Geoscience ›› 2020, Vol. 34 ›› Issue (05): 1001-1014.DOI: 10.19657/j.geoscience.1000-8527.2019.032
• Petrology • Previous Articles Next Articles
NONG Junnian1,2(), GUO Shangyu2, SUN Minghang2, TANG Juanhong2, QIN Ruicai2, ZHOU Qiue2
Received:
2018-07-05
Revised:
2020-04-21
Online:
2020-10-28
Published:
2020-10-29
CLC Number:
NONG Junnian, GUO Shangyu, SUN Minghang, TANG Juanhong, QIN Ruicai, ZHOU Qiue. Petrogenesis of the Guluo and Wangjiangchong Shoshonite-gabbro in Southeastern Guangxi Province: Constraints from Petrochemistry, Zircon U-Pb Age and Hf Isotope[J]. Geoscience, 2020, 34(05): 1001-1014.
测点 编号 | wB/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Pb | 207Pb/206Pb±1σ | 207Pb/235U±1σ | 206Pb/238U±1σ | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||
GL-1 (古罗 岩体) | 1 | 391 | 330 | 39 | 1.19 | 0.048 93±0.001 39 | 0.174 53±0.004 65 | 0.025 87±0.000 21 | 144±47 | 163±4 | 165±1 | |||
2 | 302 | 255 | 32 | 1.19 | 0.048 83±0.004 19 | 0.186 24±0.015 75 | 0.027 66±0.000 39 | 140±163 | 173±13 | 176±2 | ||||
3 | 340 | 417 | 48 | 0.82 | 0.048 81±0.001 43 | 0.173 98±0.004 80 | 0.025 85±0.000 21 | 139±49 | 163±4 | 165±1 | ||||
4 | 268 | 220 | 26 | 1.22 | 0.049 06±0.002 78 | 0.175 13±0.009 70 | 0.025 89±0.000 28 | 151±106 | 164±8 | 165±2 | ||||
5 | 631 | 524 | 63 | 1.21 | 0.049 50±0.001 90 | 0.176 35±0.006 51 | 0.025 84±0.000 24 | 172±69 | 165±6 | 164±2 | ||||
6 | 1 028 | 761 | 92 | 1.35 | 0.048 96±0.001 02 | 0.174 58±0.003 27 | 0.025 86±0.000 18 | 146±31 | 163±3 | 165±1 | ||||
7 | 1 004 | 659 | 77 | 1.52 | 0.050 31±0.002 58 | 0.174 69±0.008 73 | 0.025 18±0.000 27 | 209±96 | 163±8 | 160±2 | ||||
8 | 116 | 154 | 17 | 0.75 | 0.050 60±0.004 06 | 0.177 25±0.013 92 | 0.025 41±0.000 42 | 223±147 | 166±12 | 162±3 | ||||
9 | 560 | 465 | 55 | 1.20 | 0.049 16±0.001 34 | 0.173 67±0.004 44 | 0.025 62±0.000 20 | 155±45 | 163±4 | 163±1 | ||||
10 | 352 | 344 | 40 | 1.02 | 0.050 13±0.001 41 | 0.177 66±0.004 69 | 0.025 71±0.000 20 | 201±47 | 166±4 | 164±1 | ||||
11 | 1 067 | 691 | 82 | 1.55 | 0.049 08±0.001 17 | 0.171 59±0.003 77 | 0.025 36±0.000 19 | 152±37 | 161±3 | 161±1 | ||||
12 | 752 | 516 | 63 | 1.46 | 0.049 96±0.001 30 | 0.176 85±0.004 29 | 0.025 67±0.000 20 | 193±42 | 165±4 | 163±1 | ||||
13 | 331 | 381 | 43 | 0.87 | 0.049 83±0.002 54 | 0.174 85±0.008 68 | 0.025 45±0.000 26 | 187±96 | 164±8 | 162±2 | ||||
14 | 1 069 | 921 | 107 | 1.16 | 0.049 04±0.001 02 | 0.172 35±0.003 22 | 0.025 49±0.000 18 | 150±30 | 161±3 | 162±1 | ||||
15 | 375 | 298 | 36 | 1.26 | 0.048 97±0.002 80 | 0.173 81±0.009 74 | 0.025 74±0.000 28 | 146±107 | 163±8 | 164±2 | ||||
16 | 448 | 298 | 35 | 1.50 | 0.050 10±0.003 89 | 0.175 05±0.013 31 | 0.025 35±0.000 38 | 200±144 | 164±12 | 161±2 | ||||
17 | 194 | 261 | 31 | 0.74 | 0.049 44±0.002 43 | 0.180 53±0.008 61 | 0.026 49±0.000 30 | 169±90 | 169±7 | 169±2 | ||||
18 | 804 | 594 | 72 | 1.35 | 0.050 15±0.001 68 | 0.177 18±0.005 68 | 0.025 63±0.000 22 | 202±58 | 166±5 | 163±1 | ||||
19 | 59 | 87 | 10 | 0.68 | 0.052 44±0.129 43 | 0.182 72±0.449 77 | 0.025 28±0.004 79 | 305±2 844 | 170±386 | 161±30 | ||||
20 | 836 | 624 | 76 | 1.34 | 0.048 59±0.001 14 | 0.172 27±0.003 74 | 0.025 72±0.000 19 | 128±37 | 161±3 | 164±1 | ||||
21 | 515 | 453 | 55 | 1.14 | 0.049 49±0.001 41 | 0.177 16±0.004 76 | 0.025 97±0.000 20 | 171±48 | 166±4 | 165±1 | ||||
22 | 955 | 798 | 97 | 1.20 | 0.048 90±0.000 93 | 0.174 92±0.002 95 | 0.025 95±0.000 18 | 143±27 | 164±3 | 165±1 | ||||
23 | 1 188 | 670 | 83 | 1.77 | 0.049 31±0.002 15 | 0.172 27±0.007 30 | 0.025 34±0.000 24 | 163±81 | 161±6 | 161±2 | ||||
24 | 535 | 548 | 65 | 0.98 | 0.050 08±0.001 58 | 0.175 78±0.005 30 | 0.025 46±0.000 20 | 199±55 | 164±5 | 162±1 | ||||
25 | 1 158 | 741 | 89 | 1.56 | 0.050 30±0.002 61 | 0.175 97±0.008 90 | 0.025 38±0.000 27 | 209±98 | 165±8 | 162±2 | ||||
26 | 214 | 233 | 28 | 0.92 | 0.048 59±0.002 04 | 0.174 18±0.007 06 | 0.026 01±0.000 25 | 128±76 | 163±6 | 166±2 | ||||
27 | 246 | 328 | 38 | 0.75 | 0.049 92±0.001 36 | 0.177 17±0.004 53 | 0.025 75±0.000 21 | 191±44 | 166±4 | 164±1 | ||||
28 | 324 | 329 | 40 | 0.99 | 0.048 86±0.001 25 | 0.175 47±0.004 18 | 0.026 05±0.000 20 | 141±41 | 164±4 | 166±1 | ||||
29 | 626 | 554 | 67 | 1.13 | 0.048 81±0.001 07 | 0.173 51±0.003 48 | 0.025 79±0.000 18 | 139±34 | 162±3 | 164±1 | ||||
30 | 625 | 454 | 56 | 1.38 | 0.048 95±0.001 39 | 0.175 75±0.004 72 | 0.026 05±0.000 22 | 145±47 | 164±4 | 166±1 | ||||
WJC-2 (王姜 冲岩体) | 1 | 658 | 468 | 45 | 0.71 | 0.048 70±0.001 10 | 0.166 15±0.003 46 | 0.024 76±0.000 18 | 133±35 | 156±3 | 158±1 | |||
2 | 286 | 275 | 28 | 0.96 | 0.048 51±0.002 87 | 0.170 88±0.009 89 | 0.025 56±0.000 31 | 124±107 | 160±9 | 163±2 | ||||
