Earth Science Frontiers ›› 2024, Vol. 31 ›› Issue (3): 20-39.DOI: 10.13745/j.esf.sf.2023.6.18
Previous Articles Next Articles
LI Guangjie1(), CHEN Yongqing1,*(
), SHANG Zhi1,2, LIU Shibo1
Received:
2022-10-04
Revised:
2023-07-03
Online:
2024-05-25
Published:
2024-05-25
CLC Number:
LI Guangjie, CHEN Yongqing, SHANG Zhi, LIU Shibo. Geochemical characteristics and petrogenesis of the Neoproterozoic Eshan highly fractionated I-type granites, western Yangtze block[J]. Earth Science Frontiers, 2024, 31(3): 20-39.
Fig.1 Distribution of Neoproterozoic magmatic rocks in the South China block(a), distribution of Neoproterozoic magmatic rocks in the middle of Yunnan(b) and simplified geological map(c) of Eshan area. a, b modified after [32],published data from [32⇓⇓⇓⇓-37]. c modified after [38-39], published data from [11,39].
编号 | 含量/10-6 | 232Th/238U | 同位素比值及误差 | 年龄及误差/Ma | |||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
232Th | 238U | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||||||||||||||
肉红色中粗粒花岗岩 | |||||||||||||||||||||||||||
1 | 286.33 | 360.09 | 0.8 | 0.070 6 | 0.004 | 1.05 | 0.076 9 | 0.108 | 0.005 | 944 | 79 | 729 | 38 | 661 | 29 | ||||||||||||
2 | 333.78 | 435.72 | 0.77 | 0.067 4 | 0.003 8 | 1.117 5 | 0.080 2 | 0.120 3 | 0.005 3 | 849 | 80 | 762 | 38 | 732 | 30 | ||||||||||||
3 | 211.69 | 229.87 | 0.92 | 0.063 | 0.004 | 1.231 1 | 0.095 4 | 0.141 8 | 0.006 3 | 707 | 92 | 815 | 43 | 855 | 36 | ||||||||||||
4 | 540.85 | 680.67 | 0.79 | 0.089 9 | 0.005 2 | 1.003 9 | 0.073 | 0.081 | 0.003 6 | 1 424 | 74 | 706 | 37 | 502 | 21 | ||||||||||||
5 | 120.65 | 128.89 | 0.94 | 0.078 9 | 0.005 3 | 1.480 2 | 0.120 2 | 0.136 | 0.006 2 | 1 170 | 91 | 922 | 49 | 822 | 35 | ||||||||||||
6 | 429.91 | 521.79 | 0.82 | 0.068 | 0.003 8 | 0.918 | 0.065 4 | 0.097 9 | 0.004 4 | 869 | 78 | 661 | 35 | 602 | 26 | ||||||||||||
7 | 196.82 | 296.7 | 0.66 | 0.071 1 | 0.004 3 | 1.088 8 | 0.083 | 0.111 1 | 0.005 2 | 959 | 83 | 748 | 40 | 679 | 30 | ||||||||||||
8 | 382.82 | 512.32 | 0.75 | 0.081 8 | 0.004 7 | 1.310 8 | 0.094 9 | 0.116 3 | 0.005 1 | 1 240 | 76 | 850 | 42 | 709 | 30 | ||||||||||||
9 | 452.31 | 548.04 | 0.83 | 0.072 3 | 0.004 1 | 0.948 9 | 0.068 8 | 0.095 2 | 0.004 2 | 995 | 79 | 678 | 36 | 586 | 25 | ||||||||||||
10 | 348.47 | 319.68 | 1.09 | 0.074 9 | 0.004 5 | 1.091 7 | 0.083 3 | 0.105 7 | 0.004 9 | 1 065 | 83 | 749 | 40 | 648 | 29 | ||||||||||||
11 | 940.53 | 647.6 | 1.45 | 0.076 7 | 0.004 5 | 1.059 1 | 0.079 1 | 0.100 1 | 0.004 6 | 1 114 | 80 | 733 | 39 | 615 | 27 | ||||||||||||
12 | 963.95 | 1 155.81 | 0.83 | 0.094 9 | 0.005 2 | 0.751 9 | 0.053 7 | 0.057 5 | 0.002 6 | 1 526 | 70 | 569 | 31 | 360 | 16 | ||||||||||||
13 | 174.06 | 240.04 | 0.73 | 0.070 4 | 0.004 3 | 1.303 | 0.099 2 | 0.134 2 | 0.006 | 940 | 86 | 847 | 44 | 812 | 34 | ||||||||||||
14 | 316.9 | 479.63 | 0.66 | 0.150 3 | 0.009 5 | 1.657 3 | 0.128 5 | 0.08 | 0.003 6 | 2 350 | 73 | 992 | 49 | 496 | 22 | ||||||||||||
15 | 213.72 | 368.19 | 0.58 | 0.081 4 | 0.004 6 | 1.135 4 | 0.083 1 | 0.101 2 | 0.004 7 | 1 230 | 75 | 770 | 40 | 622 | 27 | ||||||||||||
16 | 160.67 | 198.38 | 0.81 | 0.066 7 | 0.004 1 | 1.230 8 | 0.093 2 | 0.133 9 | 0.005 9 | 827 | 87 | 815 | 42 | 810 | 34 | ||||||||||||
17 | 562.94 | 376.06 | 1.5 | 0.067 | 0.004 1 | 0.937 4 | 0.071 6 | 0.101 4 | 0.004 7 | 838 | 86 | 672 | 38 | 623 | 27 | ||||||||||||
18 | 374 | 395.9 | 0.94 | 0.066 4 | 0.004 5 | 1.015 8 | 0.083 2 | 0.111 | 0.005 1 | 818 | 97 | 712 | 42 | 679 | 30 | ||||||||||||
19 | 267.99 | 225.54 | 1.19 | 0.099 9 | 0.007 2 | 1.699 1 | 0.144 7 | 0.123 3 | 0.005 7 | 1 622 | 92 | 1 008 | 54 | 750 | 33 | ||||||||||||
20 | 342.02 | 632.93 | 0.54 | 0.097 6 | 0.005 5 | 1.172 9 | 0.084 1 | 0.087 2 | 0.003 9 | 1 578 | 71 | 788 | 39 | 539 | 23 | ||||||||||||
21 | 302.72 | 473.44 | 0.64 | 0.147 5 | 0.012 | 1.958 7 | 0.187 6 | 0.096 3 | 0.004 9 | 2 317 | 96 | 1 101 | 64 | 593 | 29 | ||||||||||||
22 | 257.13 | 436.67 | 0.59 | 0.102 9 | 0.007 | 1.138 8 | 0.097 4 | 0.080 3 | 0.004 2 | 1 677 | 85 | 772 | 46 | 498 | 25 | ||||||||||||
23 | 289.32 | 416.76 | 0.69 | 0.067 2 | 0.003 9 | 1.160 9 | 0.084 6 | 0.125 4 | 0.005 6 | 843 | 81 | 782 | 40 | 761 | 32 | ||||||||||||
24 | 415.65 | 398.12 | 1.04 | 0.065 | 0.003 6 | 1.053 9 | 0.074 2 | 0.117 6 | 0.005 2 | 775 | 78 | 731 | 37 | 717 | 30 | ||||||||||||
25 | 989.16 | 1 916.99 | 0.52 | 0.046 1 | 0.005 6 | 0.130 5 | 0.015 1 | 0.020 6 | 0.000 8 | 239 | 125 | 14 | 131 | 5 | |||||||||||||
26 | 253.03 | 198.89 | 1.27 | 0.081 2 | 0.005 | 1.333 | 0.102 1 | 0.119 1 | 0.005 4 | 1 227 | 82 | 860 | 44 | 725 | 31 | ||||||||||||
27 | 455.38 | 597.31 | 0.76 | 0.061 3 | 0.004 6 | 0.970 2 | 0.085 8 | 0.114 9 | 0.005 3 | 649 | 112 | 689 | 44 | 701 | 31 | ||||||||||||
28 | 192.32 | 185.44 | 1.04 | 0.064 5 | 0.004 4 | 1.326 9 | 0.108 9 | 0.149 3 | 0.006 8 | 757 | 99 | 858 | 48 | 897 | 38 | ||||||||||||
29 | 294.05 | 367.14 | 0.8 | 0.065 5 | 0.003 8 | 1.060 1 | 0.076 8 | 0.117 3 | 0.005 2 | 791 | 81 | 734 | 38 | 715 | 30 | ||||||||||||
30 | 230.14 | 200.87 | 1.15 | 0.077 7 | 0.005 5 | 1.455 2 | 0.123 4 | 0.135 8 | 0.006 3 | 1 140 | 97 | 912 | 51 | 821 | 36 | ||||||||||||
