The detrital zircon LA-ICP-MS U-Pb age of Early Permian Shoushangou Formation in Hanwula area of Xi Ujimqin Banner, Inner Mongolia, and its significance
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摘要:
中亚造山带南缘二叠纪的构造背景一直存在争议。以内蒙古西乌旗罕乌拉地区发育的寿山沟组为研究对象，开展了野外地质、岩石学、碎屑锆石LA-ICP-MS U-Pb年龄研究。2个样品锆石阴极发光图像和Th/U值指示，锆石为岩浆成因锆石。103颗碎屑锆石年龄测试结果显示，年龄信息可划分为5组：285~328Ma，峰期年龄302Ma；338~361Ma；455~490Ma；757Ma；1278Ma、2380Ma。最年轻的年龄为285Ma，结合侵入其中的花岗岩同位素年龄，指示西乌旗罕乌拉地区寿山沟组沉积时限介于285~280Ma之间，主体沉积时代应为早二叠世Sakmarian期—Artinskian期。寿山沟组碎屑锆石反映出近源、快速沉积的特点，沉积物源中含有较多的火山碎屑物，可能代表弧后盆地沉积，为早二叠世古亚洲洋闭合前洋壳俯冲消减作用的沉积响应。结合区域资料，寿山沟组碎屑锆石的年龄对应于东北地区的变质基底及其后的构造岩浆事件，物源区物质主要来自于苏尼特左旗—锡林浩特—西乌旗一带早石炭世末—晚石炭世岩浆弧及贺根山—东乌旗一带，并进一步限制了华北与西伯利亚两大板块的缝合线应位于寿山沟组发育地区的南部，即索伦缝合带，拼合时代最可能为晚二叠世—早三叠世。
Abstract:There exist different opinions concerning the structural setting of southern Central Asia Orogenic Belt (CAOB) in the Permian period. The authors studied the Shoushangou Formation in Hanwula area of Xi Ujimqin Banner, Inner Mongolia, in such aspects as field occurrence, petrology, and detrital zircon U-Pb isotopic geochronology. The result shows that the cathodoluminescence (CL) images of analyzed zircons of two samples from Shoushangou Formation and their Th/U ratios imply the igneous origin. And the ages of total 103 detrital zircons can be mainly divided into 5 groups:285~328Ma (peak age being 302Ma), 338~361Ma, 455~490Ma (Early Paleozoic), 757Ma (Neoproterozoic)and the fifth group including 1278Ma and 2380Ma (Mesoproterozoic- Paleoproterozoic).The youngest age of dating zircons is 285Ma. Together with the age of the granite that intruded into it, the authors have come to the conclusion that the sedimentary age of the Shoushangou Formation ranges from 285Ma to 280Ma, with the main deposition epoch being the Sakmarian -Artinskian stage of Early Permian. The detrital zircons of Shoushangou Formation indicate that the investigated rocks are immature, probably due to the results of rapid erosion, transport, and diagenetic process and nearby supply derived from the nearby source. Additionally, lots of volcanic clastics were found in the provenance of the Shoushangou Formation. All these characteristics suggest that the Shoushangou Formation was most probably formed in a back-arc spreading environment triggered by oceanic crust subduction before closure of the Paleoasian Ocean in Early Permian. Combined with the regional geology and timing of the magmatism, it is concluded that the detrital zircons of the Shoushangou Formation reflect the information of the metamorphic basement and following tectonomagmatic event in Northeast China, and the provenance of Shoushangou Formation mainly came from the Paleozoic granitoids and volcanic rocks in the Sonid Zuoqi-Xilin Hot-Xi Ujimqin Banner area, with the probable addition of materials from Hegenshan-Dong Ujimqin Banner area. Therefore, the suture zone between the North China and Siberia plate is situated in the south of Shoushangou Formation, which is located along the the Solonker suture zone, and the timing for the final collision might be Late Permian-Early Triassic.