3 | 961 | 533 | 51 | 0.55 | 0.050 03±0.001 10 | 0.169 09±0.003 39 | 0.024 53±0.000 18 | 196±33 | 159±3 | 156±1 | ||||
4 | 1 482 | 927 | 89 | 0.63 | 0.050 04±0.000 93 | 0.169 00±0.002 79 | 0.024 51±0.000 17 | 197±25 | 159±2 | 156±1 | ||||
5 | 1 338 | 783 | 76 | 0.58 | 0.048 56±0.001 02 | 0.165 08±0.003 14 | 0.024 67±0.000 17 | 127±32 | 155±3 | 157±1 | ||||
6 | 273 | 228 | 22 | 0.83 | 0.048 46±0.002 48 | 0.168 43±0.008 40 | 0.025 22±0.000 26 | 122±93 | 158±7 | 161±2 | ||||
7 | 1 117 | 680 | 66 | 0.61 | 0.049 76±0.001 10 | 0.171 53±0.003 45 | 0.025 01±0.000 18 | 184±33 | 161±3 | 159±1 | ||||
8 | 297 | 331 | 32 | 1.11 | 0.049 24±0.002 06 | 0.168 30±0.006 80 | 0.024 79±0.000 25 | 159±75 | 158±6 | 158±2 | ||||
9 | 245 | 220 | 21 | 0.90 | 0.049 16±0.003 44 | 0.166 86±0.011 44 | 0.024 63±0.000 34 | 155±129 | 157±10 | 157±2 | ||||
10 | 961 | 624 | 60 | 0.65 | 0.049 21±0.001 13 | 0.167 64±0.003 52 | 0.024 71±0.000 18 | 158±35 | 157±3 | 157±1 | ||||
11 | 959 | 524 | 50 | 0.55 | 0.049 91±0.001 26 | 0.168 86±0.003 97 | 0.024 54±0.000 19 | 191±40 | 158±3 | 156±1 | ||||
12 | 279 | 211 | 20 | 0.76 | 0.049 09±0.001 63 | 0.167 44±0.005 31 | 0.024 74±0.000 21 | 152±58 | 157±5 | 158±1 | ||||
13 | 270 | 238 | 23 | 0.88 | 0.049 55±0.003 07 | 0.171 22±0.010 38 | 0.025 07±0.000 30 | 174±116 | 160±9 | 160±2 | ||||
测点 编号 | wB/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||||||
Th | U | Pb | 207Pb/206Pb±1σ | 207Pb/235U±1σ | 206Pb/238U±1σ | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||
WJC-2 (王姜 冲岩体) | 14 | 1 378 | 785 | 76 | 0.57 | 0.049 43±0.001 34 | 0.169 32±0.004 29 | 0.024 85±0.000 20 | 168±44 | 159±4 | 158±1 | |||
16 | 313 | 286 | 28 | 0.91 | 0.049 28±0.002 67 | 0.171 07±0.008 98 | 0.025 18±0.000 31 | 161±97 | 160±8 | 160±2 | ||||
17 | 967 | 738 | 71 | 0.76 | 0.048 87±0.000 97 | 0.166 49±0.002 96 | 0.024 71±0.000 17 | 142±29 | 156±3 | 157±1 | ||||
18 | 1 695 | 1 095 | 106 | 0.65 | 0.049 43±0.000 83 | 0.170 12±0.002 45 | 0.024 96±0.000 16 | 168±22 | 160±2 | 159±1 | ||||
19 | 163 | 300 | 29 | 1.83 | 0.048 87±0.003 67 | 0.170 76±0.012 55 | 0.025 34±0.000 38 | 142±137 | 160±11 | 161±2 | ||||
20 | 517 | 508 | 52 | 0.98 | 0.051 21±0.006 10 | 0.184 67±0.021 59 | 0.026 15±0.000 62 | 250±220 | 172±19 | 166±4 | ||||
21 | 352 | 347 | 33 | 0.99 | 0.049 72±0.002 00 | 0.169 44±0.006 56 | 0.024 71±0.000 25 | 182±71 | 159±6 | 157±2 | ||||
22 | 322 | 328 | 32 | 1.02 | 0.049 82±0.002 17 | 0.172 48±0.007 24 | 0.025 11±0.000 27 | 187±78 | 162±6 | 160±2 | ||||
23 | 265 | 293 | 30 | 1.11 | 0.048 81±0.003 22 | 0.176 61±0.011 41 | 0.026 24±0.000 32 | 139±123 | 165±10 | 167±2 | ||||
24 | 240 | 283 | 28 | 1.18 | 0.049 49±0.003 92 | 0.172 08±0.013 35 | 0.025 22±0.000 39 | 171±146 | 161±12 | 161±2 | ||||
25 | 459 | 422 | 41 | 0.92 | 0.049 66±0.001 62 | 0.171 32±0.005 35 | 0.025 02±0.000 20 | 179±58 | 161±5 | 159±1 | ||||
26 | 353 | 306 | 30 | 0.87 | 0.049 23±0.001 34 | 0.172 39±0.004 40 | 0.025 40±0.000 20 | 159±45 | 161±4 | 162±1 | ||||
27 | 891 | 653 | 63 | 0.73 | 0.049 38±0.000 96 | 0.169 29±0.002 92 | 0.024 86±0.000 17 | 166±27 | 159±3 | 158±1 | ||||
28 | 605 | 440 | 41 | 0.73 | 0.049 93±0.001 19 | 0.168 65±0.003 07 | 0.024 50±0.000 18 | 192±37 | 158±3 | 156±1 | ||||
29 | 222 | 234 | 23 | 1.05 | 0.049 52±0.002 89 | 0.172 50±0.009 78 | 0.025 26±0.000 33 | 173±105 | 162±8 | 161±2 | ||||
30 | 441 | 468 | 45 | 1.06 | 0.049 13±0.001 10 | 0.169 53±0.003 45 | 0.025 03±0.000 18 | 154±34 | 159±3 | 159±1 |
Table 1 LA-ICP-MS zircon U-Pb data of the Guluo and Wangjiangchong gabbros
测点 编号 | wB/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Pb | 207Pb/206Pb±1σ | 207Pb/235U±1σ | 206Pb/238U±1σ | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||
GL-1 (古罗 岩体) | 1 | 391 | 330 | 39 | 1.19 | 0.048 93±0.001 39 | 0.174 53±0.004 65 | 0.025 87±0.000 21 | 144±47 | 163±4 | 165±1 | |||
2 | 302 | 255 | 32 | 1.19 | 0.048 83±0.004 19 | 0.186 24±0.015 75 | 0.027 66±0.000 39 | 140±163 | 173±13 | 176±2 | ||||
3 | 340 | 417 | 48 | 0.82 | 0.048 81±0.001 43 | 0.173 98±0.004 80 | 0.025 85±0.000 21 | 139±49 | 163±4 | 165±1 | ||||
4 | 268 | 220 | 26 | 1.22 | 0.049 06±0.002 78 | 0.175 13±0.009 70 | 0.025 89±0.000 28 | 151±106 | 164±8 | 165±2 | ||||
5 | 631 | 524 | 63 | 1.21 | 0.049 50±0.001 90 | 0.176 35±0.006 51 | 0.025 84±0.000 24 | 172±69 | 165±6 | 164±2 | ||||
6 | 1 028 | 761 | 92 | 1.35 | 0.048 96±0.001 02 | 0.174 58±0.003 27 | 0.025 86±0.000 18 | 146±31 | 163±3 | 165±1 | ||||
7 | 1 004 | 659 | 77 | 1.52 | 0.050 31±0.002 58 | 0.174 69±0.008 73 | 0.025 18±0.000 27 | 209±96 | 163±8 | 160±2 | ||||
8 | 116 | 154 | 17 | 0.75 | 0.050 60±0.004 06 | 0.177 25±0.013 92 | 0.025 41±0.000 42 | 223±147 | 166±12 | 162±3 | ||||
9 | 560 | 465 | 55 | 1.20 | 0.049 16±0.001 34 | 0.173 67±0.004 44 | 0.025 62±0.000 20 | 155±45 | 163±4 | 163±1 | ||||
