Geoscience ›› 2019, Vol. 33 ›› Issue (01): 112-120.DOI: 10.19657/j.geoscience.1000-8527.2019.01.11
• Petrology • Previous Articles Next Articles
SONG Zhijie1(), LIU Wencan1, ZHANG Hongyuan1, LIU Changfeng1, LUO Kai1,2, WU Chen1
Received:
2017-12-01
Revised:
2018-10-30
Online:
2019-02-26
Published:
2019-02-28
CLC Number:
SONG Zhijie, LIU Wencan, ZHANG Hongyuan, LIU Changfeng, LUO Kai, WU Chen. Detrital Zircon Geochronology and Its Geological Significance of Upper Permian Sandstones in Yushigou Area of Western Qilian Mountains, China[J]. Geoscience, 2019, 33(01): 112-120.
测 点 号 | wB/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Pb | U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | Th/U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | 最佳 年龄 | 1σ | |||||
1 | 21 | 285 | 0.072 0 | 0.000 5 | 0.552 2 | 0.017 8 | 0.055 7 | 0.001 8 | 0.353 3 | 448 | 3 | 446 | 14 | 439 | 71 | 448 | 3 | ||||
2 | 28 | 361 | 0.070 6 | 0.000 5 | 0.547 5 | 0.015 0 | 0.056 2 | 0.001 5 | 0.649 8 | 440 | 3 | 443 | 12 | 461 | 61 | 440 | 3 | ||||
3 | 22 | 431 | 0.049 9 | 0.000 3 | 0.365 5 | 0.006 7 | 0.053 1 | 0.001 0 | 0.399 3 | 314 | 2 | 316 | 6 | 334 | 43 | 314 | 2 | ||||
4 | 8 | 24 | 0.325 1 | 0.002 2 | 4.998 7 | 0.038 6 | 0.111 5 | 0.001 0 | 0.056 3 | 1 815 | 12 | 1 819 | 14 | 1 824 | 16 | 1 824 | 16 | ||||
5 | 53 | 154 | 0.333 9 | 0.002 1 | 5.429 2 | 0.036 4 | 0.117 9 | 0.000 9 | 0.186 7 | 1 857 | 12 | 1 889 | 13 | 1 925 | 14 | 1 925 | 14 | ||||
6 | 231 | 707 | 0.337 4 | 0.002 2 | 5.375 8 | 0.039 8 | 0.115 5 | 0.001 0 | 0.013 5 | 1 874 | 12 | 1 881 | 14 | 1 888 | 15 | 1 888 | 15 | ||||
7 | 73 | 204 | 0.338 0 | 0.002 2 | 5.367 6 | 0.060 3 | 0.115 2 | 0.001 4 | 0.346 6 | 1 877 | 12 | 1 880 | 21 | 1 883 | 22 | 1 883 | 22 | ||||
8 | 52 | 159 | 0.309 8 | 0.001 9 | 4.529 8 | 0.043 0 | 0.106 0 | 0.001 1 | 0.368 6 | 1 740 | 11 | 1 736 | 16 | 1 732 | 19 | 1 732 | 19 | ||||
9 | 62 | 193 | 0.309 4 | 0.002 0 | 4.560 7 | 0.045 3 | 0.106 9 | 0.001 2 | 0.329 4 | 1 738 | 11 | 1 742 | 17 | 1 747 | 20 | 1 747 | 20 | ||||
10 | 34 | 90 | 0.377 8 | 0.002 4 | 6.612 4 | 0.055 2 | 0.126 9 | 0.001 2 | 0.054 8 | 2 066 | 13 | 2 061 | 17 | 2 056 | 17 | 2 056 | 17 | ||||
11 | 25 | 70 | 0.368 5 | 0.002 3 | 6.142 6 | 0.083 2 | 0.120 9 | 0.001 7 | 0.029 1 | 2 022 | 13 | 1 996 | 27 | 1 969 | 25 | 1 969 | 25 | ||||
12 | 17 | 42 | 0.341 1 | 0.002 3 | 5.492 2 | 0.040 0 | 0.116 8 | 0.001 0 | 1.010 2 | 1 892 | 13 | 1 899 | 14 | 1 908 | 15 | 1 908 | 15 | ||||
13 | 42 | 117 | 0.340 0 | 0.002 2 | 5.423 1 | 0.098 3 | 0.115 7 | 0.002 0 | 0.403 0 | 1 886 | 12 | 1 889 | 34 | 1 891 | 32 | 1 891 | 32 | ||||
14 | 17 | 49 | 0.304 5 | 0.002 2 | 4.429 2 | 0.035 6 | 0.105 5 | 0.001 0 | 0.629 9 | 1 714 | 12 | 1 718 | 14 | 1 723 | 17 | 1 723 | 17 | ||||
15 | 49 | 641 | 0.073 7 | 0.000 5 | 0.566 4 | 0.029 6 | 0.055 7 | 0.002 9 | 0.465 9 | 459 | 3 | 456 | 24 | 441 | 117 | 459 | 3 | ||||
16 | 11 | 135 | 0.073 6 | 0.000 5 | 0.561 6 | 0.111 3 | 0.055 3 | 0.010 8 | 0.593 3 | 458 | 3 | 453 | 90 | 425 | 436 | 458 | 3 | ||||
