The provenance of Salawula Formation in East Kunlun and the tectonic thermal events of provenance: The evidence from U-Pb chronology of detrital zircons
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摘要:
沙松乌拉组出露于东昆中构造混杂岩带，是东昆仑地区原特提斯洋洋盆打开时的沉积记录，确定其地层形成时代、物质来源及恢复构造演化过程，对研究东昆仑地区原特提斯洋的演化具有重要意义。对出露于东昆仑黑海湖—拉宁灶火沟一带的沙松乌拉组进行LA-ICP-MS碎屑锆石U-Pb年定，得到最年轻的锆石年龄为632±6 Ma，结合地层接触关系，为沙松乌拉组的时代划分提供了年龄依据；得到约650 Ma、约800 Ma、980 Ma三个明显峰值及大量未形成明显峰值的其他古老年龄，推测沙松乌拉组的主要物源有小庙群、万保沟群、晋宁期岩浆岩，次要物源为白沙河组。将得到的锆石年龄与各期构造-岩浆活动比对，认为沙松乌拉组的源区经历了古元古代早期构造-岩浆事件、中元古代晚期构造-岩浆事件和新元古代早期构造-岩浆事件。
Abstract:Salawula Formation is the earliest marine deposit of East Kunlun in early Paleozoic.It's meaningful to reconstruct the tectonic evolution of east Kunlun in Early Paleozoic by studying Salawula Formation's formation time and its provenance.The authors obtained the youngest zircon age of 632±6 Ma by LA-ICP-MS U-Pb dating of the detrital zircons from Salawula Formation's clastic rocks and constrained its formation time.Moreover, there are three age ranges of ~650 Ma, ~800 Ma and ~980 Ma existent in the detrital zircons, and the authors infer that Baishahe Group, Xiaomiao Group, Wanbaogou Group and magmatic rocks formed during early Neoproterpzoic were Salawula Formation's provenance because of their similar zircon age distributions.Furthermore, the authors hold that the source areas experienced Early Paleoproterozoic, Late Paleoproterozoic, Late Mesoproterpzoic and Early Neoproterpzoic tectono-magmatic events according to the characteristics of their zircons' U-Pb age.
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表 1 东昆仑沙松乌拉组碎屑锆石LA-ICP-MS U-Th-Pb分析结果
Table 1. The LA-ICP-MS U-Th-Pb analyses of detrital zircons from Salawula Formation in East Kunlun
序号 含量/10-6 Th/U 同位素比值 年龄/Ma 谐和度 Th U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 1 346 539 0.642 0.0723 0.0018 1.7122 0.0424 0.1706 0.0016 995 47 1013 16 1015 9 99% 2 163 289 0.563 0.0652 0.0022 1.1157 0.0361 0.1241 0.0014 780 65 761 17 754 8 99% 3 31.8 43.4 0.732 0.1953 0.0056 15.1344 0.4489 0.5613 0.0077 2787 44 2824 28 2872 32 98% 4 174 279 0.621 0.0800 0.0029 1.5999 0.0558 0.1463 0.0021 1196 64 970 22 880 12 90% 5 206 781 0.263 0.0602 0.0018 0.8680 0.0268 0.1045 0.0011 609 64 634 15 641 7 98% 6 67.8 429 0.158 0.0714 0.0020 1.9556 0.0554 0.1980 0.0021 970 55 1100 19 1165 11 94% 7 48.7 77.3 0.630 0.0713 0.0099 1.0049 0.1384 0.1022 0.0022 966 302 706 70 627 13 59% 8 42.1 