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表 1 寿山沟组LA-ICP-MS碎屑锆石U-Th-Pb同位素分析结果
Table 1. LA-ICP-MS U-Th-Pb data of detrital zircons from Shoushangou Formation
点号 含量/10-6 同位素比值 年龄/Ma Pb U 207Pb/
206Pb1σ 207Pb/
235U1σ 206Pb/
238U1σ 208Pb/
232Th1σ 232Th/
238U1σ 207Pb/
206Pb1σ 207Pb/
235U1σ 206Pb/
238U1σ Pm19B31 1 3 53 0.0526 0.0066 0.358 0.044 0.0480 0.0006 0.0085 0.0007 0.557 0.005 312 284 310 38 302 4 2 8 172 0.0519 0.0028 0.330 0.018 0.0461 0.0005 0.0077 0.0002 0.876 0.007 279 124 289 16 290 3 3 1 28 0.0528 0.0106 0.349 0.066 0.0472 0.0008 0.0128 0.0024 0.454 0.004 320 458 304 58 298 5 4 2 30 0.0514 0.0107 0.362 0.070 0.0498 0.0008 0.0117 0.0018 0.607 0.005 260 476 314 61 313 5 5 7 119 0.0765 0.0028 0.540 0.021 0.0509 0.0005 0.0181 0.0006 0.588 0.005 1107 74 438 17 320 3 6 3 57 0.0527 0.0057 0.354 0.038 0.0476 0.0006 0.0150 0.0008 0.599 0.005 316 246 308 33 300 3 7 11 206 0.0538 0.0019 0.353 0.013 0.0476 0.0005 0.0128 0.0002 0.674 0.007 361 82 307 11 299 3 8 14 258 0.0542 0.0019 0.359 0.013 0.0481 0.0005 0.0167 0.0003 0.845 0.007 378 79 312 11 303 3 9 13 258 0.0529 0.0014 0.352 0.010 0.0481 0.0005 0.0148 0.0003 0.406 0.005 326 60 306 8 303 3 10 3 53 0.0504 0.0050 0.350 0.035 0.0489 0.0005 0.0152 0.0008 0.624 0.005 211 232 305 30 308 3 11 30 540 0.0543 0.0012 0.354 0.008 0.0472 0.0005 0.0158 0.0002 0.946 0.010 384 48 308 7 298 3 12 44 872 0.0519 0.0008 0.351 0.006 0.0491 0.0005 0.0144 0.0001 0.503 0.006 282 35 306 5 309 3 13 65 1163 0.0535 0.0008 0.375 0.006 0.0509 0.0005 0.0186 0.0001 0.558 0.006 349 36 323 5 320 3 14 18 360 0.0538 0.0011 0.354 0.008 0.0477 0.0005 0.0159 0.0002 0.563 0.005 361 47 307 7 300 3 15 3 48 0.0539 0.0064 0.367 0.044 0.0492 0.0006 0.0152 0.0011 0.613 0.005 366 268 317 38 310 4 16 2 46 0.0536 0.0092 0.334 0.055 0.0452 0.0007 0.0220 0.0013 0.665 0.006 356 385 293 48 285 4 17 18 344 0.0527 0.0011 0.349 0.008 0.0480 0.0005 0.0185 0.0002 0.497 0.005 315 49 304 7 302 3 18 15 288 0.0533 0.0015 0.354 0.010 0.0482 0.0005 0.0189 0.0002 0.532 0.006 340 62 308 9 303 3 19 4 89 0.0551 0.0036 0.351 0.023 0.0459 0.0005 0.0151 0.0007 0.572 0.004 416 146 306 20 290 3 20 5 80 0.0534 0.0041 0.374 0.029 0.0504 0.0005 0.0261 0.0007 0.515 0.004 344 174 322 25 317 3 21 44 861 0.0521 0.0008 0.345 0.006 0.0481 0.0005 0.0197 0.0001 0.441 0.003 288 36 301 