17 | 3 | 54 | 0.052 9 | 0.000 7 | 0.395 4 | 0.018 1 | 0.054 2 | 0.002 5 | 0.505 2 | 332 | 4 | 338 | 16 | 380 | 105 | 332 | 4 | ||||
18 | 6 | 86 | 0.068 6 | 0.000 5 | 0.513 7 | 0.004 1 | 0.054 3 | 0.000 5 | 0.316 9 | 428 | 3 | 421 | 3 | 385 | 20 | 428 | 3 | ||||
19 | 23 | 71 | 0.305 3 | 0.001 9 | 4.546 6 | 0.371 0 | 0.108 0 | 0.008 4 | 0.428 3 | 1 717 | 11 | 1 740 | 142 | 1 766 | 142 | 1 766 | 142 | ||||
20 | 7 | 114 | 0.049 9 | 0.000 4 | 0.359 8 | 0.002 4 | 0.052 3 | 0.000 4 | 1.140 7 | 314 | 3 | 312 | 2 | 297 | 18 | 314 | 3 | ||||
21 | 15 | 286 | 0.045 8 | 0.000 3 | 0.329 0 | 0.011 3 | 0.052 1 | 0.001 8 | 1.150 5 | 289 | 2 | 289 | 10 | 288 | 79 | 289 | 2 | ||||
22 | 18 | 236 | 0.071 2 | 0.000 5 | 0.548 4 | 0.005 5 | 0.055 9 | 0.000 5 | 0.637 2 | 443 | 3 | 444 | 4 | 448 | 22 | 443 | 3 | ||||
23 | 39 | 140 | 0.236 0 | 0.001 8 | 2.851 2 | 0.022 2 | 0.087 6 | 0.000 8 | 0.974 5 | 1 366 | 10 | 1 369 | 11 | 1 374 | 17 | 1 374 | 17 | ||||
24 | 37 | 138 | 0.241 3 | 0.001 5 | 2.970 1 | 0.020 2 | 0.089 3 | 0.000 7 | 0.732 8 | 1 393 | 9 | 1 400 | 10 | 1 410 | 16 | 1 410 | 16 | ||||
25 | 96 | 162 | 0.494 5 | 0.003 1 | 11.848 3 | 0.118 7 | 0.173 8 | 0.001 9 | 0.943 2 | 2 590 | 16 | 2 592 | 26 | 2 594 | 18 | 2 594 | 18 | ||||
26 | 44 | 647 | 0.071 4 | 0.000 5 | 0.551 0 | 0.005 2 | 0.056 0 | 0.000 6 | 0.179 1 | 444 | 3 | 446 | 4 | 452 | 23 | 444 | 3 | ||||
27 | 32 | 66 | 0.435 8 | 0.002 8 | 9.056 1 | 0.468 2 | 0.150 7 | 0.007 8 | 0.710 9 | 2 332 | 15 | 2 344 | 121 | 2 354 | 88 | 2 354 | 88 | ||||
28 | 5 | 70 | 0.071 6 | 0.000 5 | 0.551 3 | 0.005 4 | 0.055 9 | 0.000 6 | 0.443 4 | 446 | 3 | 446 | 4 | 447 | 23 | 446 | 3 | ||||
29 | 38 | 119 | 0.307 7 | 0.002 0 | 4.567 7 | 0.974 0 | 0.107 7 | 0.023 2 | 0.416 3 | 1 729 | 11 | 1 743 | 372 | 1 760 | 394 | 1 760 | 394 | ||||
30 | 5 | 77 | 0.068 9 | 0.001 0 | 0.526 3 | 0.016 7 | 0.055 4 | 0.001 8 | 0.589 0 | 429 | 6 | 429 | 14 | 429 | 71 | 429 | 6 | ||||
31 | 12 | 157 | 0.071 4 | 0.000 5 | 0.548 2 | 0.005 2 | 0.055 7 | 0.000 6 | 0.503 1 | 445 | 3 | 444 | 4 | 440 | 23 | 445 | 3 | ||||
32 | 24 | 48 | 0.416 0 | 0.002 7 | 8.181 3 | 6.329 2 | 0.142 6 | 0.080 7 | 1.006 7 | 2 242 | 15 | 2 251 | 1 742 | 2 260 | 976 | 2 260 | 976 | ||||
33 | 3 | 49 | 0.053 0 | 0.000 5 | 0.389 6 | 0.003 6 | 0.053 3 | 0.000 5 | 0.423 3 | 333 | 3 | 334 | 3 | 344 | 23 | 333 | 3 | ||||
34 | 31 | 82 | 0.338 0 | 0.002 1 | 5.415 1 | 0.044 0 | 0.116 2 | 0.000 9 | 0.655 4 | 1 877 | 12 | 1 887 | 15 | 1 899 | 14 | 1 899 | 14 | ||||
35 | 298 | 549 | 0.472 6 | 0.003 9 | 10.779 6 | 0.242 6 | 0.165 4 | 0.003 7 | 0.608 8 | 2 495 | 20 | 2 504 | 56 | 2 512 | 38 | 2 495 | 38 | ||||
36 | 13 | 168 | 0.073 6 | 0.000 5 | 0.576 3 | 0.004 0 | 0.056 8 | 0.000 5 | 0.646 8 | 458 | 3 | 462 | 3 | 483 | 18 | 458 | 3 | ||||
37 | 45 | 137 | 0.306 4 | 0.002 0 | 4.476 4 | 0.030 9 | 0.106 0 | 0.000 9 | 0.449 9 | 1 723 | 11 | 1 727 | 12 | 1 731 | 15 | 1 731 | 15 | ||||
38 | 76 | 148 | 0.453 0 | 0.002 9 | 9.879 1 | 0.157 9 | 0.158 2 | 0.002 6 | 0.591 6 | 2 409 | 15 | 2 424 | 39 | 2 436 | 28 | 2 436 | 28 | ||||
