[J]. Chemical Geology, 2003, 200(1/2): 155-170. https://www.sciencedirect.com/science/article/pii/S0009254103001657

    [39]

    Zhang G B, Ireland T, Zhang L F, et al. Zircon geochemistry of two contrasting types ofeclogite: Implications for the tectonic evolution of the North Qaidam UHPM belt, northern Tibet[J]. Gondwana Research, 2016, 35: 27-39. doi: 10.1016/j.gr.2016.04.002

    [40]

    Paton C, Hellstrom J, Paul B, et al. Iolite: Freeware for the visualisation and processing of mass spectrometric data[J]. Journal of Analytical Atomic Spectrometry, 2011, 26(12): 2508-2518. doi: 10.1039/c1ja10172b

    [41]

    Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology[J]. Chemical Geology, 2006, 234: 105-126. doi: 10.1016/j.chemgeo.2006.05.003

    [42]

    Sláma J, Košler J, Condon D J, et al. Plešovice zircon-a new natural reference material for U-Pb and Hf isotopic microanalysis[J]. Chemical Geology, 2008, 249: 1-35. doi: 10.1016/j.chemgeo.2007.11.005

    [43]

    Grant M L, Wilde S A, Wu F, et al. The application of zircon cathodoluminescence imaging, Th-U-Pb chemistry and U-Pb ages in interpreting discrete magmatic and high-grade metamorphic events in the North China Craton at the Archean/Proterozoic boundary[J]. Chemical Geology, 2009, 261(1): 155-171. https://researchers.mq.edu.au/en/publications/the-application-of-zircon-cathodoluminescence-imaging-th-u-pb-che

    [44]

    Xia X P, Sun M, Zhao G C, et al. Paleoproterozoic crustal growth in the Western Block of the North China Craton: evidence from detrital zircon Hf and whole rock Sr-Nd isotope compositions of the khondalites in the Jining Complex[J]. American Journal of Science, 2008, 308: 304-327. doi: 10.2475/03.2008.05

    [45]

    Ma X D, Guo J H, Liu F, et al. Zircon U-Pb ages, trace elements and Nd-Hf isotopic geochemistry of Guyang sanukitoids and related rocks: implications for the Archean crustal evolution of the Yinshan Block, North China Craton[J]. Precambrian Research, 2013, 230: 61-78. doi: 10.1016/j.precamres.2013.02.001

    [46]

    马铭株, 徐仲元, 张连昌, 等. 内蒙古武川西乌兰不浪地区早前寒武纪变质基底锆石SHRIMP定年及Hf同位素组成[J]. 岩石学报, 2013, 29(2): 501-516. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201302012.htm

    [47]

    Wang D, Guo J H, Huang G Y, et al. The Neoarchean ultramafic-mafic complex in the Yinshan Block, North China Craton: Magmatic monitor of development of Archean lithospheric mantle[J]. Precambrian Research, 2015, 270: 80-99. doi: 10.1016/j.precamres.2015.09.002

    [48]

    杨振德, 潘行适, 杨易福. 阿拉善地块及邻区地质构造特征及沉积[M]. 北京: 科学出版社, 1988: 1-254.

    [49]

    李俊健. 内蒙古阿拉善地块区域成矿系统[D]. 中国地质大学(北京)博士学位论文, 2006: 1-117.

    [50]

    张建新, 宫江华. 阿拉善地块性质和归属的再认识[J]. 岩石学报, 2018, 34(4): 940-962. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201804008.htm

    [51]

    Zhao G C, Cawood P A, Wilde S A, et al. Review of global 2.1-1.8 Ga collisional orogens and accreted cratons: a pre-Rodinia supercontinent?[J]Earth-Science Reviews, 2002, (59): 125-162.

    [52]

    Zhao G C, Sun M, Wilde S A, et al. A Paleo-Mesoproterozoic supercontinent: assembly, growth, and breakup[J]. Earth-Science Reviews, 2004, (67): 91-123. https://www.sciencedirect.com/science/article/pii/S0012825204000182

    [53]

    Hou G, Santosh M, Qian X, et al. Configuration of the Late Paleoproterozoic supercontinent Columbia: insights from radiating mafic dyke swarms[J]. Gondwana Research, 2008, (14): 395-409. https://www.sciencedirect.com/science/article/pii/S1342937X08000300

    [54]

    Zhai M G, Guo J H, Liu W J. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton[J]. Journal of Asian Earth Sciences, 2005, 24: 547-561. doi: 10.1016/j.jseaes.2004.01.018

    [55]

    宫江华. 西阿拉善地块早前寒武纪变质基底组成、性质、年代格架及归属[D]. 中国地质科学院博士学位论文, 2013: 1-195.