5 303 3 22 32 601 0.0524 0.0009 0.348 0.006 0.0482 0.0005 0.0218 0.0001 0.449 0.004 301 39 303 6 304 3 23 78 1218 0.0861 0.0013 0.608 0.010 0.0512 0.0005 0.0341 0.0002 0.539 0.004 1340 29 482 8 322 3 24 2 38 0.0543 0.0073 0.372 0.0499 0.0497 0.0007 0.0330 0.0012 0.717 0.006 385 303 321 43 313 4 25 9 156 0.0525 0.0027 0.339 0.017 0.0468 0.0005 0.0255 0.0003 0.828 0.008 309 115 296 15 295 3 26 2 31 0.0524 0.0102 0.342 0.067 0.0474 0.0008 0.0292 0.0015 0.642 0.005 303 445 299 58 298 5 27 10 177 0.0527 0.0017 0.350 0.011 0.0481 0.0005 0.0238 0.0002 0.708 0.007 315 72 304 10 303 3 28 27 476 0.0541 0.0012 0.357 0.008 0.0479 0.0005 0.0352 0.0003 0.436 0.003 373 51 310 7 302 3 29 26 452 0.0532 0.0011 0.357 0.008 0.0486 0.0005 0.0325 0.0002 0.437 0.004 339 46 310 6 306 3 30 26 333 0.0779 0.0015 0.534 0.011 0.0496 0.0005 0.0387 0.0002 0.911 0.013 1145 38 434 9 312 3 31 8 103 0.0543 0.0038 0.359 0.025 0.0480 0.0005 0.0392 0.0003 0.919 0.008 382 157 312 22 302 3 32 14 217 0.0536 0.0021 0.350 0.014 0.0473 0.0005 0.0403 0.0003 0.551 0.006 355 88 304 12 298 3 33 25 350 0.0543 0.0013 0.362 0.009 0.0483 0.0005 0.0407 0.0001 0.761 0.006 383 54 313 8 304 3 34 19 239 0.1195 0.0027 0.788 0.019 0.0478 0.0005 0.0577 0.0005 0.684 0.009 1948 41 590 14 301 3 35 15 192 0.1228 0.0029 0.868 0.021 0.0512 0.0005 0.0683 0.0004 0.481 0.009 1997 41 635 16 322 3 36 35 332 0.2133 0.0033 1.458 0.024 0.0496 0.0005 0.0721 0.0004 0.828 0.010 2931 25 913 15 312 3 37 18 252 0.0534 0.0016 0.361 0.011 0.0490 0.0005 0.0323 0.0001 1.009 0.013 345 67 313 9 309 3 38 29 366 0.0528 0.0012 0.367 0.009 0.0504 0.0005 0.0371 0.0001 0.985 0.007 320 53 317 8 317 3 39 20 247 0.0548 0.0014 0.394 0.011 0.0521 0.0005 0.0331 0.0001 1.106 0.015 403 58 337 9 328 3 40 36 661 0.0540 0.0009 0.355 0.006 0.0476 0.0005 0.0227 0.0001 0.577 0.005 373 37 308 5 300 3 41 14 248 0.0539 0.0016 0.346 0.010 0.0466 0.0004 0.0189 0.0002 0.741 0.006 366 66 302 9 294 3 42 33 611 0.0524 0.0009 0.360 0.007 0.0499 0.0005 0.0193 0.0001 0.527 0.004 302 40 312 6 314 3 43 24 383 0.0532 0.0010 0.394 0.008 0.0538 0.0005 0.0254 0.0002 0.593 0.005 339 44 338 7 338 3 44 77 915 0.0818 0.0012 0.575 0.009 0.0510 0.0005 0.0267 0.0002 1.559 0.011 1240 29 461 7 321 3 45 12 139 0.0540 0.0023 0.406 0.017 0.0545 0.0005 0.0631 0.0004 0.602 0.005 371 95 346 15 342 