39 | 17 | 60 | 0.241 7 | 0.001 6 | 3.051 4 | 0.070 2 | 0.091 6 | 0.002 1 | 0.885 7 | 1 396 | 10 | 1 421 | 33 | 1 458 | 44 | 1 458 | 44 | ||||
40 | 13 | 229 | 0.050 8 | 0.000 3 | 0.379 2 | 0.004 4 | 0.054 1 | 0.000 6 | 0.652 0 | 320 | 2 | 326 | 4 | 375 | 24 | 320 | 2 | ||||
41 | 19 | 42 | 0.365 5 | 0.003 2 | 6.207 6 | 0.185 7 | 0.123 2 | 0.003 7 | 1.478 5 | 2 008 | 17 | 2 006 | 60 | 2 003 | 53 | 2 003 | 53 | ||||
42 | 5 | 13 | 0.337 7 | 0.002 8 | 5.348 2 | 0.150 9 | 0.114 9 | 0.003 2 | 0.751 6 | 1 875 | 15 | 1 877 | 53 | 1 878 | 50 | 1 878 | 50 | ||||
43 | 17 | 204 | 0.071 4 | 0.000 5 | 0.549 6 | 0.005 0 | 0.055 8 | 0.000 6 | 0.983 1 | 445 | 3 | 445 | 4 | 445 | 22 | 445 | 3 | ||||
测 点 号 | wB/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||||||
Pb | U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | Th/U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | 最佳 年龄 | 1σ | |||||
44 | 35 | 53 | 0.473 3 | 0.003 1 | 10.736 8 | 0.100 9 | 0.164 5 | 0.002 6 | 1.604 2 | 2 498 | 17 | 2 501 | 24 | 2 503 | 27 | 2 503 | 27 | ||||
45 | 100 | 283 | 0.329 2 | 0.003 5 | 5.164 8 | 0.028 5 | 0.113 8 | 0.001 6 | 0.398 3 | 1 834 | 19 | 1 847 | 10 | 1 861 | 26 | 1 861 | 26 | ||||
46 | 20 | 231 | 0.076 8 | 0.000 5 | 0.611 4 | 0.005 3 | 0.057 8 | 0.000 6 | 0.778 2 | 477 | 3 | 484 | 4 | 521 | 21 | 477 | 3 | ||||
47 | 28 | 81 | 0.308 0 | 0.001 9 | 4.551 9 | 0.722 2 | 0.107 2 | 0.011 0 | 0.630 3 | 1 731 | 11 | 1 740 | 276 | 1 752 | 188 | 1 752 | 188 | ||||
48 | 4 | 53 | 0.071 3 | 0.000 8 | 0.550 3 | 0.193 2 | 0.056 0 | 0.020 4 | 0.565 1 | 444 | 5 | 445 | 156 | 451 | 809 | 444 | 5 | ||||
49 | 4 | 73 | 0.046 3 | 0.000 6 | 0.332 8 | 0.008 4 | 0.052 2 | 0.011 2 | 1.005 7 | 292 | 4 | 292 | 7 | 293 | 492 | 292 | 4 | ||||
50 | 6 | 71 | 0.067 1 | 0.001 0 | 0.515 5 | 0.014 0 | 0.055 7 | 0.002 9 | 1.313 4 | 419 | 6 | 422 | 11 | 441 | 116 | 419 | 6 | ||||
51 | 19 | 52 | 0.300 7 | 0.007 1 | 4.337 2 | 0.153 7 | 0.104 6 | 0.006 5 | 0.867 9 | 1 695 | 40 | 1 700 | 60 | 1 708 | 115 | 1 708 | 115 | ||||
52 | 9 | 131 | 0.053 5 | 0.000 4 | 0.396 0 | 0.023 7 | 0.053 7 | 0.003 2 | 1.066 0 | 336 | 2 | 339 | 20 | 358 | 133 | 336 | 2 | ||||
53 | 9 | 107 | 0.070 6 | 0.000 6 | 0.556 3 | 0.006 3 | 0.057 1 | 0.003 4 | 0.949 8 | 440 | 4 | 449 | 5 | 496 | 131 | 440 | 4 | ||||
54 | 7 | 78 | 0.070 0 | 0.000 4 | 0.540 8 | 0.006 2 | 0.056 0 | 0.000 7 | 0.920 8 | 436 | 3 | 439 | 5 | 454 | 26 | 436 | 3 | ||||
55 | 20 | 28 | 0.418 4 | 0.002 8 | 8.199 9 | 0.118 5 | 0.142 1 | 0.009 9 | 2.279 0 | 2 253 | 15 | 2 253 | 33 | 2 253 | 120 | 2 253 | 120 | ||||
56 | 3 | 38 | 0.070 6 | 0.000 7 | 0.561 2 | 0.004 5 | 0.057 7 | 0.000 6 | 0.728 6 | 440 | 4 | 452 | 4 | 517 | 23 | 440 | 4 | ||||
57 | 52 | 148 | 0.314 7 | 0.002 2 | 4.682 9 | 0.151 3 | 0.107 9 | 0.001 4 | 0.481 3 | 1 764 | 12 | 1 764 | 57 | 1 765 | 24 | 1 765 | 24 | ||||
58 | 24 | 161 | 0.144 9 | 0.001 0 | 1.376 6 | 0.044 2 | 0.068 9 | 0.002 2 | 0.352 1 | 872 | 6 | 879 | 28 | 896 | 67 | 872 | 6 | ||||
59 | 26 | 312 | 0.073 7 | 0.000 5 | 0.570 5 | 0.005 3 | 0.056 1 | 0.000 6 | 0.531 8 | 458 | 3 | 458 | 4 | 458 | 23 | 458 | 3 | ||||