31 | 260.66 | 723.58 | 0.36 | 0.074 8 | 0.004 3 | 0.925 8 | 0.067 5 | 0.089 8 | 0.004 | 1 062 | 78 | 665 | 36 | 554 | 24 | ||||||||||||
32 | 2 306.86 | 1 890.61 | 1.22 | 0.106 | 0.006 | 0.588 4 | 0.042 4 | 0.040 3 | 0.001 8 | 1 731 | 70 | 470 | 27 | 255 | 11 | ||||||||||||
灰白色中粗粒花岗岩 | |||||||||||||||||||||||||||
1 | 149.671 07 | 156.982 43 | 0.953 425 6 | 0.077 07 | 0.005 9 | 1.177 2 | 0.100 21 | 0.110 78 | 0.004 13 | 1 123 | 111 | 790 | 47 | 677 | 24 | ||||||||||||
2 | 634.060 18 | 483.761 95 | 1.310 686 3 | 0.086 76 | 0.005 8 | 0.990 53 | 0.073 62 | 0.082 8 | 0.002 7 | 1 355 | 93 | 699 | 38 | 513 | 16 | ||||||||||||
3 | 306.696 74 | 304.856 56 | 1.006 036 2 | 0.110 17 | 0.007 26 | 1.592 37 | 0.116 52 | 0.104 83 | 0.003 34 | 1 802 | 87 | 967 | 46 | 643 | 20 | ||||||||||||
4 | 168.948 09 | 144.843 89 | 1.166 415 | 0.065 07 | 0.004 8 | 1.196 72 | 0.097 19 | 0.133 38 | 0.004 51 | 777 | 114 | 799 | 45 | 807 | 26 | ||||||||||||
5 | 247.152 57 | 376.989 63 | 0.655 595 1 | 0.070 87 | 0.004 52 | 1.183 07 | 0.084 32 | 0.121 07 | 0.003 85 | 954 | 94 | 793 | 39 | 737 | 22 | ||||||||||||
6 | 2 144.279 7 | 1 388.478 5 | 1.544 337 7 | 0.046 05 | 0.004 | 0.249 33 | 0.020 82 | 0.039 27 | 0.000 93 | 191 | 226 | 17 | 248 | 6 | |||||||||||||
7 | 351.505 29 | 442.921 24 | 0.793 606 8 | 0.078 01 | 0.005 15 | 1.176 19 | 0.087 17 | 0.109 35 | 0.003 68 | 1 147 | 94 | 790 | 41 | 669 | 21 | ||||||||||||
8 | 354.322 57 | 492.087 41 | 0.720 039 9 | 0.090 68 | 0.005 99 | 0.910 6 | 0.067 39 | 0.072 83 | 0.002 43 | 1 440 | 90 | 657 | 36 | 453 | 15 | ||||||||||||
9 | 588.123 41 | 1 102.442 1 | 0.533 473 3 | 0.118 68 | 0.007 99 | 0.976 23 | 0.073 56 | 0.059 66 | 0.002 02 | 1 936 | 87 | 692 | 38 | 374 | 12 | ||||||||||||
10 | 888.199 24 | 1 450.600 9 | 0.612 297 5 | 0.140 29 | 0.009 96 | 1.021 92 | 0.080 93 | 0.052 83 | 0.001 85 | 2 231 | 89 | 715 | 41 | 332 | 11 | ||||||||||||
11 | 381.355 69 | 329.541 85 | 1.157 229 9 | 0.080 76 | 0.005 54 | 1.342 15 | 0.101 59 | 0.120 53 | 0.003 85 | 1 216 | 99 | 864 | 44 | 734 | 22 | ||||||||||||
12 | 684.989 16 | 904.253 14 | 0.757 519 3 | 0.098 39 | 0.006 63 | 0.852 84 | 0.063 56 | 0.062 87 | 0.002 | 1 594 | 92 | 626 | 35 | 393 | 12 | ||||||||||||
13 | 513.82 | 557.321 59 | 0.921 945 3 | 0.113 99 | 0.006 94 | 1.523 02 | 0.104 45 | 0.096 9 | 0.003 07 | 1 864 | 78 | 940 | 42 | 596 | 18 | ||||||||||||
14 | 327.226 65 | 223.377 34 | 1.464 905 3 | 0.074 58 | 0.004 96 | 1.067 | 0.080 09 | 0.103 76 | 0.003 6 | 1 057 | 96 | 737 | 39 | 636 | 21 | ||||||||||||
15 | 273.815 28 | 567.772 16 | 0.482 262 6 | 0.101 67 | 0.006 49 | 1.231 27 | 0.088 32 | 0.087 84 | 0.002 87 | 1 655 | 85 | 815 | 40 | 543 | 17 | ||||||||||||
16 | 1 378.725 3 | 1 453.815 8 | 0.948 349 3 | 0.117 6 | 0.008 99 | 1.015 11 | 0.087 21 | 0.062 6 | 0.002 46 | 1 920 | 98 | 711 | 44 | 391 | 15 | ||||||||||||
17 | 154.337 38 | 192.261 42 | 0.802 747 5 | 0.081 87 | 0.006 78 | 1.418 34 | 0.127 18 | 0.125 65 | 0.004 34 | 1 242 | 122 | 897 | 53 | 763 | 25 | ||||||||||||
18 | 926.376 14 | 1 015.220 9 | 0.912 487 3 | 0.090 45 | 0.005 68 | 0.773 33 | 0.054 46 | 0.062 01 | 0.001 98 | 1 435 | 86 | 582 | 31 | 388 | 12 | ||||||||||||
19 | 371.491 7 | 601.158 91 | 0.617 959 2 | 0.084 98 | 0.006 67 | 1.378 95 | 0.122 22 | 0.117 68 | 0.004 85 | 1 315 | 109 | 880 | 52 | 717 | 28 | ||||||||||||
20 | 648.983 33 | 725.294 6 | 0.894 785 8 | 0.096 | 0.006 66 | 1.075 78 | 0.081 87 | 0.081 27 | 0.002 54 | 1 548 | 96 | 742 | 40 | 504 | 15 | ||||||||||||
21 | 577.454 01 | 500.641 43 | 1.153 428 3 | 0.111 14 | 0.007 18 | 1.431 01 | 0.103 16 | 0.093 39 | 0.002 98 | 1 818 | 85 | 902 | 43 | 576 | 18 | ||||||||||||
22 | 1 959.226 1 | 1 266.946 1 | 1.546 416 3 | 0.127 02 | 0.008 22 | 1.004 73 | 0.075 02 | 0.057 37 | 0.002 14 | 2 057 | 80 | 706 | 38 | 360 | 13 | ||||||||||||
23 | 997.528 59 | 1 169.791 3 | 0.852 740 6 | 0.104 31 | 0.006 23 | 0.933 56 | 0.063 59 | 0.064 91 | 0.002 12 | 1 702 | 78 | 670 | 33 | 405 | 13 | ||||||||||||
24 | 345.202 45 | 623.503 82 | 0.553 649 3 | 0.093 71 | 0.006 06 | 0.956 16 | 0.068 54 | 0.074 | 0.002 3 | 1 502 | 89 | 681 | 36 | 460 | 14 | ||||||||||||
25 | 825.054 66 | 1 672.045 1 | 0.493 440 4 | 0.089 28 | 0.005 39 | 0.547 17 | 0.037 41 | 0.044 45 | 0.001 43 | 1 410 | 82 | 443 | 25 | 280 | 9 | ||||||||||||
26 | 256.908 02 | 280.222 97 | 0.916 798 6 | 0.074 67 | 0.005 22 | 1.265 81 | 0.097 93 | 0.122 96 | 0.004 08 | 1 060 | 103 | 831 | 44 | 748 | 23 | ||||||||||||
27 | 240.136 77 | 314.163 64 | 0.764 368 4 | 0.075 47 | 0.004 81 | 1.217 98 | 0.086 52 | 0.117 04 | 0.003 67 | 1 081 | 92 | 809 | 40 | 714 | 21 | ||||||||||||
28 | 1 864.141 2 | 1 882.394 | 0.990 303 4 | 0.152 8 | 0.008 89 | 1.105 82 | 0.073 56 | 0.052 49 | 0.001 69 | 2 377 | 70 | 756 | 35 | 330 | 10 | ||||||||||||
29 | 1 019.152 1 | 1 778.956 2 | 0.572 893 3 | 0.187 9 | 0.011 55 | 0.905 2 | 0.064 31 | 0.034 94 | 0.001 25 | 2 724 | 71 | 655 | 34 | 221 | 8 | ||||||||||||
30 | 262.946 42 | 365.560 99 | 0.719 295 6 | 0.083 47 | 0.005 58 | 1.481 89 | 0.110 29 | 0.128 76 | 0.004 2 | 1 280 | 94 | 923 | 45 | 781 | 24 | ||||||||||||