10 | 352 | 344 | 40 | 1.02 | 0.050 13±0.001 41 | 0.177 66±0.004 69 | 0.025 71±0.000 20 | 201±47 | 166±4 | 164±1 | ||||
11 | 1 067 | 691 | 82 | 1.55 | 0.049 08±0.001 17 | 0.171 59±0.003 77 | 0.025 36±0.000 19 | 152±37 | 161±3 | 161±1 | ||||
12 | 752 | 516 | 63 | 1.46 | 0.049 96±0.001 30 | 0.176 85±0.004 29 | 0.025 67±0.000 20 | 193±42 | 165±4 | 163±1 | ||||
13 | 331 | 381 | 43 | 0.87 | 0.049 83±0.002 54 | 0.174 85±0.008 68 | 0.025 45±0.000 26 | 187±96 | 164±8 | 162±2 | ||||
14 | 1 069 | 921 | 107 | 1.16 | 0.049 04±0.001 02 | 0.172 35±0.003 22 | 0.025 49±0.000 18 | 150±30 | 161±3 | 162±1 | ||||
15 | 375 | 298 | 36 | 1.26 | 0.048 97±0.002 80 | 0.173 81±0.009 74 | 0.025 74±0.000 28 | 146±107 | 163±8 | 164±2 | ||||
16 | 448 | 298 | 35 | 1.50 | 0.050 10±0.003 89 | 0.175 05±0.013 31 | 0.025 35±0.000 38 | 200±144 | 164±12 | 161±2 | ||||
17 | 194 | 261 | 31 | 0.74 | 0.049 44±0.002 43 | 0.180 53±0.008 61 | 0.026 49±0.000 30 | 169±90 | 169±7 | 169±2 | ||||
18 | 804 | 594 | 72 | 1.35 | 0.050 15±0.001 68 | 0.177 18±0.005 68 | 0.025 63±0.000 22 | 202±58 | 166±5 | 163±1 | ||||
19 | 59 | 87 | 10 | 0.68 | 0.052 44±0.129 43 | 0.182 72±0.449 77 | 0.025 28±0.004 79 | 305±2 844 | 170±386 | 161±30 | ||||
20 | 836 | 624 | 76 | 1.34 | 0.048 59±0.001 14 | 0.172 27±0.003 74 | 0.025 72±0.000 19 | 128±37 | 161±3 | 164±1 | ||||
21 | 515 | 453 | 55 | 1.14 | 0.049 49±0.001 41 | 0.177 16±0.004 76 | 0.025 97±0.000 20 | 171±48 | 166±4 | 165±1 | ||||
22 | 955 | 798 | 97 | 1.20 | 0.048 90±0.000 93 | 0.174 92±0.002 95 | 0.025 95±0.000 18 | 143±27 | 164±3 | 165±1 | ||||
23 | 1 188 | 670 | 83 | 1.77 | 0.049 31±0.002 15 | 0.172 27±0.007 30 | 0.025 34±0.000 24 | 163±81 | 161±6 | 161±2 | ||||
24 | 535 | 548 | 65 | 0.98 | 0.050 08±0.001 58 | 0.175 78±0.005 30 | 0.025 46±0.000 20 | 199±55 | 164±5 | 162±1 | ||||
25 | 1 158 | 741 | 89 | 1.56 | 0.050 30±0.002 61 | 0.175 97±0.008 90 | 0.025 38±0.000 27 | 209±98 | 165±8 | 162±2 | ||||
26 | 214 | 233 | 28 | 0.92 | 0.048 59±0.002 04 | 0.174 18±0.007 06 | 0.026 01±0.000 25 | 128±76 | 163±6 | 166±2 | ||||
27 | 246 | 328 | 38 | 0.75 | 0.049 92±0.001 36 | 0.177 17±0.004 53 | 0.025 75±0.000 21 | 191±44 | 166±4 | 164±1 | ||||
28 | 324 | 329 | 40 | 0.99 | 0.048 86±0.001 25 | 0.175 47±0.004 18 | 0.026 05±0.000 20 | 141±41 | 164±4 | 166±1 | ||||
29 | 626 | 554 | 67 | 1.13 | 0.048 81±0.001 07 | 0.173 51±0.003 48 | 0.025 79±0.000 18 | 139±34 | 162±3 | 164±1 | ||||
30 | 625 | 454 | 56 | 1.38 | 0.048 95±0.001 39 | 0.175 75±0.004 72 | 0.026 05±0.000 22 | 145±47 | 164±4 | 166±1 | ||||
WJC-2 (王姜 冲岩体) | 1 | 658 | 468 | 45 | 0.71 | 0.048 70±0.001 10 | 0.166 15±0.003 46 | 0.024 76±0.000 18 | 133±35 | 156±3 | 158±1 | |||
2 | 286 | 275 | 28 | 0.96 | 0.048 51±0.002 87 | 0.170 88±0.009 89 | 0.025 56±0.000 31 | 124±107 | 160±9 | 163±2 | ||||
3 | 961 | 533 | 51 | 0.55 | 0.050 03±0.001 10 | 0.169 09±0.003 39 | 0.024 53±0.000 18 | 196±33 | 159±3 | 156±1 | ||||
4 | 1 482 | 927 | 89 | 0.63 | 0.050 04±0.000 93 | 0.169 00±0.002 79 | 0.024 51±0.000 17 | 197±25 | 159±2 | 156±1 | ||||
5 | 1 338 | 783 | 76 | 0.58 | 0.048 56±0.001 02 | 0.165 08±0.003 14 | 0.024 67±0.000 17 | 127±32 | 155±3 | 157±1 | ||||
6 | 273 | 228 | 22 | 0.83 | 0.048 46±0.002 48 | 0.168 43±0.008 40 | 0.025 22±0.000 26 | 122±93 | 158±7 | 161±2 | ||||
7 | 1 117 | 680 | 66 | 0.61 | 0.049 76±0.001 10 | 0.171 53±0.003 45 | 0.025 01±0.000 18 | 184±33 | 161±3 | 159±1 | ||||
8 | 297 | 331 | 32 | 1.11 | 0.049 24±0.002 06 | 0.168 30±0.006 80 | 0.024 79±0.000 25 | 159±75 | 158±6 | 158±2 | ||||
9 | 245 | 220 | 21 | 0.90 | 0.049 16±0.003 44 | 0.166 86±0.011 44 | 0.024 63±0.000 34 | 155±129 | 157±10 | 157±2 | ||||
10 | 961 | 624 | 60 | 0.65 | 0.049 21±0.001 13 | 0.167 64±0.003 52 | 0.024 71±0.000 18 | 158±35 | 157±3 | 157±1 | ||||
11 | 959 | 524 | 50 | 0.55 | 0.049 91±0.001 26 | 0.168 86±0.003 97 | 0.024 54±0.000 19 | 191±40 | 158±3 | 156±1 | ||||
12 | 279 | 211 | 20 | 0.76 | 0.049 09±0.001 63 | 0.167 44±0.005 31 | 0.024 74±0.000 21 | 152±58 | 157±5 | 158±1 | ||||
13 | 270 | 238 | 23 | 0.88 | 0.049 55±0.003 07 | 0.171 22±0.010 38 | 0.025 07±0.000 30 | 174±116 | 160±9 | 160±2 | ||||
测点 编号 | wB/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||||||
Th | U | Pb | 207Pb/206Pb±1σ | 207Pb/235U±1σ | 206Pb/238U±1σ | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||
WJC-2 (王姜 冲岩体) | 14 | 1 378 | 785 | 76 | 0.57 | 0.049 43±0.001 34 | 0.169 32±0.004 29 | 0.024 85±0.000 20 | 168±44 | 159±4 | 158±1 | |||
16 | 313 | 286 | 28 | 0.91 | 0.049 28±0.002 67 | 0.171 07±0.008 98 | 0.025 18±0.000 31 | 161±97 | 160±8 | 160±2 | ||||
17 | 967 | 738 | 71 | 0.76 | 0.048 87±0.000 97 | 0.166 49±0.002 96 | 0.024 71±0.000 17 | 142±29 | 156±3 | 157±1 | ||||