3 46 33 313 0.0536 0.0012 0.361 0.009 0.0488 0.0005 0.0530 0.0001 1.308 0.015 356 52 313 7 307 3 47 26 298 0.0556 0.0013 0.390 0.009 0.0509 0.0005 0.0770 0.0002 0.604 0.005 435 51 334 8 320 3 48 28 218 0.0530 0.0018 0.377 0.013 0.0514 0.0005 0.0748 0.0001 1.242 0.011 329 77 325 11 323 3 49 13 94 0.0792 0.0033 0.632 0.027 0.0576 0.0006 0.1460 0.0006 0.644 0.011 1177 81 498 21 361 4 50 11 133 0.0531 0.0030 0.353 0.020 0.0481 0.0005 0.0840 0.0005 0.568 0.008 332 127 307 17 303 3 51 16 143 0.0658 0.0027 0.455 0.019 0.0503 0.0005 0.0882 0.0003 0.831 0.007 799 87 381 16 316 3 52 4 64 0.0523 0.0056 0.344 0.037 0.0473 0.0005 0.0543 0.0010 0.523 0.007 299 246 300 32 298 3 53 9 95 0.0549 0.0034 0.357 0.022 0.0469 0.0005 0.0434 0.0002 1.371 0.012 410 137 310 19 295 3 54 5 87 0.0529 0.0040 0.344 0.026 0.0466 0.0005 0.0304 0.0005 0.651 0.006 323 172 300 23 294 3 55 19 330 0.0507 0.0013 0.328 0.009 0.0469 0.0005 0.0229 0.0001 0.805 0.006 229 60 288 8 296 3 56 36 683 0.0557 0.0009 0.373 0.006 0.0485 0.0005 0.0147 0.0001 0.627 0.007 441 36 322 6 306 3 57 12 215 0.0532 0.0019 0.345 0.013 0.0470 0.0005 0.0126 0.0001 1.084 0.009 339 80 301 11 296 3 58 12 224 0.0535 0.0016 0.353 0.011 0.0478 0.0005 0.0154 0.0004 0.661 0.016 350 70 307 10 301 3 59 20 398 0.0548 0.0011 0.371 0.008 0.0492 0.0005 0.0132 0.0002 0.535 0.006 403 46 321 7 310 3 60 36 678 0.0538 0.0009 0.352 0.006 0.0475 0.0005 0.0103 0.0001 0.999 0.009 361 38 307 6 299 3 61 3 49 0.0531 0.0091 0.361 0.060 0.0481 0.0006 0.0118 0.0008 0.906 0.008 332 391 313 52 303 4 62 39 757 0.0531 0.0010 0.333 0.008 0.0455 0.0005 0.0089 0.0002 1.349 0.031 332 44 292 7 287 3 63 11 228 0.0540 0.0018 0.358 0.012 0.0481 0.0005 0.0091 0.0003 0.605 0.009 369 73 311 10 303 3 B1401 1 4 72 0.0889 0.0049 0.618 0.036 0.0504 0.0004 0.0211 0.0005 0.506 0.001 1402 106 488 28 317 3 2 5 93 0.0847 0.0029 0.532 0.019 0.0455 0.0003 0.0195 0.0003 0.522 0.005 1309 66 433 15 287 2 3 46
81166 0.1530 0.0011 8.205 0.060 0.3888 0.0019 0.1177 0.0002 0.130 0.002 2380 12 2254 17 2117 10 4 41 555 0.0569 0.0006 0.612 0.006 0.0781 0.0004 0.0260 0.0003 0.141 0.001 486 23 485 5 485 3 5 10 194 0.0862 0.0022 0.556 0.014 0.0468 0.0003 0.0243 0.0003 0.348 0.002 1342 50 449 11 295 2 6 13 269 0.0672 0.0016 0.452 0.010 0.0488 0.0003 0.0204 0.0003 0.285 0.002 845 48 379 8 307 2 