31 | 1 695.790 1 | 1 210.949 4 | 1.400 380 7 | 0.046 05 | 0.003 05 | 0.199 36 | 0.012 08 | 0.031 4 | 0.000 85 | 146 | 185 | 10 | 199 | 5 | |||||||||||||
32 | 424.562 97 | 514.095 72 | 0.825 844 2 | 0.073 18 | 0.004 55 | 0.948 37 | 0.068 67 | 0.093 99 | 0.003 49 | 1 019 | 88 | 677 | 36 | 579 | 21 |
Table 1 Results of LA-MC-ICPMS zircon U-Pb dating
编号 | 含量/10-6 | 232Th/238U | 同位素比值及误差 | 年龄及误差/Ma | |||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
232Th | 238U | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||||||||||||||
肉红色中粗粒花岗岩 | |||||||||||||||||||||||||||
1 | 286.33 | 360.09 | 0.8 | 0.070 6 | 0.004 | 1.05 | 0.076 9 | 0.108 | 0.005 | 944 | 79 | 729 | 38 | 661 | 29 | ||||||||||||
2 | 333.78 | 435.72 | 0.77 | 0.067 4 | 0.003 8 | 1.117 5 | 0.080 2 | 0.120 3 | 0.005 3 | 849 | 80 | 762 | 38 | 732 | 30 | ||||||||||||
3 | 211.69 | 229.87 | 0.92 | 0.063 | 0.004 | 1.231 1 | 0.095 4 | 0.141 8 | 0.006 3 | 707 | 92 | 815 | 43 | 855 | 36 | ||||||||||||
4 | 540.85 | 680.67 | 0.79 | 0.089 9 | 0.005 2 | 1.003 9 | 0.073 | 0.081 | 0.003 6 | 1 424 | 74 | 706 | 37 | 502 | 21 | ||||||||||||
5 | 120.65 | 128.89 | 0.94 | 0.078 9 | 0.005 3 | 1.480 2 | 0.120 2 | 0.136 | 0.006 2 | 1 170 | 91 | 922 | 49 | 822 | 35 | ||||||||||||
6 | 429.91 | 521.79 | 0.82 | 0.068 | 0.003 8 | 0.918 | 0.065 4 | 0.097 9 | 0.004 4 | 869 | 78 | 661 | 35 | 602 | 26 | ||||||||||||
7 | 196.82 | 296.7 | 0.66 | 0.071 1 | 0.004 3 | 1.088 8 | 0.083 | 0.111 1 | 0.005 2 | 959 | 83 | 748 | 40 | 679 | 30 | ||||||||||||
8 | 382.82 | 512.32 | 0.75 | 0.081 8 | 0.004 7 | 1.310 8 | 0.094 9 | 0.116 3 | 0.005 1 | 1 240 | 76 | 850 | 42 | 709 | 30 | ||||||||||||
9 | 452.31 | 548.04 | 0.83 | 0.072 3 | 0.004 1 | 0.948 9 | 0.068 8 | 0.095 2 | 0.004 2 | 995 | 79 | 678 | 36 | 586 | 25 | ||||||||||||
10 | 348.47 | 319.68 | 1.09 | 0.074 9 | 0.004 5 | 1.091 7 | 0.083 3 | 0.105 7 | 0.004 9 | 1 065 | 83 | 749 | 40 | 648 | 29 | ||||||||||||
11 | 940.53 | 647.6 | 1.45 | 0.076 7 | 0.004 5 | 1.059 1 | 0.079 1 | 0.100 1 | 0.004 6 | 1 114 | 80 | 733 | 39 | 615 | 27 | ||||||||||||
12 | 963.95 | 1 155.81 | 0.83 | 0.094 9 | 0.005 2 | 0.751 9 | 0.053 7 | 0.057 5 | 0.002 6 | 1 526 | 70 | 569 | 31 | 360 | 16 | ||||||||||||
13 | 174.06 | 240.04 | 0.73 | 0.070 4 | 0.004 3 | 1.303 | 0.099 2 | 0.134 2 | 0.006 | 940 | 86 | 847 | 44 | 812 | 34 | ||||||||||||
14 | 316.9 | 479.63 | 0.66 | 0.150 3 | 0.009 5 | 1.657 3 | 0.128 5 | 0.08 | 0.003 6 | 2 350 | 73 | 992 | 49 | 496 | 22 | ||||||||||||
15 | 213.72 | 368.19 | 0.58 | 0.081 4 | 0.004 6 | 1.135 4 | 0.083 1 | 0.101 2 | 0.004 7 | 1 230 | 75 | 770 | 40 | 622 | 27 | ||||||||||||
16 | 160.67 | 198.38 | 0.81 | 0.066 7 | 0.004 1 | 1.230 8 | 0.093 2 | 0.133 9 | 0.005 9 | 827 | 87 | 815 | 42 | 810 | 34 | ||||||||||||
17 | 562.94 | 376.06 | 1.5 | 0.067 | 0.004 1 | 0.937 4 | 0.071 6 | 0.101 4 | 0.004 7 | 838 | 86 | 672 | 38 | 623 | 27 | ||||||||||||
18 | 374 | 395.9 | 0.94 | 0.066 4 | 0.004 5 | 1.015 8 | 0.083 2 | 0.111 | 0.005 1 | 818 | 97 | 712 | 42 | 679 | 30 | ||||||||||||
19 | 267.99 | 225.54 | 1.19 | 0.099 9 | 0.007 2 | 1.699 1 | 0.144 7 | 0.123 3 | 0.005 7 | 1 622 | 92 | 1 008 | 54 | 750 | 33 | ||||||||||||
20 | 342.02 | 632.93 | 0.54 | 0.097 6 | 0.005 5 | 1.172 9 | 0.084 1 | 0.087 2 | 0.003 9 | 1 578 | 71 | 788 | 39 | 539 | 23 | ||||||||||||
21 | 302.72 | 473.44 | 0.64 | 0.147 5 | 0.012 | 1.958 7 | 0.187 6 | 0.096 3 | 0.004 9 | 2 317 | 96 | 1 101 | 64 | 593 | 29 | ||||||||||||
22 | 257.13 | 436.67 | 0.59 | 0.102 9 | 0.007 | 1.138 8 | 0.097 4 | 0.080 3 | 0.004 2 | 1 677 | 85 | 772 | 46 | 498 | 25 | ||||||||||||
23 | 289.32 | 416.76 | 0.69 | 0.067 2 | 0.003 9 | 1.160 9 | 0.084 6 | 0.125 4 | 0.005 6 | 843 | 81 | 782 | 40 | 761 | 32 | ||||||||||||
24 | 415.65 | 398.12 | 1.04 | 0.065 | 0.003 6 | 1.053 9 | 0.074 2 | 0.117 6 | 0.005 2 | 775 | 78 | 731 | 37 | 717 | 30 | ||||||||||||
25 | 989.16 | 1 916.99 | 0.52 | 0.046 1 | 0.005 6 | 0.130 5 | 0.015 1 | 0.020 6 | 0.000 8 | 239 | 125 | 14 | 131 | 5 | |||||||||||||
26 | 253.03 | 198.89 | 1.27 | 0.081 2 | 0.005 | 1.333 | 0.102 1 | 0.119 1 | 0.005 4 | 1 227 | 82 | 860 | 44 | 725 | 31 | ||||||||||||
27 | 455.38 | 597.31 | 0.76 | 0.061 3 | 0.004 6 | 0.970 2 | 0.085 8 | 0.114 9 | 0.005 3 | 649 | 112 | 689 | 44 | 701 | 31 | ||||||||||||
28 | 192.32 | 185.44 | 1.04 | 0.064 5 | 0.004 4 | 1.326 9 | 0.108 9 | 0.149 3 | 0.006 8 | 757 | 99 | 858 | 48 | 897 | 38 | ||||||||||||
29 | 294.05 | 367.14 | 0.8 | 0.065 5 | 0.003 8 | 1.060 1 | 0.076 8 | 0.117 3 | 0.005 2 | 791 | 81 | 734 | 38 | 715 | 30 | ||||||||||||
30 | 230.14 | 200.87 | 1.15 | 0.077 7 | 0.005 5 | 1.455 2 | 0.123 4 | 0.135 8 | 0.006 3 | 1 140 | 97 | 912 | 51 | 821 | 36 | ||||||||||||
31 | 260.66 | 723.58 | 0.36 | 0.074 8 | 0.004 3 | 0.925 8 | 0.067 5 | 0.089 8 | 0.004 | 1 062 | 78 | 665 | 36 | 554 | 24 | ||||||||||||
32 | 2 306.86 | 1 890.61 | 1.22 | 0.106 | 0.006 | 0.588 4 | 0.042 4 | 0.040 3 | 0.001 8 | 1 731 | 70 | 470 | 27 | 255 | 11 | ||||||||||||
灰白色中粗粒花岗岩 | |||||||||||||||||||||||||||
1 | 149.671 07 | 156.982 43 | 0.953 425 6 | 0.077 07 | 0.005 9 | 1.177 2 | 0.100 21 | 0.110 78 | 0.004 13 | 1 123 | 111 | 790 | 47 | 677 | 24 | ||||||||||||