18 | 1 695 | 1 095 | 106 | 0.65 | 0.049 43±0.000 83 | 0.170 12±0.002 45 | 0.024 96±0.000 16 | 168±22 | 160±2 | 159±1 | ||||
19 | 163 | 300 | 29 | 1.83 | 0.048 87±0.003 67 | 0.170 76±0.012 55 | 0.025 34±0.000 38 | 142±137 | 160±11 | 161±2 | ||||
20 | 517 | 508 | 52 | 0.98 | 0.051 21±0.006 10 | 0.184 67±0.021 59 | 0.026 15±0.000 62 | 250±220 | 172±19 | 166±4 | ||||
21 | 352 | 347 | 33 | 0.99 | 0.049 72±0.002 00 | 0.169 44±0.006 56 | 0.024 71±0.000 25 | 182±71 | 159±6 | 157±2 | ||||
22 | 322 | 328 | 32 | 1.02 | 0.049 82±0.002 17 | 0.172 48±0.007 24 | 0.025 11±0.000 27 | 187±78 | 162±6 | 160±2 | ||||
23 | 265 | 293 | 30 | 1.11 | 0.048 81±0.003 22 | 0.176 61±0.011 41 | 0.026 24±0.000 32 | 139±123 | 165±10 | 167±2 | ||||
24 | 240 | 283 | 28 | 1.18 | 0.049 49±0.003 92 | 0.172 08±0.013 35 | 0.025 22±0.000 39 | 171±146 | 161±12 | 161±2 | ||||
25 | 459 | 422 | 41 | 0.92 | 0.049 66±0.001 62 | 0.171 32±0.005 35 | 0.025 02±0.000 20 | 179±58 | 161±5 | 159±1 | ||||
26 | 353 | 306 | 30 | 0.87 | 0.049 23±0.001 34 | 0.172 39±0.004 40 | 0.025 40±0.000 20 | 159±45 | 161±4 | 162±1 | ||||
27 | 891 | 653 | 63 | 0.73 | 0.049 38±0.000 96 | 0.169 29±0.002 92 | 0.024 86±0.000 17 | 166±27 | 159±3 | 158±1 | ||||
28 | 605 | 440 | 41 | 0.73 | 0.049 93±0.001 19 | 0.168 65±0.003 07 | 0.024 50±0.000 18 | 192±37 | 158±3 | 156±1 | ||||
29 | 222 | 234 | 23 | 1.05 | 0.049 52±0.002 89 | 0.172 50±0.009 78 | 0.025 26±0.000 33 | 173±105 | 162±8 | 161±2 | ||||
30 | 441 | 468 | 45 | 1.06 | 0.049 13±0.001 10 | 0.169 53±0.003 45 | 0.025 03±0.000 18 | 154±34 | 159±3 | 159±1 |
样品编号 | SiO2 | Al2O3 | Fe2O3 | FeO | CaO | MgO | Na2O | K2O | TiO2 | MnO | P2O5 | SrO | BaO | 烧失量 | 总量 | |||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
GL-1 | 40.60 | 10.80 | 19.68 | — | 10.05 | 9.42 | 2.00 | 1.41 | 3.65 | 0.23 | 0.35 | 0.07 | 0.01 | 1.69 | 101.39 | |||||||||||||||||||||
GL-2 | 47.56 | 15.95 | 4.72 | 8.13 | 6.91 | 5.67 | 2.70 | 2.04 | 2.28 | 0.18 | 1.02 | — | — | 2.42 | 99.58 | |||||||||||||||||||||
GL-3 | 46.86 | 20.15 | 3.18 | 7.15 | 8.50 | 2.26 | 3.54 | 1.72 | 1.84 | 0.16 | 1.13 | — | — | 3.21 | 99.70 | |||||||||||||||||||||
WJC-1 | 46.90 | 15.25 | 13.36 | — | 8.78 | 5.49 | 2.98 | 1.78 | 2.60 | 0.21 | 0.81 | 0.07 | 0.01 | 1.67 | 101.13 | |||||||||||||||||||||
WJC-3 | 45.86 | 16.17 | 3.12 | 10.87 | 7.90 | 4.55 | 2.73 | 2.05 | 2.51 | 0.17 | 0.88 | — | — | 2.42 | 99.23 | |||||||||||||||||||||
样品编号 | A/CNK | K/Na | ALK | Mg# | Li | Be | Sc | V | Cr | Co | Ni | Cu | Zn | Ga | Rb | |||||||||||||||||||||
GL-1 | 0.47 | 0.71 | 3.41 | 48.92 | 6.10 | 1.02 | 51.8 | 602 | 66.0 | 74.6 | 55.9 | 140.5 | 143 | 20.6 | 34.1 | |||||||||||||||||||||
GL-2 | 0.83 | 0.76 | 4.74 | 55.66 | 17.90 | 1.95 | 34.3 | 339 | 41.4 | 39.1 | 14.9 | 36.5 | 111 | 26.5 | 99.6 | |||||||||||||||||||||
GL-3 | 0.87 | 0.49 | 5.26 | 36.26 | 12.20 | 2.04 | 11.6 | 257 | 37.0 | 26.1 | 11.6 | 86.3 | 87 | 26.6 | 78.8 | |||||||||||||||||||||
WJC-1 | 0.67 | 0.60 | 4.76 | 45.12 | 7.50 | 1.47 | 28.6 | 281 | 31.0 | 38.5 | 21.0 | 131.5 | 117 | 23.4 | 58.1 | |||||||||||||||||||||
WJC-3 | 0.77 | 0.75 | 4.78 | 42.97 | 13.80 | 1.77 | 25.3 | 424 | 110.0 | 55.4 | 38.2 | 172.4 | 123 | 27.8 | 74.9 | |||||||||||||||||||||
样品编号 | Sr | Zr | Nb | Cs | Ba | Hf | Ta | Pb | Th | U | La | Ce | Pr | Nd | Sm | Eu | ||||||||||||||||||||
GL-1 | 518 | 90.7 | 43.6 | 0.94 | 420 | 3.40 | 2.66 | 3.30 | 3.20 | 0.70 | 35.0 | 79.2 | 10.5 | 42.4 | 8.35 | 2.81 | ||||||||||||||||||||
GL-2 | 703 | 192.0 | 41.7 | — | 857 | 5.36 | 3.23 | 6.81 | 6.83 | 1.44 | 51.4 | 104.0 | 13.5 | 55.1 | 11.00 | 3.05 | ||||||||||||||||||||
GL-3 | 1 034 | 201.0 | 36.5 | — | 527 | 8.62 | 2.37 | 12.20 | 6.51 | 1.50 | 49.7 | 97.7 | 12.8 | 51.6 | 9.00 | 2.47 | ||||||||||||||||||||
WJC-1 | 985 | 87.8 | 59.1 | 3.15 | 580 | 3.70 | 3.19 | 5.00 | 5.50 | 1.20 | 61.9 | 133.5 | 17.2 | 67.2 | 12.25 | 3.85 | ||||||||||||||||||||
WJC-3 | 862 | 267.0 | 46.5 | — | 793 | 6.78 | 3.35 | 6.26 | 6.27 | 1.67 | 51.4 | 101.0 | 12.2 | 47.5 | 8.83 | 2.50 | ||||||||||||||||||||
样品编号 | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Y | ΣREE | LREE | L/H | (La/Yb)N | δEu | δCe | |||||||||||||||||||||
GL-1 | 8.22 | 1.18 | 6.39 | 1.24 | 3.39 | 0.41 | 2.52 | 0.36 | 33.1 | 201.97 | 178.26 | 7.52 | 9.96 | 1.02 | 1.00 | |||||||||||||||||||||
GL-2 | 10.16 | 1.38 | 7.56 | 1.41 | 3.89 | 0.54 | 3.31 | 0.48 | 37.4 | 266.78 | 238.05 | 8.29 | 11.14 | 0.87 | 0.95 | |||||||||||||||||||||
GL-3 | 7.72 | 1.06 | 5.82 | 1.04 | 2.80 | 0.38 | 2.38 | 0.34 | 27.4 | 244.81 | 223.27 | 10.37 | 14.98 | 0.88 | 0.93 | |||||||||||||||||||||
WJC-1 | 11.00 | 1.58 | 8.40 | 1.61 | 4.47 | 0.56 | 3.44 | 0.50 | 45.7 | 327.46 | 295.90 | 9.38 | 12.91 | 0.99 | 0.99 | |||||||||||||||||||||