    [56]

    陈志勇, 杨师帅, 孟二根, 等内蒙古阿拉善左旗巴音诺日公地区前寒武系的厘定[J]. 地质通报, 2004, 23(4): 345-351. doi: 10.3969/j.issn.1671-2552.2004.04.007 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20040467&flag=1

    [57]

    陈志勇, 郑翻身, 王忠, 等. 内蒙古中西部色尔腾山岩群的厘定及其地质意义[J]. 地质与资源, 2007, 23(4): 345-351. https://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200701002.htm

    [58]

    宫江华, 张建新, 于胜尧, 等. 西阿拉善地块~2.5Ga TTG岩石及地质意义[J]. 科学通报, 2012, 57(28/29): 2715-2730. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB2012Z2009.htm

    [59]

    Jian P, Kröner A, Windley B F, et al. Episodic mantle melting crustal reworking in the late Neoarchean of the northwestern North China Craton: Zircon ages of magmatic and metamorphic rocks from the Yinshan Block[J]. Precambrian Research, 2012, 222/223: 230-254. doi: 10.1016/j.precamres.2012.03.002

    [60]

    张维杰, 李龙, 耿明山. 内蒙古固阳地区新太古代侵入岩的岩石特征及时代[J]. 地球科学, 2000, 25(3): 221-226. doi: 10.3321/j.issn:1000-2383.2000.03.001

    [61]

    范宏瑞, 杨奎锋, 胡芳芳, 等. 内蒙古白云鄂博地区基底岩石锆石年代学及对构造背景的指示[J]. 岩石学报, 2010, 26(5): 1342-1350. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201005002.htm

    [62]

    简平, 张旗, 刘敦一, 等. 内蒙古固阳晚太古代赞岐岩(sanukite)——角闪花岗岩的SHRIMP定年及其意义[J]. 岩石学报, 2005, 21(1): 151-157. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200501016.htm

    [63]

    董晓杰, 徐仲元, 刘正宏, 等. 内蒙古大青山北麓2.7Ga花岗质片麻岩的发现及其地质意义[J]. 地球科学, 2012, 37: 20-27. doi: 10.3969/j.issn.1672-6561.2012.01.003

    [64]

    刘平华, 刘福来, 蔡佳, 等. 阴山陆块武川石榴基性麻粒岩P-T条件及其变质时代: 来自相平衡模拟与锆石U-Pb定年的约束[J]. 岩石学报, 2016, 32(7): 1949-1979. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201607003.htm

    [65]

    Wan Y S, Xu Z, Dong C Y, et al. Episodic Paleoproterozoic (~2.45, ~1.95 and ~1.85Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating and whole-rock geochemistry[J]. Precambrian Research, 2013, 224: 71-93. doi: 10.1016/j.precamres.2012.09.014

    [66]

    周喜文, 耿元生. 贺兰山孔兹岩系的变质时代及其对华北克拉通西部陆块演化的制约[J]. 岩石学报, 2009, 25(8): 1843-1852. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200908011.htm

    [67]

    蔡佳, 刘福来, 刘平华, 等. 内蒙古孔兹岩带乌拉山—大青山地区古元古代孔兹岩系年代学研究[J]. 岩石学报, 2015, 31(10): 3081-3106. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201510012.htm

    [68]

    Xia X P, Sun M, Zhao G C, et al. LA-ICP-MS U-Pb geochronology of detrital zircons from the Jining Complex, North China Craton and its tectonic significance[J]. Precambrian Research, 2006, 144: 199-212. doi: 10.1016/j.precamres.2005.11.004

    [69]

    Dong C Y, Wan Y S, Wilde S A, et al. Earliest Paleoproterozoic supracrustal rocks in the North China Craton recognized from the Daqingshan area of the Khondalite Belt: Constraints on craton evolution[J]. Gondwana Research, 2014, 4(25): 1535-1553. https://www.sciencedirect.com/science/article/pii/S1342937X13002074

    [70]

    吴昌华, 李惠民, 钟长汀, 等. 内蒙古黄土窑孔兹岩系的锆石与金红石年龄研究[J]. 地质论评, 1998, 44: 618-626. doi: 10.3321/j.issn:0371-5736.1998.06.009

    [71]

    吴昌华. 华北克拉通的变质沉积岩及其克拉通的构造划分[J]. 高校地质学报, 2007, 13(3): 442-457. doi: 10.3969/j.issn.1006-7493.2007.03.013

    [72]

    Ma M Z, Wan Y S, Santosh M, et al. Decoding multiple tectonothermal events in zircons from single rock samples: SHRIMP zircon U-Pb data from the late Neoarchean rocks of Daqingshan, North China Craton[J]. Gondwana Research, 2012, 22: 810-827. doi: 10.1016/j.gr.2012.02.020

    [73]

    Wan Y S, Song B, Liu D Y, et al. SHRIMP U-Pb zircon geochronology of Paleoproterozoic metasedimentary rocks in the North China Craton: Evidence for a major Late Paleoproterozoic tectonothermal event[J]. Precambrian Research, 2006, 149(3/4): 249-27. https://www.sciencedirect.com/science/article/pii/S0301926806001471

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