2 | 634.060 18 | 483.761 95 | 1.310 686 3 | 0.086 76 | 0.005 8 | 0.990 53 | 0.073 62 | 0.082 8 | 0.002 7 | 1 355 | 93 | 699 | 38 | 513 | 16 | ||||||||||||
3 | 306.696 74 | 304.856 56 | 1.006 036 2 | 0.110 17 | 0.007 26 | 1.592 37 | 0.116 52 | 0.104 83 | 0.003 34 | 1 802 | 87 | 967 | 46 | 643 | 20 | ||||||||||||
4 | 168.948 09 | 144.843 89 | 1.166 415 | 0.065 07 | 0.004 8 | 1.196 72 | 0.097 19 | 0.133 38 | 0.004 51 | 777 | 114 | 799 | 45 | 807 | 26 | ||||||||||||
5 | 247.152 57 | 376.989 63 | 0.655 595 1 | 0.070 87 | 0.004 52 | 1.183 07 | 0.084 32 | 0.121 07 | 0.003 85 | 954 | 94 | 793 | 39 | 737 | 22 | ||||||||||||
6 | 2 144.279 7 | 1 388.478 5 | 1.544 337 7 | 0.046 05 | 0.004 | 0.249 33 | 0.020 82 | 0.039 27 | 0.000 93 | 191 | 226 | 17 | 248 | 6 | |||||||||||||
7 | 351.505 29 | 442.921 24 | 0.793 606 8 | 0.078 01 | 0.005 15 | 1.176 19 | 0.087 17 | 0.109 35 | 0.003 68 | 1 147 | 94 | 790 | 41 | 669 | 21 | ||||||||||||
8 | 354.322 57 | 492.087 41 | 0.720 039 9 | 0.090 68 | 0.005 99 | 0.910 6 | 0.067 39 | 0.072 83 | 0.002 43 | 1 440 | 90 | 657 | 36 | 453 | 15 | ||||||||||||
9 | 588.123 41 | 1 102.442 1 | 0.533 473 3 | 0.118 68 | 0.007 99 | 0.976 23 | 0.073 56 | 0.059 66 | 0.002 02 | 1 936 | 87 | 692 | 38 | 374 | 12 | ||||||||||||
10 | 888.199 24 | 1 450.600 9 | 0.612 297 5 | 0.140 29 | 0.009 96 | 1.021 92 | 0.080 93 | 0.052 83 | 0.001 85 | 2 231 | 89 | 715 | 41 | 332 | 11 | ||||||||||||
11 | 381.355 69 | 329.541 85 | 1.157 229 9 | 0.080 76 | 0.005 54 | 1.342 15 | 0.101 59 | 0.120 53 | 0.003 85 | 1 216 | 99 | 864 | 44 | 734 | 22 | ||||||||||||
12 | 684.989 16 | 904.253 14 | 0.757 519 3 | 0.098 39 | 0.006 63 | 0.852 84 | 0.063 56 | 0.062 87 | 0.002 | 1 594 | 92 | 626 | 35 | 393 | 12 | ||||||||||||
13 | 513.82 | 557.321 59 | 0.921 945 3 | 0.113 99 | 0.006 94 | 1.523 02 | 0.104 45 | 0.096 9 | 0.003 07 | 1 864 | 78 | 940 | 42 | 596 | 18 | ||||||||||||
14 | 327.226 65 | 223.377 34 | 1.464 905 3 | 0.074 58 | 0.004 96 | 1.067 | 0.080 09 | 0.103 76 | 0.003 6 | 1 057 | 96 | 737 | 39 | 636 | 21 | ||||||||||||
15 | 273.815 28 | 567.772 16 | 0.482 262 6 | 0.101 67 | 0.006 49 | 1.231 27 | 0.088 32 | 0.087 84 | 0.002 87 | 1 655 | 85 | 815 | 40 | 543 | 17 | ||||||||||||
16 | 1 378.725 3 | 1 453.815 8 | 0.948 349 3 | 0.117 6 | 0.008 99 | 1.015 11 | 0.087 21 | 0.062 6 | 0.002 46 | 1 920 | 98 | 711 | 44 | 391 | 15 | ||||||||||||
17 | 154.337 38 | 192.261 42 | 0.802 747 5 | 0.081 87 | 0.006 78 | 1.418 34 | 0.127 18 | 0.125 65 | 0.004 34 | 1 242 | 122 | 897 | 53 | 763 | 25 | ||||||||||||
18 | 926.376 14 | 1 015.220 9 | 0.912 487 3 | 0.090 45 | 0.005 68 | 0.773 33 | 0.054 46 | 0.062 01 | 0.001 98 | 1 435 | 86 | 582 | 31 | 388 | 12 | ||||||||||||
19 | 371.491 7 | 601.158 91 | 0.617 959 2 | 0.084 98 | 0.006 67 | 1.378 95 | 0.122 22 | 0.117 68 | 0.004 85 | 1 315 | 109 | 880 | 52 | 717 | 28 | ||||||||||||
20 | 648.983 33 | 725.294 6 | 0.894 785 8 | 0.096 | 0.006 66 | 1.075 78 | 0.081 87 | 0.081 27 | 0.002 54 | 1 548 | 96 | 742 | 40 | 504 | 15 | ||||||||||||
21 | 577.454 01 | 500.641 43 | 1.153 428 3 | 0.111 14 | 0.007 18 | 1.431 01 | 0.103 16 | 0.093 39 | 0.002 98 | 1 818 | 85 | 902 | 43 | 576 | 18 | ||||||||||||
22 | 1 959.226 1 | 1 266.946 1 | 1.546 416 3 | 0.127 02 | 0.008 22 | 1.004 73 | 0.075 02 | 0.057 37 | 0.002 14 | 2 057 | 80 | 706 | 38 | 360 | 13 | ||||||||||||
23 | 997.528 59 | 1 169.791 3 | 0.852 740 6 | 0.104 31 | 0.006 23 | 0.933 56 | 0.063 59 | 0.064 91 | 0.002 12 | 1 702 | 78 | 670 | 33 | 405 | 13 | ||||||||||||
24 | 345.202 45 | 623.503 82 | 0.553 649 3 | 0.093 71 | 0.006 06 | 0.956 16 | 0.068 54 | 0.074 | 0.002 3 | 1 502 | 89 | 681 | 36 | 460 | 14 | ||||||||||||
25 | 825.054 66 | 1 672.045 1 | 0.493 440 4 | 0.089 28 | 0.005 39 | 0.547 17 | 0.037 41 | 0.044 45 | 0.001 43 | 1 410 | 82 | 443 | 25 | 280 | 9 | ||||||||||||
26 | 256.908 02 | 280.222 97 | 0.916 798 6 | 0.074 67 | 0.005 22 | 1.265 81 | 0.097 93 | 0.122 96 | 0.004 08 | 1 060 | 103 | 831 | 44 | 748 | 23 | ||||||||||||
27 | 240.136 77 | 314.163 64 | 0.764 368 4 | 0.075 47 | 0.004 81 | 1.217 98 | 0.086 52 | 0.117 04 | 0.003 67 | 1 081 | 92 | 809 | 40 | 714 | 21 | ||||||||||||
28 | 1 864.141 2 | 1 882.394 | 0.990 303 4 | 0.152 8 | 0.008 89 | 1.105 82 | 0.073 56 | 0.052 49 | 0.001 69 | 2 377 | 70 | 756 | 35 | 330 | 10 | ||||||||||||
29 | 1 019.152 1 | 1 778.956 2 | 0.572 893 3 | 0.187 9 | 0.011 55 | 0.905 2 | 0.064 31 | 0.034 94 | 0.001 25 | 2 724 | 71 | 655 | 34 | 221 | 8 | ||||||||||||
30 | 262.946 42 | 365.560 99 | 0.719 295 6 | 0.083 47 | 0.005 58 | 1.481 89 | 0.110 29 | 0.128 76 | 0.004 2 | 1 280 | 94 | 923 | 45 | 781 | 24 | ||||||||||||
31 | 1 695.790 1 | 1 210.949 4 | 1.400 380 7 | 0.046 05 | 0.003 05 | 0.199 36 | 0.012 08 | 0.031 4 | 0.000 85 | 146 | 185 | 10 | 199 | 5 | |||||||||||||
32 | 424.562 97 | 514.095 72 | 0.825 844 2 | 0.073 18 | 0.004 55 | 0.948 37 | 0.068 67 | 0.093 99 | 0.003 49 | 1 019 | 88 | 677 | 36 | 579 | 21 |
Fig.5 Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element patterns (b) for the Eshan granites. Normalization values after [75-76].