7 9 178 0.0596 0.0018 0.397 0.012 0.0483 0.0003 0.0201 0.0003 0.295 0.001 589 66 339 11 304 2 8 42 750 0.0573 0.0006 0.379 0.004 0.0479 0.0002 0.0184 0.0001 0.788 0.007 504 22 326 3 302 1 9 7 127 0.0880 0.0043 0.565 0.030 0.0466 0.0003 0.0310 0.0011 0.369 0.003 1382 93 455 24 293 2 10 20 332 0.0679 0.0014 0.456 0.010 0.0486 0.0003 0.0262 0.0002 0.616 0.006 866 44 381 8 306 2 11 23 397 0.0850 0.0014 0.530 0.010 0.0452 0.0002 0.0254 0.0003 0.700 0.002 1316 32 431 8 285 1 12 22 360 0.0854 0.0033 0.594 0.025 0.0505 0.0003 0.0318 0.0009 0.536 0.003 1325 74 474 20 317 2 13 4 67 0.0861 0.0038 0.580 0.026 0.0488 0.0003 0.0304 0.0006 0.617 0.006 1340 85 464 20 307 2 14 21 362 0.0582 0.0011 0.383 0.007 0.0477 0.0002 0.0271 0.0002 0.653 0.001 537 40 329 6 301 2 15 7 101 0.0879 0.0026 0.594 0.019 0.0490 0.0003 0.0258 0.0004 0.965 0.004 1380 58 473 15 309 2 16 68 894 0.0583 0.0005 0.588 0.005 0.0731 0.0004 0.0424 0.0002 0.248 0.001 541 18 469 4 455 2 17 5 81 0.0675 0.0057 0.452 0.040 0.0486 0.0004 0.0315 0.0006 0.537 0.001 853 174 379 33 306 3 18 7 115 0.0554 0.0021 0.365 0.014 0.0479 0.0003 0.0273 0.0003 0.609 0.003 426 83 316 12 301 2 19 28 516 0.0557 0.0008 0.368 0.005 0.0479 0.0002 0.0232 0.0001 0.505 0.001 441 32 318 5 301 1 20 23 434 0.0636 0.0013 0.422 0.009 0.0481 0.0002 0.0249 0.0002 0.375 0.001 728 43 357 7 303 1 21 12 211 0.0653 0.0022 0.440 0.015 0.0488 0.0003 0.0204 0.0003 0.584 0.001 784 70 370 12 307 2 22 57 610 0.0882 0.0011 0.960 0.010 0.0789 0.0006 0.0618 0.0006 0.345 0.004 1387 25 683 7 490 4 23 9 154 0.0543 0.0027 0.357 0.018 0.0477 0.0003 0.0205 0.0003 0.789 0.002 383 110 310 16 300 2 24 29 459 0.0592 0.0018 0.393 0.012 0.0482 0.0002 0.0232 0.0001 0.991 0.002 574 65 337 10 303 2 25 12 194 0.0867 0.0041 0.662 0.036 0.0554 0.0005 0.0267 0.0007 0.510 0.001 1353 91 516 28 347 3 26 20 397 0.0519 0.0012 0.340 0.007 0.0474 0.0004 0.0167 0.0003 0.433 0.001 281 53 297 6 299 3 26 20 397 0.0519 0.0012 0.340 0.007 0.0474 0.0004 0.0167 0.0003 0.433 0.001 281 53 297 6 299 3 27 11 211 0.0548 0.0013 0.362 0.009 0.0479 0.0002 0.0121 0.0002 0.881 0.023 405 53 314 7 302 2 28 11 209 0.0711 0.0018 0.483 0.012 0.0493 0.0003 0.0188 0.0003 0.402 0.004 961 51 400 10 310 2 29 8 142 0.0645 0.0019 0.431 0.013 0.0484 0.0003 0.0158 0.0002 0.616 0.002 757 63 364 11 305 2 30 7 143 