60 | 56 | 679 | 0.071 7 | 0.000 5 | 0.555 1 | 0.003 8 | 0.056 2 | 0.000 7 | 0.819 5 | 446 | 3 | 448 | 3 | 460 | 29 | 446 | 3 | ||||
61 | 63 | 95 | 0.453 8 | 0.006 2 | 9.807 6 | 0.106 1 | 0.156 7 | 0.003 9 | 1.634 7 | 2 412 | 33 | 2 417 | 26 | 2 421 | 42 | 2 421 | 42 | ||||
62 | 15 | 193 | 0.071 3 | 0.000 5 | 0.549 7 | 0.006 9 | 0.055 9 | 0.000 8 | 0.615 0 | 444 | 3 | 445 | 6 | 448 | 30 | 444 | 3 | ||||
63 | 45 | 281 | 0.157 7 | 0.001 0 | 1.531 4 | 0.089 4 | 0.070 4 | 0.000 9 | 0.267 8 | 944 | 6 | 943 | 55 | 940 | 27 | 944 | 6 | ||||
64 | 138 | 278 | 0.454 3 | 0.005 2 | 9.782 4 | 0.107 3 | 0.156 2 | 0.001 8 | 0.331 3 | 2 414 | 28 | 2 414 | 26 | 2 415 | 20 | 2 415 | 20 |
Table 1 LA-ICP-MS zircon U-Pb data of sandstones from the Hongquan Formation (D4404.TW1) in the Yushigou area
测 点 号 | wB/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Pb | U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | Th/U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | 最佳 年龄 | 1σ | |||||
1 | 21 | 285 | 0.072 0 | 0.000 5 | 0.552 2 | 0.017 8 | 0.055 7 | 0.001 8 | 0.353 3 | 448 | 3 | 446 | 14 | 439 | 71 | 448 | 3 | ||||
2 | 28 | 361 | 0.070 6 | 0.000 5 | 0.547 5 | 0.015 0 | 0.056 2 | 0.001 5 | 0.649 8 | 440 | 3 | 443 | 12 | 461 | 61 | 440 | 3 | ||||
3 | 22 | 431 | 0.049 9 | 0.000 3 | 0.365 5 | 0.006 7 | 0.053 1 | 0.001 0 | 0.399 3 | 314 | 2 | 316 | 6 | 334 | 43 | 314 | 2 | ||||
4 | 8 | 24 | 0.325 1 | 0.002 2 | 4.998 7 | 0.038 6 | 0.111 5 | 0.001 0 | 0.056 3 | 1 815 | 12 | 1 819 | 14 | 1 824 | 16 | 1 824 | 16 | ||||
5 | 53 | 154 | 0.333 9 | 0.002 1 | 5.429 2 | 0.036 4 | 0.117 9 | 0.000 9 | 0.186 7 | 1 857 | 12 | 1 889 | 13 | 1 925 | 14 | 1 925 | 14 | ||||
6 | 231 | 707 | 0.337 4 | 0.002 2 | 5.375 8 | 0.039 8 | 0.115 5 | 0.001 0 | 0.013 5 | 1 874 | 12 | 1 881 | 14 | 1 888 | 15 | 1 888 | 15 | ||||
7 | 73 | 204 | 0.338 0 | 0.002 2 | 5.367 6 | 0.060 3 | 0.115 2 | 0.001 4 | 0.346 6 | 1 877 | 12 | 1 880 | 21 | 1 883 | 22 | 1 883 | 22 | ||||
8 | 52 | 159 | 0.309 8 | 0.001 9 | 4.529 8 | 0.043 0 | 0.106 0 | 0.001 1 | 0.368 6 | 1 740 | 11 | 1 736 | 16 | 1 732 | 19 | 1 732 | 19 | ||||
9 | 62 | 193 | 0.309 4 | 0.002 0 | 4.560 7 | 0.045 3 | 0.106 9 | 0.001 2 | 0.329 4 | 1 738 | 11 | 1 742 | 17 | 1 747 | 20 | 1 747 | 20 | ||||
10 | 34 | 90 | 0.377 8 | 0.002 4 | 6.612 4 | 0.055 2 | 0.126 9 | 0.001 2 | 0.054 8 | 2 066 | 13 | 2 061 | 17 | 2 056 | 17 | 2 056 | 17 | ||||
11 | 25 | 70 | 0.368 5 | 0.002 3 | 6.142 6 | 0.083 2 | 0.120 9 | 0.001 7 | 0.029 1 | 2 022 | 13 | 1 996 | 27 | 1 969 | 25 | 1 969 | 25 | ||||
12 | 17 | 42 | 0.341 1 | 0.002 3 | 5.492 2 | 0.040 0 | 0.116 8 | 0.001 0 | 1.010 2 | 1 892 | 13 | 1 899 | 14 | 1 908 | 15 | 1 908 | 15 | ||||
13 | 42 | 117 | 0.340 0 | 0.002 2 | 5.423 1 | 0.098 3 | 0.115 7 | 0.002 0 | 0.403 0 | 1 886 | 12 | 1 889 | 34 | 1 891 | 32 | 1 891 | 32 | ||||
14 | 17 | 49 | 0.304 5 | 0.002 2 | 4.429 2 | 0.035 6 | 0.105 5 | 0.001 0 | 0.629 9 | 1 714 | 12 | 1 718 | 14 | 1 723 | 17 | 1 723 | 17 | ||||