WJC-3 | 7.88 | 1.03 | 5.69 | 1.05 | 2.83 | 0.40 | 2.47 | 0.37 | 27.6 | 245.15 | 223.43 | 10.29 | 14.93 | 0.90 | 0.96 |
Table 2 Major (%), trace element (10-6) and REE (10-6) contents of the Guluo and Wangjiangchong gabbro samples
样品编号 | SiO2 | Al2O3 | Fe2O3 | FeO | CaO | MgO | Na2O | K2O | TiO2 | MnO | P2O5 | SrO | BaO | 烧失量 | 总量 | |||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
GL-1 | 40.60 | 10.80 | 19.68 | — | 10.05 | 9.42 | 2.00 | 1.41 | 3.65 | 0.23 | 0.35 | 0.07 | 0.01 | 1.69 | 101.39 | |||||||||||||||||||||
GL-2 | 47.56 | 15.95 | 4.72 | 8.13 | 6.91 | 5.67 | 2.70 | 2.04 | 2.28 | 0.18 | 1.02 | — | — | 2.42 | 99.58 | |||||||||||||||||||||
GL-3 | 46.86 | 20.15 | 3.18 | 7.15 | 8.50 | 2.26 | 3.54 | 1.72 | 1.84 | 0.16 | 1.13 | — | — | 3.21 | 99.70 | |||||||||||||||||||||
WJC-1 | 46.90 | 15.25 | 13.36 | — | 8.78 | 5.49 | 2.98 | 1.78 | 2.60 | 0.21 | 0.81 | 0.07 | 0.01 | 1.67 | 101.13 | |||||||||||||||||||||
WJC-3 | 45.86 | 16.17 | 3.12 | 10.87 | 7.90 | 4.55 | 2.73 | 2.05 | 2.51 | 0.17 | 0.88 | — | — | 2.42 | 99.23 | |||||||||||||||||||||
样品编号 | A/CNK | K/Na | ALK | Mg# | Li | Be | Sc | V | Cr | Co | Ni | Cu | Zn | Ga | Rb | |||||||||||||||||||||
GL-1 | 0.47 | 0.71 | 3.41 | 48.92 | 6.10 | 1.02 | 51.8 | 602 | 66.0 | 74.6 | 55.9 | 140.5 | 143 | 20.6 | 34.1 | |||||||||||||||||||||
GL-2 | 0.83 | 0.76 | 4.74 | 55.66 | 17.90 | 1.95 | 34.3 | 339 | 41.4 | 39.1 | 14.9 | 36.5 | 111 | 26.5 | 99.6 | |||||||||||||||||||||
GL-3 | 0.87 | 0.49 | 5.26 | 36.26 | 12.20 | 2.04 | 11.6 | 257 | 37.0 | 26.1 | 11.6 | 86.3 | 87 | 26.6 | 78.8 | |||||||||||||||||||||
WJC-1 | 0.67 | 0.60 | 4.76 | 45.12 | 7.50 | 1.47 | 28.6 | 281 | 31.0 | 38.5 | 21.0 | 131.5 | 117 | 23.4 | 58.1 | |||||||||||||||||||||
WJC-3 | 0.77 | 0.75 | 4.78 | 42.97 | 13.80 | 1.77 | 25.3 | 424 | 110.0 | 55.4 | 38.2 | 172.4 | 123 | 27.8 | 74.9 | |||||||||||||||||||||
样品编号 | Sr | Zr | Nb | Cs | Ba | Hf | Ta | Pb | Th | U | La | Ce | Pr | Nd | Sm | Eu | ||||||||||||||||||||
GL-1 | 518 | 90.7 | 43.6 | 0.94 | 420 | 3.40 | 2.66 | 3.30 | 3.20 | 0.70 | 35.0 | 79.2 | 10.5 | 42.4 | 8.35 | 2.81 | ||||||||||||||||||||
GL-2 | 703 | 192.0 | 41.7 | — | 857 | 5.36 | 3.23 | 6.81 | 6.83 | 1.44 | 51.4 | 104.0 | 13.5 | 55.1 | 11.00 | 3.05 | ||||||||||||||||||||
GL-3 | 1 034 | 201.0 | 36.5 | — | 527 | 8.62 | 2.37 | 12.20 | 6.51 | 1.50 | 49.7 | 97.7 | 12.8 | 51.6 | 9.00 | 2.47 | ||||||||||||||||||||
WJC-1 | 985 | 87.8 | 59.1 | 3.15 | 580 | 3.70 | 3.19 | 5.00 | 5.50 | 1.20 | 61.9 | 133.5 | 17.2 | 67.2 | 12.25 | 3.85 | ||||||||||||||||||||
WJC-3 | 862 | 267.0 | 46.5 | — | 793 | 6.78 | 3.35 | 6.26 | 6.27 | 1.67 | 51.4 | 101.0 | 12.2 | 47.5 | 8.83 | 2.50 | ||||||||||||||||||||
样品编号 | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Y | ΣREE | LREE | L/H | (La/Yb)N | δEu | δCe | |||||||||||||||||||||
GL-1 | 8.22 | 1.18 | 6.39 | 1.24 | 3.39 | 0.41 | 2.52 | 0.36 | 33.1 | 201.97 | 178.26 | 7.52 | 9.96 | 1.02 | 1.00 | |||||||||||||||||||||
GL-2 | 10.16 | 1.38 | 7.56 | 1.41 | 3.89 | 0.54 | 3.31 | 0.48 | 37.4 | 266.78 | 238.05 | 8.29 | 11.14 | 0.87 | 0.95 | |||||||||||||||||||||
GL-3 | 7.72 | 1.06 | 5.82 | 1.04 | 2.80 | 0.38 | 2.38 | 0.34 | 27.4 | 244.81 | 223.27 | 10.37 | 14.98 | 0.88 | 0.93 | |||||||||||||||||||||
WJC-1 | 11.00 | 1.58 | 8.40 | 1.61 | 4.47 | 0.56 | 3.44 | 0.50 | 45.7 | 327.46 | 295.90 | 9.38 | 12.91 | 0.99 | 0.99 | |||||||||||||||||||||
WJC-3 | 7.88 | 1.03 | 5.69 | 1.05 | 2.83 | 0.40 | 2.47 | 0.37 | 27.6 | 245.15 | 223.43 | 10.29 | 14.93 | 0.90 | 0.96 |
Fig.6 Chondrite-normalized REE patterns ((a),base map after reference [31]) and primitive-mantle-normalized multi-element spidergram for gabbro samples ((b),base map after reference[31])
样品及 分析点号 | 年龄/Ma | 176Yb/ 177Hf | 176Lu/ 177Hf | 176Hf/177Hf±2σ | TDM /Ma | /Ma | εHf(0) | εHf(t) | ||
---|---|---|---|---|---|---|---|---|---|---|
GL-1 (古罗岩体) | 1 | 165 | 0.090 269 | 0.001 619 | 0.282 756±0.000 027 | 714 | 1 028 | -0.55 | 2.9 | -0.96 |
2 | 176 | 0.076 848 | 0.001 362 | 0.282 822±0.000 030 | 615 | 871 | 1.77 | 5.5 | -0.95 | |
3 | 165 | 0.093 650 | 0.001 705 | 0.282 830±0.000 026 | 609 | 862 | 2.05 | 5.5 | -0.98 | |
4 | 165 | 0.030 093 | 0.000 560 | 0.282 723±0.000 027 | 741 | 1 097 | -1.74 | 1.8 | -0.96 | |
5 | 164 | 0.071 446 | 0.001 235 | 0.282 817±0.000 025 | 620 | 889 | 1.59 | 5.1 | -0.93 | |
6 | 165 | 0.132 881 | 0.002 177 | 0.282 841±0.000 030 | 601 | 840 | 2.44 | 5.8 | -0.95 | |
7 | 160 | 0.094 543 | 0.001 611 | 0.282 837±0.000 023 | 597 | 848 | 2.31 | 5.7 | -0.96 | |
8 | 162 | 0.079 647 | 0.001 325 | 0.282 821±0.000 026 | 617 | 882 | 1.72 | 5.1 | -0.97 | |
9 | 163 | 0.060 721 | 0.001 059 | 0.282 693±0.000 026 | 793 | 1 168 | -2.78 | 0.7 | -0.95 | |
10 | 164 | 0.089 598 | 0.001 512 | 0.282 762±0.000 027 | 704 | 1 015 | -0.36 | 3.1 | -0.93 | |