0.0856 0.0090 0.535 0.063 0.0453 0.0005 0.0177 0.0013 0.586 0.004 1329 203 435 51 286 3 31 6 99 0.0901 0.0040 0.629 0.033 0.0506 0.0003 0.0187 0.0006 0.856 0.013 1427 85 495 26 318 2 32 44 354 0.0879 0.0012 1.510 0.017 0.1246 0.0009 0.0354 0.0006 0.260 0.002 1380 25 934 11 757 5 33 51 292 0.0834 0.0007 2.019 0.016 0.1756 0.0009 0.0574 0.0010 0.194 0.003 1278 17 1122 9 1043 5 34 52 937 0.0712 0.0010 0.483 0.007 0.0492 0.0002 0.0144 0.0001 0.773 0.003 963 30 400 6 309 1 35 17 301 0.0896 0.0027 0.614 0.027 0.0497 0.0004 0.0197 0.0008 0.466 0.002 1416 58 486 21 313 2 36 13 246 0.0884 0.0012 0.581 0.008 0.0476 0.0002 0.0156 0.0002 0.569 0.008 1391 27 465 7 300 2 37 16 275 0.0697 0.0010 0.473 0.007 0.0492 0.0002 0.0155 0.0001 0.801 0.003 918 29 393 5 310 2 38 12 222 0.0743 0.0012 0.503 0.008 0.0491 0.0002 0.0154 0.0001 0.759 0.001 1050 32 414 7 309 2 39 22 386 0.0886 0.0026 0.628 0.020 0.0514 0.0003 0.0167 0.0003 0.623 0.002 1396 56 495 16 323 2 40 16 273 0.0883 0.0016 0.617 0.011 0.0507 0.0002 0.0159 0.0001 0.748 0.002 1390 35 488 9 319 2 41 28 571 0.0861 0.0013 0.548 0.009 0.0461 0.0002 0.0123 0.0002 0.548 0.004 1341 29 444 8 291 2 42 27 529 0.0876 0.0024 0.565 0.017 0.0467 0.0002 0.0155 0.0004 0.473 0.001 1374 52 455 14 294 2 43 6 109 0.0875 0.0025 0.595 0.018 0.0493 0.0003 0.0160 0.0003 0.604 0.003 1372 54 474 14 310 2 44 7 152 0.0676 0.0028 0.453 0.020 0.0486 0.0003 0.0078 0.0003 0.397 0.007 855 85 379 16 306 2 
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表 2 主要构造岩浆事件年龄值统计
Table 2. The dating results of main geological events
事件 地质体 年龄 测试方法 资料来源 早二叠世早期岩浆事件 白音乌拉-东乌旗碱性-碱长花岗岩带 286~279Ma Rb-Sr [23] 白音乌拉正长花岗岩 293~294Ma SHRIMP [84] 白音乌拉-东乌旗罕布音布敦岩体 295.1±2.8Ma LA-ICP-MS [59] 东乌旗京格斯台碱性花岗岩 284.8±1.1Ma TIMS [60] 贺根山浩雅尔洪克尔玄武岩 294±30Ma LA-ICP-MS [59] 贺根山西南块状玄武岩 292.9±0.6Ma Ar-Ar [15] 朝克山辉长岩、基性脉岩 295±15Ma、298±9Ma SHRIMP [15] 晚石炭世—早石炭世末岩浆事件 苏左旗白音宝力道岩体 309Ma SHRIMP [28] 锡林浩特东南石榴石花岗岩 316士3Ma SHRIMP [53] 锡林浩特片麻状二长花岗岩、花岗闪长岩 316.5±1.8Ma、324±2.4Ma SHRIMP [42] 锡林浩特水库地区Ⅰ型花岗岩 317.0±4.0Ma LA-ICP-MS [77] 维拉斯托石英闪长岩和闪长岩、拜仁达坝花岗闪长岩 310±2Ma、11±2Ma SHRIMP [62] 以及道伦达坝英安质晶屑凝灰岩 319±3Ma、300±5Ma 锡林浩特变质基性火山岩 334.5±3.5Ma、323.4±2.4Ma LA-ICP-MS [79] 西乌旗达其浑迪、金星石英闪长岩 325±3Ma、322±3Ma LA-ICP-MS [76] 西乌旗巴音高勒苏木白音陶勒盖二云母花岗岩 316.7±2.1Ma LA-ICP-MS [59] 西乌旗白音高勒石英闪长岩 313~323Ma SHRIMP [54] 西乌旗梅劳特乌拉蛇绿岩中块状辉长岩 