岩性 | 样号 | 年龄 | 87Rb/86Sr | 87Sr/86Sr | ±2σ | εSr(t) | (87Sr/86S)i |
---|---|---|---|---|---|---|---|
肉红色中粗粒花岗岩 | ZHM1-05 | 746 | 17.836 64 | 0.900 37 | 0.000 03 | 94.2 | 0.710 42 |
ZHM1-06 | 746 | 16.933 61 | 0.895 21 | 0.000 03 | 157.4 | 0.714 87 | |
灰白色中粗粒花岗岩 | ZHM2-01 | 732 | 24.018 4 | 0.963 27 | 0.000 02 | 120.7 | 0.712 31 |
ZHM2-02 | 732 | 13.775 26 | 0.822 49 | 0.000 02 | -358.9 | 0.678 55 | |
岩性 | 样号 | ±1σ | 147Sm/144Nd | 143Nd/144Nd | (143Nd/144Nd)i | εNd(t) | TDM2 |
肉红色中粗粒花岗岩 | ZHM1-05 | 0.000 02 | 0.175 12 | 0.512 1 | 0.511 25 | -8.4 | 2 105 |
ZHM1-06 | 0.000 03 | 0.170 56 | 0.512 07 | 0.511 24 | -8.6 | 2 120 | |
灰白色中粗粒花岗岩 | ZHM2-01 | 0.000 03 | 0.216 71 | 0.512 35 | 0.511 31 | -7.5 | 2 023 |
ZHM2-02 | 0.000 03 | 0.238 51 | 0.512 28 | 0.511 14 | -10.8 | 2 290 |
Table 3 Sr-Nd isotopic analyses of Eshan granites
岩性 | 样号 | 年龄 | 87Rb/86Sr | 87Sr/86Sr | ±2σ | εSr(t) | (87Sr/86S)i |
---|---|---|---|---|---|---|---|
肉红色中粗粒花岗岩 | ZHM1-05 | 746 | 17.836 64 | 0.900 37 | 0.000 03 | 94.2 | 0.710 42 |
ZHM1-06 | 746 | 16.933 61 | 0.895 21 | 0.000 03 | 157.4 | 0.714 87 | |
灰白色中粗粒花岗岩 | ZHM2-01 | 732 | 24.018 4 | 0.963 27 | 0.000 02 | 120.7 | 0.712 31 |
ZHM2-02 | 732 | 13.775 26 | 0.822 49 | 0.000 02 | -358.9 | 0.678 55 | |
岩性 | 样号 | ±1σ | 147Sm/144Nd | 143Nd/144Nd | (143Nd/144Nd)i | εNd(t) | TDM2 |
肉红色中粗粒花岗岩 | ZHM1-05 | 0.000 02 | 0.175 12 | 0.512 1 | 0.511 25 | -8.4 | 2 105 |
ZHM1-06 | 0.000 03 | 0.170 56 | 0.512 07 | 0.511 24 | -8.6 | 2 120 | |
灰白色中粗粒花岗岩 | ZHM2-01 | 0.000 03 | 0.216 71 | 0.512 35 | 0.511 31 | -7.5 | 2 023 |
ZHM2-02 | 0.000 03 | 0.238 51 | 0.512 28 | 0.511 14 | -10.8 | 2 290 |
岩石 | 样号 | TZr/℃ | 岩石 | 样号 | TZr/℃ |
---|---|---|---|---|---|
肉红色中粗粒花岗岩 | ZHM1-01 | 767.1 | 灰白色中粗粒花岗岩 | ZHM2-01 | 765.0 |
肉红色中粗粒花岗岩 | ZHM1-02 | 781.3 | 灰白色中粗粒花岗岩 | ZHM2-02 | 764.9 |
肉红色中粗粒花岗岩 | ZHM1-03 | 744.7 | 灰白色中粗粒花岗岩 | ZHM2-03 | 764.3 |
肉红色中粗粒花岗岩 | ZHM1-04 | 767.5 | 灰白色中粗粒花岗岩 | ZHM2-04 | 767.3 |
肉红色中粗粒花岗岩 | ZHM1-05 | 762.8 | 灰白色中粗粒花岗岩 | ZHM2-05 | 754.4 |
肉红色中粗粒花岗岩 | ZHM1-06 | 773.9 | 灰白色中粗粒花岗岩 | ZHM2-06 | 766.4 |
肉红色中粗粒花岗岩 | ZHM1-07 | 769.2 | 灰白色中粗粒花岗岩 | ZHM2-07 | 759.6 |
肉红色中粗粒花岗岩 | ZHM1-08 | 771.5 | 灰白色中粗粒花岗岩 | ZHM2-08 | 759.3 |
Table 4 Zircon saturation temperatures of Eshan granites
岩石 | 样号 | TZr/℃ | 岩石 | 样号 | TZr/℃ |
---|---|---|---|---|---|
肉红色中粗粒花岗岩 | ZHM1-01 | 767.1 | 灰白色中粗粒花岗岩 | ZHM2-01 | 765.0 |
肉红色中粗粒花岗岩 | ZHM1-02 | 781.3 | 灰白色中粗粒花岗岩 | ZHM2-02 | 764.9 |
肉红色中粗粒花岗岩 | ZHM1-03 | 744.7 | 灰白色中粗粒花岗岩 | ZHM2-03 | 764.3 |
肉红色中粗粒花岗岩 | ZHM1-04 | 767.5 | 灰白色中粗粒花岗岩 | ZHM2-04 | 767.3 |
肉红色中粗粒花岗岩 | ZHM1-05 | 762.8 | 灰白色中粗粒花岗岩 | ZHM2-05 | 754.4 |
肉红色中粗粒花岗岩 | ZHM1-06 | 773.9 | 灰白色中粗粒花岗岩 | ZHM2-06 | 766.4 |
肉红色中粗粒花岗岩 | ZHM1-07 | 769.2 | 灰白色中粗粒花岗岩 | ZHM2-07 | 759.6 |
肉红色中粗粒花岗岩 | ZHM1-08 | 771.5 | 灰白色中粗粒花岗岩 | ZHM2-08 | 759.3 |
Fig.10 Schematic diagram for discriminating the tectonic environment of Emeishan granite. R1=1000×[4Si-11(Na+K)-2(Fe+Ti)]; R2=1000×(6Ca+2Mg+Al); elemental symbols in the calculations of R1 and R2 represent corresponding cation ratios; a, basemap according to reference [114]; b, basemap according to reference [115]; c, basemap according to reference [116]; d, basemap according to reference [117]. Data on continental I-type granite diorite-granite are from [54].
[1] | CAWOOD P A, STRACHAN R A, PISAREVSKY S A, et al. Linking collisional and accretionary orogens during Rodinia assembly and breakup: implications for models of supercontinent cycles[J]. Earth and Planetary Science Letters, 2016, 449: 118-126. |
[2] | ZHENG Y F, WU Y B, CHEN F K, et al. Zircon U-Pb and oxygen isotope evidence for a large-scale 18O depletion event in igneous rocks during the Neoproterozoic[J]. Geochimica et Cosmochimica Acta, 2004, 68(20): 4145-4165. |
[3] | LI X H, LI W X, LI Z X, et al. 850-790 Ma bimodal volcanic and intrusive rocks in northern Zhejiang, South China: a major episode of continental rift magmatism during the breakup of Rodinia[J]. Lithos, 2008, 102(1/2): 341-357. |
[4] | LI Z X, BOGDANOVA S V, COLLINS A S, et al. Assembly, configuration, and break-up history of Rodinia: a synthesis[J]. Precambrian Research, 2008, 160(1/2): 179-210. |
[5] | ZHAO G C, CAWOOD P A. Precambrian geology of China[J]. Precambrian Research, 2012, 222/223: 13-54. |
[6] | WANG X L, ZHOU J C, WAN Y S, et al. Magmatic evolution and crustal recycling for Neoproterozoic strongly peraluminous granitoids from southern China: Hf and O isotopes in zircon[J]. Earth and Planetary Science Letters, 2013, 366: 71-82. |
[7] | WANG X L, ZHOU J C, GRIFFIN W L, et al. Geochemical zonation across a Neoproterozoic orogenic belt: isotopic evidence from granitoids and metasedimentary rocks of the Jiangnan orogen, China[J]. Precambrian Research, 2014, 242: 154-171. |
[8] | ZHENG Y F, XIAO W J, ZHAO G C. Introduction to tectonics of China[J]. Gondwana Research, 2013, 23(4): 1189-1206. |
[9] | ZHAO J H, LI Q W, LIU H, et al. Neoproterozoic magmatism in the western and northern margins of the Yangtze Block (South China) controlled by slab subduction and subduction-transform-edgepropagator[J]. Earth-Science Reviews, 2018, 187: 1-18. |
[10] | LI Z X, LI X H, ZHOU H, et al. Grenvillian continental collision in South China: new SHRIMP U-Pb zircon results and implications for the configuration of Rodinia[J]. Geology, 2002, 30: 163-166. |
[11] | 徐丽娟, 李萍, 刘铮, 等. 扬子地块西缘峨山新元古代A2型花岗闪长岩的成因及构造意义[J]. 岩石矿物学杂志, 2021, 40(2): 383-394. |
[12] | ZHOU M F, YAN D P, KENNEDY A K, et al. SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China[J]. Earth and Planetary Science Letters, 2002, 196: 51-67. |
[13] | ZHOU M F, MA Y X, YAN D P, et al. The Yanbian terrane(southern Sichuan Province, SW China): a Neoproterozoic arc assemblage in the western margin of the Yangtze Block[J]. Precambrian Research, 2006, 144: 19-38. |
[14] | ZHOU M F, YAN D P, WANG C L, et al. Subduction-related origin of the 750 Ma Xuelongbao adakitic complex (Sichuan Province, China): implications for the tectonic setting of the giant Neoproterozoic magmatic event in South China[J]. Earth and Planetary Science Letters, 2006, 248(1/2): 286-300. |
[15] | ZHAO G. Jiangnan orogen in South China: developing from divergent double subduction[J]. Gondwana Research, 2015, 27: 1173-1180. |
[16] | 颜丹平, 周美夫, 宋鸿林, 等. 华南在Rodinia古陆中位置的讨论: 扬子地块西缘变质岩浆杂岩证据及其与Seychelles地块的对比[J]. 地学前缘, 2003, 10(4): 249-257. |
[17] | 裴先治, 李佐臣, 丁仨平, 等. 扬子地块西北缘轿子顶新元古代过铝质花岗岩: 锆石SHRIMP U-Pb年龄和岩石地球化学及其构造意义[J]. 地学前缘, 2009, 16(3): 231-249. |
[18] |
寇彩化, 刘燕学, 李江, 等. 江南造山带西段桂北四堡地区830 Ma辉长岩锆石SIMS U-Pb年代学和岩石地球化学特征及其岩石成因研究[J]. 地学前缘, 2022, 29(2): 218-233.