15 | 49 | 641 | 0.073 7 | 0.000 5 | 0.566 4 | 0.029 6 | 0.055 7 | 0.002 9 | 0.465 9 | 459 | 3 | 456 | 24 | 441 | 117 | 459 | 3 | ||||
16 | 11 | 135 | 0.073 6 | 0.000 5 | 0.561 6 | 0.111 3 | 0.055 3 | 0.010 8 | 0.593 3 | 458 | 3 | 453 | 90 | 425 | 436 | 458 | 3 | ||||
17 | 3 | 54 | 0.052 9 | 0.000 7 | 0.395 4 | 0.018 1 | 0.054 2 | 0.002 5 | 0.505 2 | 332 | 4 | 338 | 16 | 380 | 105 | 332 | 4 | ||||
18 | 6 | 86 | 0.068 6 | 0.000 5 | 0.513 7 | 0.004 1 | 0.054 3 | 0.000 5 | 0.316 9 | 428 | 3 | 421 | 3 | 385 | 20 | 428 | 3 | ||||
19 | 23 | 71 | 0.305 3 | 0.001 9 | 4.546 6 | 0.371 0 | 0.108 0 | 0.008 4 | 0.428 3 | 1 717 | 11 | 1 740 | 142 | 1 766 | 142 | 1 766 | 142 | ||||
20 | 7 | 114 | 0.049 9 | 0.000 4 | 0.359 8 | 0.002 4 | 0.052 3 | 0.000 4 | 1.140 7 | 314 | 3 | 312 | 2 | 297 | 18 | 314 | 3 | ||||
21 | 15 | 286 | 0.045 8 | 0.000 3 | 0.329 0 | 0.011 3 | 0.052 1 | 0.001 8 | 1.150 5 | 289 | 2 | 289 | 10 | 288 | 79 | 289 | 2 | ||||
22 | 18 | 236 | 0.071 2 | 0.000 5 | 0.548 4 | 0.005 5 | 0.055 9 | 0.000 5 | 0.637 2 | 443 | 3 | 444 | 4 | 448 | 22 | 443 | 3 | ||||
23 | 39 | 140 | 0.236 0 | 0.001 8 | 2.851 2 | 0.022 2 | 0.087 6 | 0.000 8 | 0.974 5 | 1 366 | 10 | 1 369 | 11 | 1 374 | 17 | 1 374 | 17 | ||||
24 | 37 | 138 | 0.241 3 | 0.001 5 | 2.970 1 | 0.020 2 | 0.089 3 | 0.000 7 | 0.732 8 | 1 393 | 9 | 1 400 | 10 | 1 410 | 16 | 1 410 | 16 | ||||
25 | 96 | 162 | 0.494 5 | 0.003 1 | 11.848 3 | 0.118 7 | 0.173 8 | 0.001 9 | 0.943 2 | 2 590 | 16 | 2 592 | 26 | 2 594 | 18 | 2 594 | 18 | ||||
26 | 44 | 647 | 0.071 4 | 0.000 5 | 0.551 0 | 0.005 2 | 0.056 0 | 0.000 6 | 0.179 1 | 444 | 3 | 446 | 4 | 452 | 23 | 444 | 3 | ||||
27 | 32 | 66 | 0.435 8 | 0.002 8 | 9.056 1 | 0.468 2 | 0.150 7 | 0.007 8 | 0.710 9 | 2 332 | 15 | 2 344 | 121 | 2 354 | 88 | 2 354 | 88 | ||||
28 | 5 | 70 | 0.071 6 | 0.000 5 | 0.551 3 | 0.005 4 | 0.055 9 | 0.000 6 | 0.443 4 | 446 | 3 | 446 | 4 | 447 | 23 | 446 | 3 | ||||
29 | 38 | 119 | 0.307 7 | 0.002 0 | 4.567 7 | 0.974 0 | 0.107 7 | 0.023 2 | 0.416 3 | 1 729 | 11 | 1 743 | 372 | 1 760 | 394 | 1 760 | 394 | ||||
30 | 5 | 77 | 0.068 9 | 0.001 0 | 0.526 3 | 0.016 7 | 0.055 4 | 0.001 8 | 0.589 0 | 429 | 6 | 429 | 14 | 429 | 71 | 429 | 6 | ||||
31 | 12 | 157 | 0.071 4 | 0.000 5 | 0.548 2 | 0.005 2 | 0.055 7 | 0.000 6 | 0.503 1 | 445 | 3 | 444 | 4 | 440 | 23 | 445 | 3 | ||||
32 | 24 | 48 | 0.416 0 | 0.002 7 | 8.181 3 | 6.329 2 | 0.142 6 | 0.080 7 | 1.006 7 | 2 242 | 15 | 2 251 | 1 742 | 2 260 | 976 | 2 260 | 976 | ||||
33 | 3 | 49 | 0.053 0 | 0.000 5 | 0.389 6 | 0.003 6 | 0.053 3 | 0.000 5 | 0.423 3 | 333 | 3 | 334 | 3 | 344 | 23 | 333 | 3 | ||||
34 | 31 | 82 | 0.338 0 | 0.002 1 | 5.415 1 | 0.044 0 | 0.116 2 | 0.000 9 | 0.655 4 | 1 877 | 12 | 1 887 | 15 | 1 899 | 14 | 1 899 | 14 | ||||
35 | 298 | 549 | 0.472 6 | 0.003 9 | 10.779 6 | 0.242 6 | 0.165 4 | 0.003 7 | 0.608 8 | 2 495 | 20 | 2 504 | 56 | 2 512 | 38 | 2 495 | 38 | ||||
36 | 13 | 168 | 0.073 6 | 0.000 5 | 0.576 3 | 0.004 0 | 0.056 8 | 0.000 5 | 0.646 8 | 458 | 3 | 462 | 3 | 483 | 18 | 458 | 3 | ||||