308.5±2.2Ma LA-ICP-MS [78] 苏尼特右旗本巴图组安山岩 300.9 ± 1.6 Ma LA-ICP-MS [80] 西乌旗达青牧场本巴图组片理化火山岩 318.4±3.4Ma、315.4±4.4Ma LA-ICP-MS [59] 扎鲁特旗巴雅尔吐胡硕本巴图组凝灰岩 323.9±3.5Ma LA-ICP-MS [59] 查干诺尔地区本巴图组火山岩 308~313Ma SHRIMP [81] 东乌旗狠麦温都尔二长花岗岩、正长花岗岩 307.0±1.9Ma、299.7±5.3 Ma SHRIMP [65] 东乌珠穆沁旗阿木古楞岩体含巨斑二长花岗岩 314.2±2.2Ma LA-ICP-MS [70] 莫若格钦二长闪长岩 312.6±4.1M a SHRIM P [64] 白音乌拉地区宝力高庙组流纹岩 300.0±2.9Ma SHRIMP [82] 东乌旗狠麦温都尔宝力高庙组火山岩 305~320Ma SHRIMP [63] 东乌旗格根敖包组火山岩 307.3±0.99Ma、311.6±1.3Ma LA-ICP-MS [83] 贺根山格根敖包组晶屑凝灰岩 323±3Ma LA-ICP-MS [22] 贺根山蛇绿岩中辉长闪长岩和玄武岩 341±3Ma和359±5Ma LA-ICP-MS [22] 早古生代岩浆事件 苏左旗地区闪长-花岗岩 464~490Ma SHRIMP [86] 锡林浩特片麻状电气石二云母花岗岩 458.8Ma SHRIMP [42] 小兴安岭片麻状花岗闪长岩-二长花岗岩、花岗闪长 508±15Ma、499±1Ma Rb-Sr [89] 岩-二长花岗岩、碱长-碱性花岗岩 、471±3Ma LA-ICP-MS 黑龙江东南部穆棱地区片麻状花岗岩 486±3Ma SHRIMP [91] 钾长花岗岩 461±6Ma SHRIMP [91] 额尔古纳地块塔河花岗岩 480~494Ma LA-ICP-MS [90] 大兴安岭东北部早古生代花岗岩 460~500Ma LA-ICP-MS [88] 松辽盆地基底变质岩锆石年龄 448Ma (424~490Ma) LA-ICP-MS [93-94] 兴华渡口群变火成岩 506±10~547±46Ma SHRIMP [92] 扎兰屯变质杂岩碎屑锆石 481~580Ma，峰期529Ma LA-ICP-MS [95] 额尔古纳地块漠河杂岩 494±3Ma LA-ICP-MS [99] 兴安地块兴华渡口群 496±7Ma LA-ICP-MS [98] 松辽地块铁力变质杂岩 514±5Ma LA-ICP-MS [100] 兴凯地块虎头杂岩 490±4Ma LA-ICP-MS [103-104] 佳木斯地块麻山群的岩浆锆石年龄 515Ma SHRIMP [96-97] 新元古代岩浆事件 “黑龙江群”中斜长角闪片岩结晶年龄 777±18Ma SHRIMP [91] 锡林浩特地区变辉长岩年龄 739.6±19.3Ma SHRIMP [42] 大兴安岭碧水一带碱性长石花岗、花岗闪长岩 795±13Ma、792±5Ma LA-ICP-MS [101] 大兴安岭满归一带碱性长石花岗岩 927±13Ma LA-ICP-MS [101] 大兴安岭奇乾一带二长花岗岩 817±6Ma LA-ICP-MS [101] 大兴安岭地区兴华渡口群片麻岩 843±6Ma LA-ICP-MS [101] 黑龙江东南秣陵地区麻山群 843~1004Ma SHRIMP [91] 佳木斯地块麻山群石榴石麻粒岩碎屑锆石 843~1004Ma SHRIMP [96-97] 佳木斯地块麻山群夕线石榴片麻岩 687~962Ma， LA-ICP-MS [98-99] 兴凯地块夕线石榴片麻岩的核部年龄 608~1073Ma LA-ICP-MS [98-99] 额尔古纳地块漠河杂岩原岩年龄 615~850Ma LA-ICP-MS [99] 兴安地块兴华渡口群原岩年龄 660~970Ma LA-ICP-MS [98] 兴凯地块虎头杂岩夕线石榴片麻岩原岩年龄 678~1373Ma LA-ICP-MS [103-104] 扎兰屯变质杂岩碎屑锆石 699~998Ma LA-ICP-MS [95] 中元古代—古元古代岩浆事件 大兴安岭东北部花岗岩 1.0~1.4Ga Hf模式年龄 [88] 大兴安岭北部兴华渡口群眼球状花岗片麻岩和条带 1741±30~1837±5Ma SHRIMP [105] 状片麻岩的正片麻岩 LA-ICP-MS 兴凯地块虎头群矽线石榴片麻岩 1300Ma LA-ICP-MS [104] 兴华渡口群变碎屑岩碎屑锆石 1.6~1.8Ga、2.5~2.6Ga SHRIMP [92] 兴安地块兴华渡口群碎屑锆石 1496±23~2791±18Ma LA-ICP-MS [98] 松辽盆地基底变质岩碎屑锆石 1823~2564Ma LA-ICP-MS [93-94] 松辽地块铁力杂岩碎屑锆石 1857~2442Ma LA-ICP-MS [100] 扎兰屯变质杂岩碎屑锆石 1213~3200Ma LA-ICP-MS [95]
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① 内蒙古区调队.罕乌拉幅（L-30-29）1：20万区域地质调查报告.1976.
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