11 | 161 | 0.135 710 | 0.002 228 | 0.282 873±0.000 028 | 556 | 771 | 3.56 | 6.9 | -0.95 | |
12 | 163 | 0.098 089 | 0.001 644 | 0.282 773±0.000 024 | 691 | 993 | 0.02 | 3.4 | -0.96 | |
13 | 162 | 0.072 985 | 0.001 324 | 0.282 746±0.000 022 | 723 | 1 050 | -0.91 | 2.5 | -0.94 | |
15 | 164 | 0.110 921 | 0.001 891 | 0.282 841±0.000 026 | 597 | 840 | 2.42 | 5.8 | -0.95 | |
16 | 161 | 0.090 756 | 0.001 517 | 0.282 769±0.000 027 | 694 | 1 001 | -0.11 | 3.3 | -0.97 | |
17 | 169 | 0.058 462 | 0.001 007 | 0.282 751±0.000 026 | 710 | 1 034 | -0.75 | 2.9 | -0.94 | |
18 | 163 | 0.108 347 | 0.001 835 | 0.282 893±0.000 027 | 521 | 722 | 4.27 | 7.7 | -0.96 | |
20 | 164 | 0.070 769 | 0.001 247 | 0.282 795±0.000 025 | 651 | 938 | 0.83 | 4.3 | -0.94 | |
21 | 165 | 0.114 290 | 0.001 901 | 0.282 836±0.000 024 | 604 | 850 | 2.27 | 5.7 | -0.95 | |
22 | 165 | 0.093 102 | 0.001 675 | 0.282 774±0.000 023 | 690 | 989 | 0.07 | 3.5 | -0.94 | |
23 | 161 | 0.121 754 | 0.002 080 | 0.282 777±0.000 029 | 693 | 987 | 0.18 | 3.5 | -0.93 | |
24 | 162 | 0.135 761 | 0.002 356 | 0.282 886±0.000 026 | 538 | 741 | 4.04 | 7.3 | -0.94 | |
25 | 162 | 0.106 936 | 0.001 850 | 0.282 757±0.000 029 | 718 | 1 031 | -0.55 | 2.8 | -0.98 | |
26 | 166 | 0.034 608 | 0.000 645 | 0.282 742±0.000 022 | 717 | 1 054 | -1.08 | 2.5 | -0.97 | |
27 | 164 | 0.048 099 | 0.000 851 | 0.282 717±0.000 026 | 755 | 1 113 | -1.96 | 1.6 | -0.96 | |
28 | 166 | 0.079 346 | 0.001 421 | 0.282 824±0.000 024 | 613 | 872 | 1.85 | 5.3 | -0.96 | |
29 | 164 | 0.079 920 | 0.001 368 | 0.282 821±0.000 023 | 618 | 882 | 1.72 | 5.2 | -0.94 | |
30 | 166 | 0.122 002 | 0.002 123 | 0.282 821±0.000 027 | 629 | 884 | 1.74 | 5.2 | -0.96 | |
WJC-2 (王姜 冲岩体) | 1 | 158 | 0.122 478 | 0.002 081 | 0.282 863±0.000 028 | 568 | 794 | 3.21 | 6.5 | -0.94 |
2 | 163 | 0.060 987 | 0.001 095 | 0.282 767±0.000 027 | 689 | 1 001 | -0.17 | 3.3 | -0.97 | |
3 | 156 | 0.062 784 | 0.001 091 | 0.282 756±0.000 028 | 704 | 1 030 | -0.56 | 2.8 | -0.97 | |
4 | 156 | 0.182 452 | 0.003 059 | 0.282 920±0.000 030 | 498 | 672 | 5.23 | 8.3 | -0.91 | |
5 | 157 | 0.072 200 | 0.001 255 | 0.282 796±0.000 028 | 651 | 941 | 0.85 | 4.2 | -0.96 | |
6 | 161 | 0.057 827 | 0.000 992 | 0.282 750±0.000 026 | 711 | 1 040 | -0.77 | 2.7 | -0.97 | |
7 | 159 | 0.078 144 | 0.001 339 | 0.282 747±0.000 022 | 722 | 1 050 | -0.88 | 2.5 | -0.96 | |
8 | 158 | 0.120 985 | 0.002 093 | 0.282 705±0.000 030 | 798 | 1 150 | -2.36 | 0.9 | -0.94 | |
9 | 157 | 0.097 548 | 0.001 693 | 0.282 765±0.000 026 | 703 | 1 013 | -0.23 | 3.0 | -0.95 | |
10 | 157 | 0.096 685 | 0.001 687 | 0.282 779±0.000 025 | 683 | 982 | 0.24 | 3.5 | -0.95 | |
11 | 156 | 0.123 280 | 0.002 153 | 0.282 797±0.000 028 | 665 | 944 | 0.90 | 4.1 | -0.94 | |
12 | 158 | 0.180 122 | 0.002 940 | 0.282 838±0.000 029 | 618 | 855 | 2.35 | 5.5 | -0.91 | |
13 | 160 | 0.094 577 | 0.001 638 | 0.282 774±0.000 023 | 688 | 990 | 0.09 | 3.4 | -0.95 | |
14 | 158 | 0.161 252 | 0.002 711 | 0.282 810±0.000 030 | 656 | 918 | 1.35 | 4.5 | -0.92 | |
16 | 160 | 0.070 054 | 0.001 240 | 0.282 789±0.000 025 | 661 | 955 | 0.60 | 4.0 | -0.96 | |
17 | 157 | 0.091 408 | 0.001 603 | 0.282 786±0.000 026 | 671 | 965 | 0.50 | 3.8 | -0.95 | |
样品及 分析点号 | 年龄/Ma | 176Yb/ 177Hf | 176Lu/ 177Hf | 176Hf/177Hf±2σ | TDM /Ma | /Ma | εHf(0) | εHf(t) | ||
WJC-2 (王姜 冲岩体) | 18 | 159 | 0.085 027 | 0.001 567 | 0.282 782±0.000 027 | 676 | 973 | 0.35 | 3.7 | -0.95 |
19 | 161 | 0.093 584 | 0.001 698 | 0.282 809±0.000 030 | 640 | 912 | 1.31 | 4.7 | -0.95 | |
20 | 166 | 0.093 402 | 0.001 684 | 0.282 729±0.000 025 | 755 | 1 090 | -1.52 | 1.9 | -0.95 | |
21 | 157 | 0.059 336 | 0.001 064 | 0.282 810±0.000 023 | 628 | 908 | 1.34 | 4.7 | -0.97 | |
22 | 160 | 0.102 317 | 0.001 782 | 0.282 715±0.000 028 | 777 | 1 125 | -2.01 | 1.3 | -0.95 | |
23 | 167 | 0.043 941 | 0.000 816 | 0.282 694±0.000 027 | 787 | 1 163 | -2.77 | 0.8 | -0.98 | |
24 | 161 | 0.126 266 | 0.002 223 | 0.282 853±0.000 029 | 585 | 817 | 2.85 | 6.2 | -0.93 | |
25 | 159 | 0.089 278 | 0.001 601 | 0.282 788±0.000 024 | 668 | 960 | 0.56 | 3.9 | -0.95 | |
26 | 162 | 0.091 475 | 0.001 675 | 0.282 766±0.000 027 | 701 | 1 008 | -0.20 | 3.2 | -0.95 | |
27 | 158 | 0.128 285 | 0.002 316 | 0.282 805±0.000 025 | 657 | 928 | 1.15 | 4.4 | -0.93 | |
28 | 156 | 0.079 977 | 0.001 469 | 0.282 719±0.000 026 | 765 | 1 117 | -1.88 | 1.4 | -0.96 | |
29 | 161 | 0.135 838 | 0.002 402 | 0.282 823±0.000 028 | 631 | 884 | 1.82 | 5.1 | -0.93 | |
30 | 159 | 0.128 861 | 0.002 305 | 0.282 749±0.000 030 | 738 | 1 053 | -0.82 | 2.4 | -0.93 |
Table 3 LA-MC-ICP-MS zircon Lu-Hf isotope data of gabbro samples from the Guluo and Wangjiangchong
样品及 分析点号 | 年龄/Ma | 176Yb/ 177Hf | 176Lu/ 177Hf | 176Hf/177Hf±2σ | TDM /Ma | /Ma | εHf(0) | εHf(t) | ||