68.0 0.619 0.0786 0.0038 1.8572 0.0840 0.1731 0.0025 1162 87 1066 30 1029 14 96% 9 87.0 337 0.258 0.0684 0.0021 1.5980 0.0481 0.1685 0.0021 881 58 969 19 1004 12 96% 10 168 333 0.506 0.2169 0.0055 16.9282 0.4335 0.5573 0.0064 2957 38 2931 25 2855 26 97% 11 77.5 164 0.472 0.1293 0.0038 6.4922 0.1804 0.3593 0.0038 2088 46 2045 24 1979 18 96% 12 104 224 0.464 0.0720 0.0035 1.6887 0.0802 0.1701 0.0020 986 102 1004 30 1013 11 88% 13 128 167 0.770 0.0846 0.0025 2.7198 0.0791 0.2296 0.0025 1307 54 1334 22 1332 13 99% 14 128 178 0.718 0.0850 0.0027 2.6195 0.0774 0.2216 0.0025 1314 54 1306 22 1290 13 98% 15 153 238 0.642 0.0819 0.0027 2.3045 0.0716 0.2022 0.0023 1243 58 1214 22 1187 12 97% 16 63.5 245 0.260 0.0764 0.0030 2.0214 0.0812 0.1908 0.0032 1105 75 1123 27 1126 17 99% 17 214 623 0.343 0.2182 0.0050 17.3081 0.3820 0.5694 0.0051 2967 33 2952 21 2905 21 98% 18 256 550 0.465 0.1313 0.0029 7.1579 0.1587 0.3914 0.0033 2115 37 2131 20 2129 15 99% 19 136 414 0.328 0.0767 0.0021 2.0396 0.0574 0.1912 0.0017 1113 55 1129 19 1128 9 99% 20 246 662 0.372 0.0639 0.0021 0.9128 0.0307 0.1030 0.0010 737 70 659 16 632 6 95% 21 78.3 181 0.433 0.1703 0.0049 10.8328 0.3109 0.4595 0.0050 2561 45 2509 27 2437 22 97% 22 91.7 175 0.524 0.0772 0.0028 1.8118 0.0674 0.1691 0.0019 1126 72 1050 24 1007 10 95% 23 94.3 178 0.529 0.0966 0.0026 3.7276 0.1023 0.2783 0.0030 1560 48 1577 22 1583 15 99% 24 162 198 0.820 0.0757 0.0025 1.9547 0.0655 0.1866 0.0023 1086 64 1100 23 1103 12 99% 25 118 211 0.560 0.0913 0.0027 3.2390 0.0932 0.2569 0.0030 1452 51 1467 22 1474 15 99% 26 166 209 0.794 0.0721 0.0025 1.8513 0.0627 0.1863 0.0023 990 66 1064 22 1102 13 96% 27 213 161 1.324 0.0694 0.0026 1.5862 0.0573 0.1658 0.0019 910 72 965 22 989 11 97% 28 92.8 424 0.219 0.0752 0.0022 1.7418 0.0516 0.1670 0.0015 1074 58 1024 19 995 8 97% 29 265 274 0.969 0.0741 0.0023 1.7271 0.0549 0.1685 0.0018 1044 62 1019 20 1004 10 98% 30 176 294 0.598 0.0826 0.0024 2.6513 0.0801 0.2319 0.0026 1259 56 1315 22 1344 14 97% 31 190 380 0.500 0.0790 0.0022 2.3272 0.0696 0.2123 0.0023 1171 56 1221 21 1241 12 98% 32 207 511 0.405 0.0726 0.0020 1.5475 0.0423 0.1538 0.0014 1004 54 949 17 922 8 97% 33 79.1 213 0.372 0.0755 0.0024 1.8849 0.0596 0.1801 0.0018 1081 62 1076 21 1067 10 99% 34 306 531 0.577 0.0754 0.0020 1.8441 0.0483 0.1760 0.0016 1078 51 1061 17 1045 9 98% 35 254 360 0.705 0.0764 0.0023 1.8690 0.0528 0.1766 0.0020 1106 53 1070 19 1048 11 97% 36 