37 | 45 | 137 | 0.306 4 | 0.002 0 | 4.476 4 | 0.030 9 | 0.106 0 | 0.000 9 | 0.449 9 | 1 723 | 11 | 1 727 | 12 | 1 731 | 15 | 1 731 | 15 | ||||
38 | 76 | 148 | 0.453 0 | 0.002 9 | 9.879 1 | 0.157 9 | 0.158 2 | 0.002 6 | 0.591 6 | 2 409 | 15 | 2 424 | 39 | 2 436 | 28 | 2 436 | 28 | ||||
39 | 17 | 60 | 0.241 7 | 0.001 6 | 3.051 4 | 0.070 2 | 0.091 6 | 0.002 1 | 0.885 7 | 1 396 | 10 | 1 421 | 33 | 1 458 | 44 | 1 458 | 44 | ||||
40 | 13 | 229 | 0.050 8 | 0.000 3 | 0.379 2 | 0.004 4 | 0.054 1 | 0.000 6 | 0.652 0 | 320 | 2 | 326 | 4 | 375 | 24 | 320 | 2 | ||||
41 | 19 | 42 | 0.365 5 | 0.003 2 | 6.207 6 | 0.185 7 | 0.123 2 | 0.003 7 | 1.478 5 | 2 008 | 17 | 2 006 | 60 | 2 003 | 53 | 2 003 | 53 | ||||
42 | 5 | 13 | 0.337 7 | 0.002 8 | 5.348 2 | 0.150 9 | 0.114 9 | 0.003 2 | 0.751 6 | 1 875 | 15 | 1 877 | 53 | 1 878 | 50 | 1 878 | 50 | ||||
43 | 17 | 204 | 0.071 4 | 0.000 5 | 0.549 6 | 0.005 0 | 0.055 8 | 0.000 6 | 0.983 1 | 445 | 3 | 445 | 4 | 445 | 22 | 445 | 3 | ||||
测 点 号 | wB/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||||||
Pb | U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | Th/U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | 最佳 年龄 | 1σ | |||||
44 | 35 | 53 | 0.473 3 | 0.003 1 | 10.736 8 | 0.100 9 | 0.164 5 | 0.002 6 | 1.604 2 | 2 498 | 17 | 2 501 | 24 | 2 503 | 27 | 2 503 | 27 | ||||
45 | 100 | 283 | 0.329 2 | 0.003 5 | 5.164 8 | 0.028 5 | 0.113 8 | 0.001 6 | 0.398 3 | 1 834 | 19 | 1 847 | 10 | 1 861 | 26 | 1 861 | 26 | ||||
46 | 20 | 231 | 0.076 8 | 0.000 5 | 0.611 4 | 0.005 3 | 0.057 8 | 0.000 6 | 0.778 2 | 477 | 3 | 484 | 4 | 521 | 21 | 477 | 3 | ||||
47 | 28 | 81 | 0.308 0 | 0.001 9 | 4.551 9 | 0.722 2 | 0.107 2 | 0.011 0 | 0.630 3 | 1 731 | 11 | 1 740 | 276 | 1 752 | 188 | 1 752 | 188 | ||||
48 | 4 | 53 | 0.071 3 | 0.000 8 | 0.550 3 | 0.193 2 | 0.056 0 | 0.020 4 | 0.565 1 | 444 | 5 | 445 | 156 | 451 | 809 | 444 | 5 | ||||
49 | 4 | 73 | 0.046 3 | 0.000 6 | 0.332 8 | 0.008 4 | 0.052 2 | 0.011 2 | 1.005 7 | 292 | 4 | 292 | 7 | 293 | 492 | 292 | 4 | ||||
50 | 6 | 71 | 0.067 1 | 0.001 0 | 0.515 5 | 0.014 0 | 0.055 7 | 0.002 9 | 1.313 4 | 419 | 6 | 422 | 11 | 441 | 116 | 419 | 6 | ||||
51 | 19 | 52 | 0.300 7 | 0.007 1 | 4.337 2 | 0.153 7 | 0.104 6 | 0.006 5 | 0.867 9 | 1 695 | 40 | 1 700 | 60 | 1 708 | 115 | 1 708 | 115 | ||||
52 | 9 | 131 | 0.053 5 | 0.000 4 | 0.396 0 | 0.023 7 | 0.053 7 | 0.003 2 | 1.066 0 | 336 | 2 | 339 | 20 | 358 | 133 | 336 | 2 | ||||
53 | 9 | 107 | 0.070 6 | 0.000 6 | 0.556 3 | 0.006 3 | 0.057 1 | 0.003 4 | 0.949 8 | 440 | 4 | 449 | 5 | 496 | 131 | 440 | 4 | ||||
54 | 7 | 78 | 0.070 0 | 0.000 4 | 0.540 8 | 0.006 2 | 0.056 0 | 0.000 7 | 0.920 8 | 436 | 3 | 439 | 5 | 454 | 26 | 436 | 3 | ||||
55 | 20 | 28 | 0.418 4 | 0.002 8 | 8.199 9 | 0.118 5 | 0.142 1 | 0.009 9 | 2.279 0 | 2 253 | 15 | 2 253 | 33 | 2 253 | 120 | 2 253 | 120 | ||||
56 | 3 | 38 | 0.070 6 | 0.000 7 | 0.561 2 | 0.004 5 | 0.057 7 | 0.000 6 | 0.728 6 | 440 | 4 | 452 | 4 | 517 | 23 | 440 | 4 | ||||
57 | 52 | 148 | 0.314 7 | 0.002 2 | 4.682 9 | 0.151 3 | 0.107 9 | 0.001 4 | 0.481 3 | 1 764 | 12 | 1 764 | 57 | 1 765 | 24 | 1 765 | 24 | ||||