DOI |
[19] | ZHAO J H, ZHOU M F, YAN D P, et al. Reappraisal of the ages of Neoproterozoic strata in South China: no connection with the Grenvillian orogeny[J]. Geology, 2011, 39(4): 299-302. |
[20] | GAO S, LING W L, QIU Y M, et al. Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze Craton: evidence for cratonic evolution and redistribution of REE during crustal anatexis[J]. Geochimica et Cosmochimica Acta, 1999, 63(13/14): 2071-2088. |
[21] | GAO S, YANG J, ZHOU L, et al. Age and growth of the Archean Kongling terrain, South China, with emphasis on 3.3 Ga granitoid gneisses[J]. American Journal of Science, 2011, 311(2): 153182. |
[22] | GUO J L, GAO S, WU Y B, et al. 3.45 Ga granitic gneisses from the Yangtze Craton, South China: implications for Early Archean crustal growth[J]. Precambrian Research, 2014, 242: 82-95. |
[23] | CHEN W T, ZHOU M F, ZHAO X F. Late Paleoproterozoic sedimentary and mafic rocks in the Hekou area, SW China: implication for the reconstruction of the Yangtze Block in Columbia[J]. Precambrian Research, 2013, 231: 61-77. |
[24] | ZHAO X F, ZHOU M F, LI J W, et al. Late Paleoproterozoic to early Mesoproterozoic Dongchuan Group in Yunnan, SW China: implications for tectonic evolution of the Yangtze Block[J]. Precambrian Research, 2010, 182(1/2): 57-69. |
[25] | GREENLREE M, LI Z X. The oldest known rocks in south-western China: SHRIMP U-Pb magmatic crystallisation age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group[J]. Journal of Asian Earth Sciences, 2008, 33: 289-302. |
[26] | 杨红, 刘福来, 杜利林, 等. 扬子地块西南缘大红山群老厂河组变质火山岩的锆石U-Pb定年及其地质意义[J]. 岩石学报, 2012, 28(9): 2994-3014. |
[27] | KOU C H, ZHANG Z C, SANTOSH M, et al. Oldest volcanic-hosted submarine iron ores in South China: evidence from zircon U-Pb geochronology and geochemistry of the Paleoproterozoic Dahongshan iron deposit[J]. Gondwana Research, 2017, 49: 182-204. |
[28] | GREENTREE M R, LI Z X, LI X H, et al. Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia[J]. Precambrian Research, 2006, 151(1/2): 79-100. |
[29] | LI H K, ZHANG C L, YAO C Y, et al. U-Pb zircon age and Hf isotope compositions of Mesoproterozoic sedimentary strata on the western margin of the Yangtze massif[J]. Science China Earth Sciences, 2013, 56(4): 628-639. |
[30] | ZHU W G, ZHONG H, LI Z X, et al. SIMS zircon U-Pb ages, geochemistry and Nd-Hf isotopes of ca. 1.0 Ga mafic dykes and volcanic rocks in the Huili area, SW China: origin and tectonic significance[J]. Precambrian Research, 2016, 273: 67-89. |
[31] | CHEN W T, SUN W H, WANG W, et al. “Grenvillian” intraplate mafic magmatism in the southwestern Yangtze Block, SW China[J]. Precambrian Research, 2014, 242: 138-153. |
[32] | 刘桂春, 陈光艳, 李静, 等. 扬子西缘祥云响水花岗岩体的成因: 锆石U-Pb年代学, 岩石地球化学和Sr-Nd同位素制约[J]. 地球科学, 2020, 45(7): 2426. |
[33] | LI X H, LI W X, LI Q L, et al. Petrogenesis and tectonic significance of the -850 Ma Gangbian alkaline complex in South China: evidence from in situ zircon U-Pb dating, Hf-O isotopes and whole-rock geochemistry[J]. Lithos, 2010, 114(1): 1-15. |
[34] | YANG Y N, WANG X C, LI Q L, et al. Integrated in situ U-Pb age and Hf-O analyses of zircon from Suixian Group in northern Yangtze: new insights into the Neoproterozoic low-delta O-18 magmas in the South China Block[J]. Precambrian Research, 2016, 273: 151-164. |
[35] | WANG Y, ZHOU Y, CAI Y, et al. Geochronological and geochemical constraints on the petrogenesis of the Ailaoshan granitic and migmatite rocks and its implications on Neoproterozoic subduction along the SW Yangtze Block[J]. Precambrian Research, 2016, 283(1): 106-124. |
[36] | CHEN X, LIU J, QI Y, et al. Neoproterozoic granitic magmatism along the Ailao Shan-Red River belt: U-Pb zircon geochronology, Lu-Hf isotopes and tectonic implications[J]. Precambrian Research, 2017, 299: 244-263. |
[37] | 李献华, 李武显, 何斌. 华南陆块的形成与Rodinia超大陆聚合-裂解: 观察、 解释与检验[J]. 矿物岩石地球化学通报, 2012, 31(6): 543-559. |
[38] | 云南省地矿局. 云南省区域地质志[M]. 北京: 地质出版社, 1990. |
[39] | HU J, ZHANG S T, ZHANG G Z, et al. Geochemistry and tectonic setting of the Eshan granites in the southwestern margin of the Yangtze Plate, Yunnan[J]. Journal of Earth Science, 2018, 29(1): 130-143. |
[40] | LI W X, LI X H, LI Z X. Ca. 850 Ma bimodal volcanic rocks in northeastern Jiangxi Province, South China: initial extension during the breakup of Rodinia?[J]. American Journal of Science, 2010, 310(9): 951-980. |
[41] | WANG X L, ZHAO G, ZHOU J C, et al. Geochronology and Hf isotopes of zircon from volcanic rocks of the Shuangqiaoshan Group, South China: implications for the Neoproterozoic tectonic evolution of the eastern Jiangnan orogen[J]. Gondwana Research, 2008, 14(3): 355-367. |
[42] | ZHOU J C, WANG X L, QIU J S. Geochronology of Neoproterozoic mafic rocks and sandstones from northeastern Guizhou, South China: coeval arc magmatism and sedimentation[J]. Precambrian Research, 2009, 170(1): 27-42. |
[43] | 周金城, 王孝磊, 邱检生. 江南造山带形成过程中若干新元古代地质事件[J]. 高校地质学报, 2009, 15(4): 453-459. |
[44] | LI Z X, LI X H, KINNY P D, et al. The breakup of Rodinia: did it start with a mantle plume beneath South China?[J]. Earth and Planetary Science Letters, 1999, 173(3): 171-181. |
[45] | SUN W H, ZHOU M F. The -860 Ma, Cordilleran-type Guandaoshan dioritic pluton in the Yangtze Block, SW China: implications for the origin of Neoproterozoic magmatism[J]. Journal of Geology, 2008, 116(3): 238-253. |
[46] | 沈渭洲, 高剑峰, 徐士进, 等. 扬子板块西缘泸定桥头基性杂岩体的地球化学特征和成因[J]. 高校地质学报, 2002, 8(4): 380-389. |
[47] | 刘树文, 闫全人, 李秋根, 等. 扬子克拉通西缘康定杂岩中花岗质岩石的成因及其构造意义[J]. 岩石学报, 2009, 25(8): 1883-1896. |
[48] | LAI S C, QIN J F, ZHU R Z, et al. Neoproterozoic quartz monzodiorite-granodiorite association from the Luding-Kangding area: implications for the interpretation of an active continental margin along the Yangtze Block (South China Block)[J]. Precambrian Research, 2015, 267(3/4): 196-208. |
[49] | MENG E, LIU F L, DU L L, et al. Petrogenesis and tectonic significance of the Baoxing granitic and mafic intrusions, southwestern China: evidence from zircon U-Pb dating and Lu-Hf isotopes, and whole-rock geochemistry[J]. Gondwana Research, 2015, 28(2): 800-815. |
[50] | 刘树文, 杨恺, 李秋根, 等. 新元古代宝兴杂岩的岩石成因及其对扬子西缘构造环境的制约[J]. 地学前缘, 2009, 16(2): 107-118. |
[51] | SUN W H, ZHOU M F, YAN D P, et al. Provenance and tectonic setting of the Neoproterozoic Yanbian Group, western Yangtze Block (SW China)[J]. Precambrian Research, 2008, 167(1): 213-236. |
[52] | DU L L, GUO J H, NUTMAN A P, et al. Implications for Rodinia reconstructions for the initiation of Neoproterozoic subduction at -860 Ma on the western margin of the Yangtze Block: evidence from the Guandaoshan pluton[J]. Lithos, 2014, 196/197: 67-82. |
[53] | MUNTEANU M, WILSON A, YAO Y, et al. The Tongde dioritic pluton (Sichuan, SW China) and its geotectonic setting: regional implications of a local-scale study[J]. Gondwana Research, 2010, 18(2): 455-465. |
[54] | 赖绍聪, 朱毓. 扬子板块西缘新元古代典型中酸性岩浆事件及其深部动力学机制: 研究进展与展望[J]. 地质力学学报, 2020, 26(5): 759-790. |