131 396 0.330 0.0856 0.0023 2.7588 0.0756 0.2319 0.0027 1329 49 1344 20 1344 14 99% 37 34.7 356 0.098 0.0680 0.0026 1.1794 0.0426 0.1258 0.0015 868 80 791 20 764 8 94% 38 235 168 1.402 0.2283 0.0061 20.3261 0.5250 0.6383 0.0084 3040 36 3107 25 3182 33 97% 39 241 538 0.448 0.0627 0.0027 0.9406 0.0387 0.1080 0.0014 697 85 673 20 661 8 98% 40 206 256 0.805 0.0717 0.0033 1.7063 0.0738 0.1722 0.0026 977 85 1011 28 1024 14 98% 41 207 402 0.514 0.0732 0.0026 1.8674 0.0653 0.1834 0.0027 1019 66 1070 23 1086 15 98% 42 291 467 0.623 0.0679 0.0025 1.6154 0.0602 0.1704 0.0025 866 73 976 23 1014 14 96% 43 97.9 130 0.755 0.1012 0.0064 4.0284 0.2423 0.2888 0.0058 1645 121 1640 49 1636 29 95% 44 566 1882 0.301 0.0729 0.0018 1.8568 0.0460 0.1828 0.0019 1012 47 1066 16 1082 10 98% 45 227 474 0.479 0.1768 0.0042 12.7483 0.3041 0.5180 0.0057 2623 36 2661 22 2691 24 98% 46 247 586 0.421 0.0681 0.0025 1.4110 0.0528 0.1492 0.0019 870 75 894 22 897 11 99% 47 113 155 0.732 0.0890 0.0041 3.2248 0.1484 0.2630 0.0047 1405 83 1463 36 1505 24 97% 48 692 961 0.721 0.0708 0.0024 1.6779 0.0556 0.1716 0.0020 951 65 1000 21 1021 11 97% 49 111 136 0.818 0.0668 0.0045 1.2993 0.0850 0.1440 0.0029 831 133 845 38 867 16 97% 50 634 1312 0.483 0.0887 0.0021 3.1731 0.0774 0.2563 0.0025 1399 44 1451 19 1471 13 98% 51 804 831 0.968 0.0688 0.0022 1.6756 0.0554 0.1747 0.0022 893 65 999 21 1038 12 96% 52 473 1593 0.297 0.0670 0.0020 1.5659 0.0451 0.1670 0.0019 839 56 957 18 995 11 96% 53 62.1 174 0.357 0.0783 0.0079 1.7627 0.1730 0.1632 0.0034 1155 207 1032 64 975 19 64% 54 652 1048 0.622 0.0684 0.0020 1.5375 0.0429 0.1615 0.0019 880 53 945 17 965 11 97% 55 695 3327 0.209 0.0697 0.0017 1.5446 0.0368 0.1587 0.0015 918 46 948 15 950 8 99% 56 793 1187 0.668 0.1340 0.0034 7.7483 0.1931 0.4146 0.0040 2151 41 2202 22 2236 18 98% 57 148 302 0.489 0.0700 0.0032 1.4335 0.0634 0.1493 0.0022 928 88 903 26 897 12 99% 58 226 265 0.853 0.0665 0.0036 1.0787 0.0562 0.1188 0.0019 821 106 743 27 723 11 97% 59 92.1 108 0.857 0.0949 0.0099 2.4818 0.2537 0.1898 0.0040 1525 205 1267 74 1120 22 76% 60 913 1851 0.494 0.0762 0.0021 2.0615 0.0702 0.1928 0.0037 1101 58 1136 23 1137 20 99% 61 158 1134 0.140 0.0770 0.0022 2.0070 0.0556 0.1869 0.0016 1122 54 1118 19 1105 9 98% 62 344 281 1.223 0.0807 0.0034 2.1956 0.0874 0.1979 0.0027 1213 75 1180 28 1164 14 98% 63 189 289 0.653 0.0649 0.0024 1.0387 0.0382 0.1151 0.0015 771 74 723 19 702 9 97% 64 653 404 1.616 