---|---|---|---|---|---|---|---|---|---|---|
GL-1 (古罗岩体) | 1 | 165 | 0.090 269 | 0.001 619 | 0.282 756±0.000 027 | 714 | 1 028 | -0.55 | 2.9 | -0.96 |
2 | 176 | 0.076 848 | 0.001 362 | 0.282 822±0.000 030 | 615 | 871 | 1.77 | 5.5 | -0.95 | |
3 | 165 | 0.093 650 | 0.001 705 | 0.282 830±0.000 026 | 609 | 862 | 2.05 | 5.5 | -0.98 | |
4 | 165 | 0.030 093 | 0.000 560 | 0.282 723±0.000 027 | 741 | 1 097 | -1.74 | 1.8 | -0.96 | |
5 | 164 | 0.071 446 | 0.001 235 | 0.282 817±0.000 025 | 620 | 889 | 1.59 | 5.1 | -0.93 | |
6 | 165 | 0.132 881 | 0.002 177 | 0.282 841±0.000 030 | 601 | 840 | 2.44 | 5.8 | -0.95 | |
7 | 160 | 0.094 543 | 0.001 611 | 0.282 837±0.000 023 | 597 | 848 | 2.31 | 5.7 | -0.96 | |
8 | 162 | 0.079 647 | 0.001 325 | 0.282 821±0.000 026 | 617 | 882 | 1.72 | 5.1 | -0.97 | |
9 | 163 | 0.060 721 | 0.001 059 | 0.282 693±0.000 026 | 793 | 1 168 | -2.78 | 0.7 | -0.95 | |
10 | 164 | 0.089 598 | 0.001 512 | 0.282 762±0.000 027 | 704 | 1 015 | -0.36 | 3.1 | -0.93 | |
11 | 161 | 0.135 710 | 0.002 228 | 0.282 873±0.000 028 | 556 | 771 | 3.56 | 6.9 | -0.95 | |
12 | 163 | 0.098 089 | 0.001 644 | 0.282 773±0.000 024 | 691 | 993 | 0.02 | 3.4 | -0.96 | |
13 | 162 | 0.072 985 | 0.001 324 | 0.282 746±0.000 022 | 723 | 1 050 | -0.91 | 2.5 | -0.94 | |
15 | 164 | 0.110 921 | 0.001 891 | 0.282 841±0.000 026 | 597 | 840 | 2.42 | 5.8 | -0.95 | |
16 | 161 | 0.090 756 | 0.001 517 | 0.282 769±0.000 027 | 694 | 1 001 | -0.11 | 3.3 | -0.97 | |
17 | 169 | 0.058 462 | 0.001 007 | 0.282 751±0.000 026 | 710 | 1 034 | -0.75 | 2.9 | -0.94 | |
18 | 163 | 0.108 347 | 0.001 835 | 0.282 893±0.000 027 | 521 | 722 | 4.27 | 7.7 | -0.96 | |
20 | 164 | 0.070 769 | 0.001 247 | 0.282 795±0.000 025 | 651 | 938 | 0.83 | 4.3 | -0.94 | |
21 | 165 | 0.114 290 | 0.001 901 | 0.282 836±0.000 024 | 604 | 850 | 2.27 | 5.7 | -0.95 | |
22 | 165 | 0.093 102 | 0.001 675 | 0.282 774±0.000 023 | 690 | 989 | 0.07 | 3.5 | -0.94 | |
23 | 161 | 0.121 754 | 0.002 080 | 0.282 777±0.000 029 | 693 | 987 | 0.18 | 3.5 | -0.93 | |
24 | 162 | 0.135 761 | 0.002 356 | 0.282 886±0.000 026 | 538 | 741 | 4.04 | 7.3 | -0.94 | |
25 | 162 | 0.106 936 | 0.001 850 | 0.282 757±0.000 029 | 718 | 1 031 | -0.55 | 2.8 | -0.98 | |
26 | 166 | 0.034 608 | 0.000 645 | 0.282 742±0.000 022 | 717 | 1 054 | -1.08 | 2.5 | -0.97 | |
27 | 164 | 0.048 099 | 0.000 851 | 0.282 717±0.000 026 | 755 | 1 113 | -1.96 | 1.6 | -0.96 | |
28 | 166 | 0.079 346 | 0.001 421 | 0.282 824±0.000 024 | 613 | 872 | 1.85 | 5.3 | -0.96 | |
29 | 164 | 0.079 920 | 0.001 368 | 0.282 821±0.000 023 | 618 | 882 | 1.72 | 5.2 | -0.94 | |
30 | 166 | 0.122 002 | 0.002 123 | 0.282 821±0.000 027 | 629 | 884 | 1.74 | 5.2 | -0.96 | |
WJC-2 (王姜 冲岩体) | 1 | 158 | 0.122 478 | 0.002 081 | 0.282 863±0.000 028 | 568 | 794 | 3.21 | 6.5 | -0.94 |
2 | 163 | 0.060 987 | 0.001 095 | 0.282 767±0.000 027 | 689 | 1 001 | -0.17 | 3.3 | -0.97 | |
3 | 156 | 0.062 784 | 0.001 091 | 0.282 756±0.000 028 | 704 | 1 030 | -0.56 | 2.8 | -0.97 | |
4 | 156 | 0.182 452 | 0.003 059 | 0.282 920±0.000 030 | 498 | 672 | 5.23 | 8.3 | -0.91 | |
5 | 157 | 0.072 200 | 0.001 255 | 0.282 796±0.000 028 | 651 | 941 | 0.85 | 4.2 | -0.96 | |
6 | 161 | 0.057 827 | 0.000 992 | 0.282 750±0.000 026 | 711 | 1 040 | -0.77 | 2.7 | -0.97 | |
7 | 159 | 0.078 144 | 0.001 339 | 0.282 747±0.000 022 | 722 | 1 050 | -0.88 | 2.5 | -0.96 | |
8 | 158 | 0.120 985 | 0.002 093 | 0.282 705±0.000 030 | 798 | 1 150 | -2.36 | 0.9 | -0.94 | |
9 | 157 | 0.097 548 | 0.001 693 | 0.282 765±0.000 026 | 703 | 1 013 | -0.23 | 3.0 | -0.95 | |
10 | 157 | 0.096 685 | 0.001 687 | 0.282 779±0.000 025 | 683 | 982 | 0.24 | 3.5 | -0.95 | |
11 | 156 | 0.123 280 | 0.002 153 | 0.282 797±0.000 028 | 665 | 944 | 0.90 | 4.1 | -0.94 | |
12 | 158 | 0.180 122 | 0.002 940 | 0.282 838±0.000 029 | 618 | 855 | 2.35 | 5.5 | -0.91 | |
13 | 160 | 0.094 577 | 0.001 638 | 0.282 774±0.000 023 | 688 | 990 | 0.09 | 3.4 | -0.95 | |
14 | 158 | 0.161 252 | 0.002 711 | 0.282 810±0.000 030 | 656 | 918 | 1.35 | 4.5 | -0.92 | |
16 | 160 | 0.070 054 | 0.001 240 | 0.282 789±0.000 025 | 661 | 955 | 0.60 | 4.0 | -0.96 | |
17 | 157 | 0.091 408 | 0.001 603 | 0.282 786±0.000 026 | 671 | 965 | 0.50 | 3.8 | -0.95 | |
样品及 分析点号 | 年龄/Ma | 176Yb/ 177Hf | 176Lu/ 177Hf | 176Hf/177Hf±2σ | TDM /Ma | /Ma | εHf(0) | εHf(t) | ||
WJC-2 (王姜 冲岩体) | 18 | 159 | 0.085 027 | 0.001 567 | 0.282 782±0.000 027 | 676 | 973 | 0.35 | 3.7 | -0.95 |
19 | 161 | 0.093 584 | 0.001 698 | 0.282 809±0.000 030 | 640 | 912 | 1.31 | 4.7 | -0.95 | |
20 | 166 | 0.093 402 | 0.001 684 | 0.282 729±0.000 025 | 755 | 1 090 | -1.52 | 1.9 | -0.95 | |
21 | 157 | 0.059 336 | 0.001 064 | 0.282 810±0.000 023 | 628 | 908 | 1.34 | 4.7 | -0.97 | |