58 | 24 | 161 | 0.144 9 | 0.001 0 | 1.376 6 | 0.044 2 | 0.068 9 | 0.002 2 | 0.352 1 | 872 | 6 | 879 | 28 | 896 | 67 | 872 | 6 | ||||
59 | 26 | 312 | 0.073 7 | 0.000 5 | 0.570 5 | 0.005 3 | 0.056 1 | 0.000 6 | 0.531 8 | 458 | 3 | 458 | 4 | 458 | 23 | 458 | 3 | ||||
60 | 56 | 679 | 0.071 7 | 0.000 5 | 0.555 1 | 0.003 8 | 0.056 2 | 0.000 7 | 0.819 5 | 446 | 3 | 448 | 3 | 460 | 29 | 446 | 3 | ||||
61 | 63 | 95 | 0.453 8 | 0.006 2 | 9.807 6 | 0.106 1 | 0.156 7 | 0.003 9 | 1.634 7 | 2 412 | 33 | 2 417 | 26 | 2 421 | 42 | 2 421 | 42 | ||||
62 | 15 | 193 | 0.071 3 | 0.000 5 | 0.549 7 | 0.006 9 | 0.055 9 | 0.000 8 | 0.615 0 | 444 | 3 | 445 | 6 | 448 | 30 | 444 | 3 | ||||
63 | 45 | 281 | 0.157 7 | 0.001 0 | 1.531 4 | 0.089 4 | 0.070 4 | 0.000 9 | 0.267 8 | 944 | 6 | 943 | 55 | 940 | 27 | 944 | 6 | ||||
64 | 138 | 278 | 0.454 3 | 0.005 2 | 9.782 4 | 0.107 3 | 0.156 2 | 0.001 8 | 0.331 3 | 2 414 | 28 | 2 414 | 26 | 2 415 | 20 | 2 415 | 20 |
[1] | 徐亚军, 杜远生, 杨江海. 沉积物物源分析研究进展[J]. 地质科技情报, 2007,26(3):26-32. |
[2] |
BHATIA M R. Plate tectonics and geochemical composition of sandstones[J]. The Journal of Geology, 1983,91(6):611-627.
DOI URL |
[3] |
WELTJE G J, EYNATTEN H V. Quantitative provenance analysis of sediments: Review and outlook[J]. Sedimentary Geology, 2004,171(1/4):1-11.
DOI URL |
[4] | 王成善, 李祥辉. 沉积盆地分析原理与方法[M]. 北京: 高等教育出版社, 2003: 86-111. |
[5] |
ANDERSON T. Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation[J]. Chemical Geology, 2005,216:249-270.
DOI URL |
[6] |
GEHRELS G E, DICKINSON W R, ROSS G M, et al. Detrital zircon reference for Cambrian to Triassic miogeoclinal strata of western North America[J]. Geology, 1995,23(9):831-834.
DOI URL |
[7] |
CARTER A, MOSS S J. Combined detrital zircon fission-track and U-Pb dating: A new approach to understanding hinter-land evolution[J]. Geology, 1999,27(3):235-238.
DOI URL |
[8] |
WEISLOGEL A L, GRAHAM S A, CHANG E Z, et al. Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks[J]. Geology, 2006,34(2):97-100.
DOI URL |
[9] | 冯益民, 何世平. 祁连山大地构造与造山作用[M]. 北京: 地质出版社, 1996: 12-101. |
[10] | 左国朝, 吴汉泉. 北祁连中段早古生代双向俯冲—碰撞造山模式剖析[J]. 地球科学进展, 1997,12(4):315-323. |
[11] | 夏林圻, 夏祖春, 徐学义. 北祁连洋壳—洋脊和弧后盆地火山作用[J]. 地质学报, 1998,72(4):301-312. |
[12] |
XIA L Q, XIA Z C, XU X Y. Magma genesis in the Ordovician back-arc basins of the northern Qilian Mountain, China[J]. Geological Society of America Bulletin, 2003,115(12):1510-1522.
DOI URL |
[13] | 张旗, 王焰, 钱青. 北祁连早古生代洋盆是裂陷槽还是大洋盆: 与葛肖虹讨论[J]. 地质科学, 2000,35(1):121-128. |
[14] | 李三忠, 李涛, 赵淑娟, 等. 东亚原特提斯洋(Ⅳ): 北界西段早古生代构造变形[J]. 岩石学报, 2017,33(6):1615-1632. |
[15] |
XIAO W J, WINDLEY B F, YONG Y, et al. Early Paleozoic to Devonian multiple-accretionary model for the Qilian Shan, NW China[J]. Journal of Asian Earth Sciences, 2009,35(3/4) : 323-333.
DOI URL |
[16] | 潘桂棠, 王立全, 张万平, 等. 青藏高原及邻区大地构造图及说明书(1∶1 500 000)[M]. 北京: 地质出版社, 2013: 37-38. |
[17] |
SONG S G, NIU Y L, SU L, et al. Tectonics of the North Qilian orogen, NW China[J]. Gondwana Research, 2013,23:1378-1401.