0.0657 0.0020 1.3557 0.0405 0.1481 0.0015 796 60 870 17 890 9 97% 65 328 417 0.786 0.1893 0.0041 14.2205 0.3054 0.5381 0.0053 2736 32 2765 20 2776 22 99% 66 95.0 168 0.565 0.0733 0.0024 1.9165 0.0643 0.1877 0.0025 1023 64 1087 22 1109 14 97% 67 68.2 78.0 0.874 0.0778 0.0041 1.5725 0.0831 0.1478 0.0028 1141 101 959 33 888 15 92% 68 183 248 0.739 0.0679 0.0024 1.4681 0.0518 0.1559 0.0020 866 70 917 21 934 11 98% 69 59.4 177 0.335 0.0705 0.0027 1.7359 0.0657 0.1780 0.0024 943 74 1022 24 1056 13 96% 70 104 174 0.597 0.0689 0.0030 1.5689 0.0669 0.1655 0.0022 894 85 958 26 987 12 97% 71 235 248 0.946 0.0798 0.0026 2.0482 0.0683 0.1848 0.0020 1191 64 1132 23 1093 11 96% 72 118 264 0.448 0.0836 0.0028 2.4641 0.0819 0.2127 0.0023 1282 63 1262 24 1243 12 98% 73 116 215 0.539 0.0701 0.0024 1.8032 0.0670 0.1847 0.0027 931 72 1047 24 1092 14 95% 74 345 557 0.619 0.0772 0.0021 1.9410 0.0541 0.1805 0.0020 1127 52 1095 19 1070 11 97% 75 66.6 486 0.137 0.0752 0.0020 2.0237 0.0545 0.1932 0.0020 1075 51 1123 18 1139 11 98% 76 392 505 0.776 0.0751 0.0020 1.9515 0.0532 0.1860 0.0020 1071 52 1099 18 1100 11 99% 77 102 372 0.275 0.0720 0.0025 1.6729 0.0562 0.1665 0.0019 987 66 998 21 993 11 99% 78 65.5 122 0.536 0.0796 0.0034 1.8452 0.0760 0.1671 0.0024 1188 78 1062 27 996 13 93% 79 159 331 0.481 0.0768 0.0023 1.8863 0.0566 0.1760 0.0019 1115 57 1076 20 1045 11 97% 80 150 379 0.397 0.0743 0.0023 2.0588 0.0664 0.1977 0.0019 1050 63 1135 22 1163 10 97% 81 423 613 0.690 0.0905 0.0022 3.1065 0.0733 0.2457 0.0022 1437 43 1434 18 1416 12 98% 82 110 149 0.739 0.0724 0.0046 1.5536 0.0971 0.1556 0.0022 998 134 952 39 932 12 92% 83 80.6 320 0.252 0.0741 0.0023 1.8898 0.0586 0.1831 0.0020 1044 60 1078 21 1084 11 99% 84 35.0 51.7 0.676 0.0704 0.0038 1.7330 0.0935 0.1786 0.0033 939 106 1021 35 1059 18 96% 85 19.4 58.2 0.334 0.0738 0.0038 1.5306 0.0786 0.1523 0.0028 1037 99 943 32 914 16 96% 86 22.8 102 0.224 0.0693 0.0036 1.4621 0.0721 0.1529 0.0021 908 100 915 30 917 12 99% 87 110 500 0.220 0.1492 0.0040 8.6318 0.2243 0.4127 0.0045 2336 41 2300 24 2227 21 96% 88 154 432 0.356 0.0680 0.0025 1.3784 0.0476 0.1454 0.0017 867 69 880 20 875 9 99% 89 120 228 0.528 0.0770 0.0041 1.8998 0.0971 0.1790 0.0026 1120 109 1081 34 1062 14 89% 注：谐和度=100×(1-abs(68Age-75Age)/((68Age+75Age)/2)) 
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① 中国地质大学(武汉).1: 5万黑海幅区域地质调查报告.2014.
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