[55] | ZHAO X F, ZHOU M F, LI J W, et al. Association of Neoproterozoic A- and I-type granites in South China: implications for generation of A-type granites in a subduction-related environment[J]. Chemical Geology, 2009, 257(1/2): 1-15. |
[56] | HUANG X L, XU Y G, LI X H, et al. Petrogenesis and tectonic implications of Neoproterozoic, highly fractionated A-type granites from Mianning, South China[J]. Precambrian Research, 2008, 165(3/4): 190-204. |
[57] | 鄢圣武, 白宪洲, 伍文湘, 等. 扬子板块西缘泸沽A型花岗岩成因与变泥质岩熔融[J]. 中国地质, 2017, 44(1): 163-150. |
[58] | ZHU Y, LAI S C, QIN J F, et al. Petrogenesis and geodynamic implications of Neoproterozoic gabbro-diorites, adakitic granites, and A-type granites in the southwestern margin of the Yangtze Block, South China[J]. Journal of Asian Earth Sciences, 2019, 183: 103977. |
[59] | HUANG X L, XU Y G, LAN J B, et al. Neoproterozoic adakitic rocks from Mopanshan in the western Yangtze Craton: partial melts of a thickened lower crust[J]. Lithos, 2009, 112(3): 367-381. |
[60] | ZHAO J H, ZHOU M F. Neoproterozoic adakitic plutons and arc magmatism along the western margin of the Yangtze Block, South China[J]. Journal of Geology, 2007, 115(6): 675-689. |
[61] | ZHAO J H, ZHOU M F, YAN D P, et al. Zircon Lu-Hf isotopic constraints on Neoproterozoic subduction-related crustal growth along the western margin of the Yangtze Block, South China[J]. Precambrian Research, 2008, 163(3): 189-209. |
[62] | 朱毓, 赖绍聪, 赵少伟, 等. 扬子板块西缘石棉安顺场新元古代钾长花岗岩地球化学特征及其地质意义[J]. 地质论评, 2017, 63(5), 1193-1208. |
[63] | 赖绍聪, 秦江锋, 朱韧之, 等. 扬子地块西缘天全新元古代过铝质花岗岩类成因机制及其构造动力学背景[J]. 岩石学报, 2015(8): 133-146. |
[64] | 郭春丽, 王登红, 陈毓川, 等. 川西新元古代花岗质杂岩体的锆石SHRIMP U-Pb年龄、 元素和Nd-Sr同位素地球化学研究: 岩石成因与构造意义[J]. 岩石学报, 2007, 23(10): 2457-2470. |
[65] | 张玉顺, 吴玉, 潘家永, 等. 扬子板块西缘黑么花岗质岩体的成因与构造意义: 来自锆石U-Pb年代学和岩石地球化学的约束[J]. 矿物岩石地球化学通报, 2020, 39(5): 983-998. |
[66] | 胡金. 云南省峨山花岗岩体新元古代岩浆演化及成矿制约[D]. 昆明: 昆明理工大学, 2018. |
[67] | 薛玺会, 蔡忠柏, 熊家镛. 关于云南峨山花岗岩体的时代问题[J]. 岩石学报, 1986, 2(1): 50-58. |
[68] | GAO S, LIU X M, YUAN H L, et al. Analysis of forty-two major and trace elements of USGS and NIST SRM Glasses by LAICPMS, Geostand[J]. Geostandards Newsletter, 2002, 22: 181-195. |
[69] | LIU Y S, ZONG K Q, KELEMEN P B, et al. Geochemistry and magmatic history of eclogites and ultramafic rock s from the Chinese continental scientific drill hole: subduction and ultrahigh-pressure metamorphism of lower crustal cumulates[J]. Chemical Geology, 2008, 247: 133-153. |
[70] | LIU Y, ZHAO C, ZONG K Q, et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Science Bulletin, 2010, 55(15): 1535-1546. |
[71] | LUDWIG K R. ISOPLOT 3.00: a geochronological toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center, 2003. |
[72] | MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4): 215-224. |
[73] | MARTIN H, SMITHIES R H, RAPP R, et al. An overview of adakite, tonalite-trondhjemite-granodiorite(TTG), and sanukitoid: relationships and some implications for crustal evolution[J]. Lithos, 2005, 79(1/2): 1-24. |
[74] | MANIAR P D, PICCOLI P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989, 101(5): 635-643. |
[75] | BOYNTON W V. Geochemistry of the rare earth elements: meteorite studies[M]//HENDERSDN P. Rare earth element geochemistry. Amsterdam: Elsevier, 1984: 63-114. |
[76] | SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1): 313-345. |
[77] | MILLER C F, MCDOWELL S M, MAPES R W. Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance[J]. Geology, 2003, 31(6): 529. |
[78] | ROMER R L, FÖRSTER H J, HAHNE K. Strontium isotopes: a persistent tracer for the recycling of Gondwana crust in Variscan orogen[J]. Gondwana Research, 2012, 22: 262-278. |
[79] | 邱检生, 肖娥, 胡建, 等. 福建北东沿海高分异I型花岗岩的成因: 锆石U-Pb年代学, 地球化学和Nd-Hf同位素制约[J]. 岩石学报, 2008, 24(11): 17. |
[80] | JANOUEK V, FRITZ F, MALCOLM R, et al. Deciphering the petrogenesis of deeply buried granites: whole-rock geochemical constraints on the origin of largely undepleted felsic granulites from the Moldanubian zone of the Bohemian massif[J]. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 2004, 95(1/2): 141-159. |
[81] | 吴福元, 刘小驰, 纪伟强, 等. 高分异花岗岩的识别与研究[J]. 中国科学: 地球科学, 2017, 47(7): 21. |
[82] | SYLVESTER P J. Post-collisional alkaline granites[J]. The Journal of Geology, 1989(3): 261-280. |
[83] | KING P L, WHITE A J R, CHAPPELL B W, et al. Characterization and origin of aluminous A-type granites from the Lachlan fold belt, southeastern Australia[J]. Journal of Petrology, 1997(3): 371-391. |
[84] | CHAPPELL B W, WHITE A J R. I- and S-type granites in the Lachlan fold belt[J]. Transactions of the Royal Society of Edinburgh: Earth Sciences, 1992, 83: 1-26. |
[85] | CHEN Y Q, LI G J, QIN L X, et al. Geochronology and geochemistry of Cretaceous-Eocene granites, Tengchong Block(SW China): petrogenesis and implications for Mesozoic-Cenozoic tectonic evolution of Eastern Tethys[J]. Geoscience Frontiers, 2022, 13(2): 220-242. |
[86] | CHAPPELL B W, WHITE A J R. Two contrasting granite type[J]. Pacific Geology, 1974, 8(2): 173-174. |
[87] | CHAPPELL B W. Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites[J]. Lithos, 1999, 46(3): 535-551. |
[88] | WHALEN J B, CURRIE K L, CHAPPELL B W. A-type granites: geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95: 407-419. |
[89] | RAPP R P, SHIMIZU N, NORMAN M D, et al. Reaction between slab-derived melts and peridotite in the mantle wedge: experimental constraints at 3.8 GPa[J]. Chemical Geology, 1999, 160(4): 335-356. |
[90] | SISSON T W, RATAJESKI K, HANKINS W B, et al. Voluminous granitic magmas from common basaltic sources[J]. Contributions to Mineralogy and Petrology, 2005, 148(6): 635-661. |
[91] | BEARD J S, LOFGREN G E. Dehydration melting and water-saturated melting of basaltic and andesitic greenstones and amphibolites at 1, 3, and 6.9 kb[J]. Journal of Petrology, 1991, 32: 365-401. |
[92] | PATIÑO DOUCE A E, BEARD J S. Dehydration-melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar[J]. Journal of Petrology, 1995, 36: 707-738. |
[93] | GAO P, ZHENG Y F, ZHAO Z F. Experimental melts from crustal rocks: a lithochemical constraint on granite petrogenesis[J]. Lithos, 2016, 266/267: 133-157. |
[94] | CHAPPELL B W, BRYANT C J, WYBORN D. Peraluminous I-type granites[J]. Lithos, 2012, 153: 142-153. |
[95] | LI X H, LI Z X, YING L, et al. U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I- and A-type granites from central Guangdong, SE China: a major igneous event in response to foundering of a subducted flat-slab?[J]. Lithos, 2007, 96(1/2): 186-204. |
[96] | LI C Y, ZHANG H, WANG F Y, et al. The formation of the Dabaoshan porphyry molybdenum deposit induced by slab rollback[J]. Lithos, 2012, 150: 101-110. |
[97] | WANG W, ZHOU M F, ZHAO X F, et al. Late Paleoproterozoic to Mesoproterozoic rift successions in SW China: implication for the Yangtze Block-North Australia-Northwest Laurentia connection in the Columbia supercontinent[J]. Sedimentary Geology, 2014, 309: 33-47. |