DOI URL |
[18] | 戚学祥, 张建新, 李海兵, 等. 北祁连南缘右行韧性走滑剪切带的同位素年代学及其地质意义[J]. 地学前缘, 2004,11(4):469-479. |
[19] | 李怀坤, 耿建珍, 郝爽, 等. 用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J]. 矿物学报, 2009,29(S1):600-601. |
[20] | ANDERSON T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002,92(1/2):59-79. |
[21] | 杨雨, 范国琳, 姚国金, 等. 甘肃省岩石地层[M]. 武汉: 中国地质大学出版社, 1997: 128-177. |
[22] | 孙崇仁, 陈国隆, 李璋荣, 等. 青海省岩石地层[M]. 武汉: 中国地质大学出版社, 1997: 112-141. |
[23] | 刘永江, FRANZ N, 李伟民, 等. 柴北缘—南祁连地区构造热事件[J]. 吉林大学学报(地球科学版), 2012,42(5):1317-1329. |
[24] | 吴才来, 徐学义, 高前明, 等. 北祁连早古生代花岗质岩浆作用及构造演化[J]. 岩石学报, 2010,26(4):1027-1044. |
[25] | 黄增保, 郑建平, 李葆华, 等. 中祁连西段野马山岩基年代学、地球化学特征及地质意义[J]. 中国地质, 2015,42(2):406-420. |
[26] | 黄增保, 郑建平, 李葆华, 等. 中祁连西段晚寒武世埃达克岩的发现及地质意义[J]. 岩石矿物学杂志, 2014,33(6):1008-1018. |
[27] |
侯荣娜, 王淑华, 张翔, 等. 中祁连西段花岗岩类的地球化学特征及构造意义[J]. 地球科学进展, 2015,30(9):1034-1049.
DOI URL |
[28] | 齐瑞荣. 中祁连西段巴嘎德尔基岩体LA-ICP-MS锆石U-Pb年龄及地质意义[J]. 沉积与特提斯地质, 2012,32(4):86-93. |
[29] | 贾群子, 杨忠堂, 肖朝阳, 等. 祁连山铜金钨铅锌矿床成矿规律和成矿预测[M]. 北京: 地质出版社, 2007: 1-313. |
[30] | 钱青, 张旗, 孙晓萌. 北祁连老虎山玄武岩和硅岩的地球化学特征及形成环境[J]. 地质科学, 2001,36(4):444-453. |
[31] | 苏建平, 胡能高, 张海峰, 等. 中祁连西段黑沟梁子花岗岩的锆石U-Pb同位素年龄及成因[J]. 现代地质, 2004,18(1):70-74. |
[32] | 陈隽璐, 徐学义, 曾佐勋, 等. 中祁连东段什川杂岩基的岩石化学特征及年代学研究[J]. 岩石学报, 2008,24(4):841-854. |
[33] | 雍拥, 肖文交, 袁超, 等. 中祁连东段古生代花岗岩的年代学、地球化学特征及其大地构造意义[J]. 岩石学报, 2008,24(4):855-866. |
[34] | 陈隽璐, 李好斌, 王洪亮, 等. 秦祁结合部位王家岔石英闪长岩体锆石LA-ICP-MS定年及地质意义[J]. 吉林大学学报(地球科学版), 2007,37(3):423-431. |
[35] | 秦海鹏, 吴才来, 王次松, 等. 祁连东部西格拉高Sr/Y型花岗岩LA-ICP-MS锆石U-Pb定年及其地球化学特征[J]. 岩石学报, 2014,30(12):3759-3771. |
[36] | 何世平, 王洪亮, 陈隽璐, 等. 中祁连马衔山岩群内基性岩墙群锆石LA-ICP-MS U-Pb年代学及其构造意义[J]. 地球科学——中国地质大学学报, 2008,33(1):35-45. |
[37] |
LI J F, ZHANG Z C, TANG W H, et al. Provenance of Oligocene-Miocene sediments in the Subei area, eastern Altyn Tagh fault and its geological implications: Evidence from detrital zircons LA-ICP-MS U-Pb chronology[J]. Journal of Asian Earth Sciences, 2014,87:130-140.
DOI URL |
[38] | 徐亚军, 杜远生, 杨江海. 北祁连造山带晚奥陶世—泥盆纪构造演化:碎屑锆石年代学证据[J]. 地球科学——中国地质大学学报, 2013,38(5):934-946. |
[39] |
XU Y, DU Y, CAWOOD P A, et al. Provenance record of a foreland basin: Detrital zircon U-Pb ages from Devonian strata in the North Qilian Orogenic Belt, China[J]. Tectonophysics, 2010,495(3/4):337-347.
DOI URL |
[40] | 陈岳龙, 周建, 皮桥辉, 等. 青海共和—花石峡三叠纪碎屑沉积岩的地球化学特征与锆石U-Pb年龄及地质意义[J]. 地学前缘, 2009,16(2):161-174. |
[41] | 郭亮, 张宏飞, 徐旺春, 等. 黄河源头区碎屑锆石U-Pb年龄及其地质意义[J]. 自然科学进展, 2008,18(12):1398-1408. |
[42] | 董国安, 杨怀仁, 杨宏仪, 等. 祁连地块前寒武纪基底锆石SHRIMP U-Pb年代学及其地质意义[J]. 科学通报, 2007,52(13):1572-1585. |
[43] | 翟明国, 胡波, 彭澎, 等. 华北中—新元古代的岩浆作用与多期裂谷事件[J]. 地学前缘, 2014,21(1):100-119. |
[44] |
SONG S G, SU L, LI X H, et al. Grenville-age orogenesis in the Qaidam-Qilian block: The link between South China and Tarim[J]. Precambrian Research, 2012,220:9-22.
DOI URL |
[45] | 郭进京, 赵凤清, 李怀坤. 中祁连东段晋宁期碰撞型花岗岩及其地质意义[J]. 地球学报, 1999,20(1):10-15. |
[46] | 万渝生, 许志琴, 杨经绥, 等. 祁连造山带及邻区前寒武纪深变质基底的时代和组成[J]. 地球学报, 2003,24(4):319-324. |
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