[98] | RAPP R P, WATSON E B. Dehydration melting of metabasalt at 8-32 kbar: implications for continental growth and crust-mantle recycling[J]. Journal of Petrology, 1995, 36: 891-931. |
[99] | 戴凤岩, 张翊钧. 稀土元素中某些元素异常值在岩石成因研究中的意义[J]. 地质科技情报, 1987(2): 57-61. |
[100] | 刘玉平, 叶霖, 李朝阳, 等. 滇东南发现新元古代岩浆岩: SHRIMP锆石U-Pb年代学和岩石地球化学证据[J]. 岩石学报, 2006, 22(4): 916-926. |
[101] | EVANS D A D, LI Z X, KIRSCHVINK J L, et al. A high quality Mid-Neoproterozoic pole from South China, with implications for ice ages and the breakup configuration of Rodinia[J]. Precambrian Research, 2000, 100: 313-334. |
[102] | 张国伟, 郭安林, 王岳军, 等. 中国华南大陆构造与问题[J]. 中国科学: 地球科学, 2013, 43(10): 1553-1582. |
[103] | 李献华, 周汉文, 李正祥. 扬子块体西缘新元古代双峰式火山岩的锆石U-Pb年龄和岩石化学特征[J]. 地球化学, 2001, 30(4): 315-322. |
[104] | SHELLNUTT J G, ZHOU M F, YAN D P, et al. Longevity of the Permian Emeishan mantle plume (SW China): 1 Ma, 8 Ma or 18 Ma?[J]. Geological Magazine, 2008, 145(3): 373-388. |
[105] | IVANOV A V, MERE S, THOMPSON J, et al. Timing and genesis of the Karoo-Ferrar large igneous province: new high precision U-Pb data for Tasmania confirm short duration of the major magmatic pulse[J]. Chemical Geology, 2017, 455: 32-43. |
[106] | SVENSEN H, CORFU F, POLTEAU S, et al. Rapid magma emplacement in the Karoo large igneous province[J]. Earth and Planetary Science Letters, 2012, 325/326(1): 1-9. |
[107] | AUGLAND L E, RYABOV V V, VERNIKOVSKY V A, et al. The main pulse of the Siberian Traps expanded in size and composition[J]. Scientific Reports, 2020, 9(1): 18723. |
[108] | MICHAEL P E, BLAIR S, KYLE M S, et al. U-Pb zircon age constraints on the earliest eruptions of the Deccan large igneous province, Malwa Plateau, India[J]. Earth and Planetary Science Letters, 2020, 540: 116249. |
[109] | SUN W H, ZHOU M F, GAO J F, et al. Detrital zircon U-Pb geochronological and Lu-Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze Block, SW China[J]. Precambrian Research, 2009, 172(1/2): 99-126. |
[110] | GAO R, CHEN C, WANG H Y, et al. SINOPROBE deep reflection profile reveals a Neoproterozoic subduction zone beneath Sichuan Basin[J]. Earth and Planetary Science Letters, 2016, 454: 86-91. |
[111] | 张慰. 扬子地台西南缘新元古代岩浆杂岩体的构造变形与地质意义[D]. 北京: 中国地质大学(北京), 2017. |
[112] | ZHAO J H, ASIMOW P D, ZHOU M F, et al. An Andean-type arc system in Rodinia constrained by the Neoproterozoic Shimian ophiolite in South China[J]. Precambrian Research, 2017, 296: 93-111. |
[113] | ZHAO J H, ZHOU M F, WU Y B, et al. Coupled evolution of Neoproterozoic arc mafic magmatism and mantle wedge in the western margin of the South China Craton[J]. Contributions to Mineralogy and Petrology, 2019, 174(4): 36. |
[114] | BATCHELOR R A, BOWDEN P. Petrogenetic interpretation of granitoid rock series using multicationic parameters[J]. Chemical Geology, 1985, 48(1/2/3/4): 43-55. |
[115] | HARRIS N B W. Geochemical characteristics of collision-zone magmatism[J]. Collision Tectonics, 1986, 19(1): 67-81. |
[116] | PEARCE J A, HARRIS N B W, TINDLE A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25(4): 956-983. |
[117] | BROWN G C. Calc-alkaline intrusive rocks: their diversity, evolution and relation to volcanic arcs[M]//THORPE R S. Andesites-orogenic andesites and related rocks[M]. New York: John Wiley & Sons, 1982: 437-464. |
[1] | ZHANG Huanbao, HE Haiyang, YANG Shijiao, LI Yalin, BI Wenjun, HAN Shili, GUO Qinpeng, DU Qing. Machine learning-based approach for adakitic rocks tectonic setting determination [J]. Earth Science Frontiers, 2024, 31(4): 417-428. |
[2] | ZHANG Jiawen, LI Mingchao, HAN Shuai, ZHANG Jingyi. Analysis and discrimination of tectonic settings based on stacking quantum neural networks [J]. Earth Science Frontiers, 2024, 31(3): 511-519. |
[3] | HE Bizhu, JIAO Cunli, LIU Ruohan, CAO Zicheng, CAI Zhihui, LAN Mingjie, YUN Xiaorui, ZHU Ding, JIANG Zhongzheng, YANG Yujie, LI Zhenyu. The paleotectonic and paleogeography reconstructions of the Tarim Basin in the Neoproterozoic and prediction of favorable deep source rock areas [J]. Earth Science Frontiers, 2023, 30(4): 19-42. |
[4] | YANG Kunkun, LI Haiyan, ZHAO Hanqing, CHU Runjian, LIU Guanghong, WU Huaichun, ZHANG Shihong. Cyclostratigraphic study of the Neoproterozoic Browne-Hussar formations in western Australia [J]. Earth Science Frontiers, 2023, 30(3): 441-451. |
[5] | LIU Leixin, LI Jianghai, MA Changming. Reconstruction of the Yangtze, Australian and Indian plates in the Late Neoproterozoic (750-540 Ma) using paleomagnetic constraints [J]. Earth Science Frontiers, 2023, 30(2): 154-162. |
[6] | LI Lushun, WANG Zecheng, XIAO Ancheng, HU Anping, CHEN Youzhi, Wang Qianqian. Tectonics of the Neoproterozoic basin and age of the Macaoyuan Group on the northern margin of the Yangtze Block [J]. Earth Science Frontiers, 2022, 29(6): 291-304. |
[7] | ZENG Zhongcheng, HONG Zenglin, BIAN Xiaowei, CHEN Ning, ZHANG Ruoyu, LI Qi. Discovery of Late Ordovician sanukitoid-like diorite in southern Altyn orogeny and its geological significance [J]. Earth Science Frontiers, 2022, 29(4): 345-357. |
[8] | LI Wangpeng, LI Huili, WANG Yi, LIU Shaofeng, ZHANG Zhongpei, YANG Weili, CAI Xiyao, QIAN Tao, LI Xiaojian. Neoproterozoic glaciations in Yecheng area, southwestern margin of the Tarim Basin [J]. Earth Science Frontiers, 2022, 29(3): 356-380. |
[9] | KOU Caihua, LIU Yanxue, LI Jiang, LI Tingdong, DING Xiaozhong, LIU Yong, JIN Shengkai. Geochronology and geochemistry of 830 Ma gabbro in the western segment of the Jiangnan Orogen and constraint on its petrogenesis [J]. Earth Science Frontiers, 2022, 29(2): 218-233. |
[10] | ZHANG Jibiao, DING Xiaozhong, LIU Yanxue. Petrogenesis and tectonic significance of OIB- and arc-type volcanic rocks in the western Yangtze Block: From intracontinental rifting to subduction [J]. Earth Science Frontiers, 2021, 28(4): 250-266. |
[11] | ZHANG Xiaoxu, SU Shangguo, LIU Meiyu, WANG Weizhu. Characteristics and tectonic significance of the early Paleozoic syenite granite from Jinchuan, Gansu Province [J]. Earth Science Frontiers, 2021, 28(4): 283-298. |
[12] | QU Xuejiao, GAO Youfeng, LIN Zhicheng, WANG Pujun, WU Kangjun. Discussion on the characteristics of the Jurassic-Cretaceous boundary correlation in the Songliao Basin and adjacent areas [J]. Earth Science Frontiers, 2021, 28(4): 299-315. |
[13] | WANG Xuying, JIANG Zaixing. Provenance characteristics and tectonic setting analysis of the 3rd Member of the Paleogene Funing Formation, Subei Basin [J]. Earth Science Frontiers, 2021, 28(2): 376-390. |
[14] | HUA Hong, CAI Yaoping, MIN Xiao, CHAI Shu, DAI Qiaokun, CUI Zaihang. Ecological diversity in the terminal Ediacaran Gaojiashan biota [J]. Earth Science Frontiers, 2020, 27(6): 28-46. |
[15] | ZHANG Dayu, FU Xiang, WEI Ouxiang, YE Longxiang, JIANG Hua, ZHANG Yong, XIN Houtian. Discovery of the Silurian andesitic porphyry in the Xiaohulishan Mo-polymetallic deposit, the Beishan district, Inner Mongolia, and its geological significance [J]. Earth Science Frontiers, 2020, 27(3): 222-238. |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||