22 | 160 | 0.102 317 | 0.001 782 | 0.282 715±0.000 028 | 777 | 1 125 | -2.01 | 1.3 | -0.95 | |
23 | 167 | 0.043 941 | 0.000 816 | 0.282 694±0.000 027 | 787 | 1 163 | -2.77 | 0.8 | -0.98 | |
24 | 161 | 0.126 266 | 0.002 223 | 0.282 853±0.000 029 | 585 | 817 | 2.85 | 6.2 | -0.93 | |
25 | 159 | 0.089 278 | 0.001 601 | 0.282 788±0.000 024 | 668 | 960 | 0.56 | 3.9 | -0.95 | |
26 | 162 | 0.091 475 | 0.001 675 | 0.282 766±0.000 027 | 701 | 1 008 | -0.20 | 3.2 | -0.95 | |
27 | 158 | 0.128 285 | 0.002 316 | 0.282 805±0.000 025 | 657 | 928 | 1.15 | 4.4 | -0.93 | |
28 | 156 | 0.079 977 | 0.001 469 | 0.282 719±0.000 026 | 765 | 1 117 | -1.88 | 1.4 | -0.96 | |
29 | 161 | 0.135 838 | 0.002 402 | 0.282 823±0.000 028 | 631 | 884 | 1.82 | 5.1 | -0.93 | |
30 | 159 | 0.128 861 | 0.002 305 | 0.282 749±0.000 030 | 738 | 1 053 | -0.82 | 2.4 | -0.93 |
Fig.8 Nb/Yb vs.Th/Yb ((a),base map after reference [43]) and La/Yb vs. Sm/Yb ((b),base map after reference [44])diagrams for the Guluo and Wangjiangchong gabbros
Fig.9 Ternary 2Nb-Zr/4-Y((a),base map after reference [53]) and Hf/3-Th-Ta((b),base map after reference [54]) tectonic discrimination diagrams for the gabbro samples
[1] | 许德如, 贺转利, 李鹏春, 等. 湘东北地区晚燕山期细碧质玄武岩的发现及地质意义[J]. 地质科学, 2006,41(2):311-332. |
[2] | LI X H, LI W X, LI Z X. On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China[J]. Science Bulletin, 2007,52(14):1873-1885. |
[3] |
YE H M, MAO J R, ZHAO X L, et al. Revisiting Early-Middle Jurassic igneous activity in the Nanling Mountains, South China: Geochemistry and implications for regional geodynamics[J]. Journal of Asian Earth Sciences, 2013,72(4):108-117.
DOI URL |
[4] |
WANG Y, FAN W, ZHANG G, et al. Phanerozoic tectonics of the South China Block: Key observations and controversies[J]. Gondwana Research, 2013,23(4):1273-1305.
DOI URL |
[5] |
MILLET L. Geochronological and geochemical results from Mesozoic basalts in southern South China Block support the flat-slab subduction model[J]. Lithos, 2012,132:127-140.
DOI URL |
[6] |
ZHOU X M, LI W X. Origin of Late Mesozoic igneous rocks in Southeastern China: Implications for lithosphere subduction and underplating of mafic magmas[J]. Tectonophysics, 2000,326(3):269-287.
DOI URL |
[7] |
JIANG Y H, WANG G C, LIU Z, et al. Repeated slab advanceâ retreat of the Palaeo-Pacific plate underneath SE China[J]. International Geology Review, 2015,57(4):472-491.
DOI URL |
[8] |
CHEN C H, LEE C Y, SHINJO R. Was there Jurassic paleo-Pacific subduction in South China?: Constraints from 40Ar/ 39Ar dating, elemental and Sr-Nd-Pb isotopic geochemistry of the Mesozoic basalts [J]. Lithos, 2008,106(1/2):83-92.
DOI URL |
[9] |
WANG Y J, FAN W M, GUO F, et al. Geochemistry of Mesozoic mafic rocks adjacent to the Chenzhou-Linwu fault, South China: Implications for the lithospheric boundary between the Yangtze and Cathaysia Blocks[J]. International Geology Review, 2003,45(3):263-286.
DOI URL |
[10] |
WANG Y, FAN W, PENG T, et al. Elemental and Sr-Nd isotopic systematics of the Early Mesozoic volcanic sequence in southern Jiangxi Province, South China: petrogenesis and tectonic implications[J]. International Journal of Earth Sciences, 2005,94(1):53-65.
DOI URL |
[11] | MÜLLER D, GROVES D I. Potassic Igneous Rocks and Associated Gold-copper Mineralization[M]. Berlin:Springer-verlag, 2000: 265-266. |
[12] | 李献华, 周汉文, 刘颖, 等. 桂东南钾玄质侵入岩带及其岩石学和地球化学特征[J]. 科学通报, 1999,44(18):1992-1998. |
[13] | 卢成忠. 浙江梧村地区钾玄质岩浆岩的发现及其找矿意义[J]. 现代地质, 2007,21(3):443-450. |
[14] | 农军年, 邹瑜, 邱恩露, 等. 桂东南大村和古龙岩体的成因:地球化学、锆石U-Pb年龄及Hf同位素制约[J]. 地质通报, 2017,36(2/3):224-237. |
[15] | 许华, 黄炳诚, 倪战旭, 等. 广西大瑶山古罗碱性辉长岩体LA-ICP-MS锆石U-Pb年龄、岩石学、地球化学及其构造意义[J]. 华南地质与矿产, 2014,30(4):342-351. |
[16] | 张云, 孙立新, 张天福, 等. 内蒙古狼山地区乌花辉长岩的年代学、地球化学和Sr-Nd-Hf同位素组成:对地幔源区特征和岩石成因的约束[J]. 现代地质, 2020,34(3):1-16. |
[17] |
SLÁMA J, KOSTLER J, CONDON D J, et al. Plesovice-a new natural reference material for U-Pb and Hf isotopic microanalysis[J]. Chemical Geology, 2008,249(1/2):1-35.
DOI URL |
[18] |
ANDERSEN T. Correction of common lead in U-Pb analyses that do not report 204Pb [J]. Chemical Geology, 2002,192(1/2):59-79.
DOI URL |
[19] | LUDWIG K R. User’s Manual for a Geochronological Toolkit for Microsoft Excel (Isoplot/Ex Version 3.0)[M]. Berkeley: Berkeley Geochronology Center, 2003: 1-70. |
[20] | 侯可军, 李延河, 田有荣. LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J]. 矿床地质, 2009,28(4):481-492. |
[21] |
SCHERER E, MUNKER C, MEZGER K. Calibration of the lutetium-hafnium clock[J]. Science, 2001,293:683-687.
DOI URL PMID |
[22] |
BLICHERTTOFT J, ALBAREDE F. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system[J]. Earth and Planetary Science Letters, 1997,148(1/2):243-258.
DOI URL |
[23] |
VERVOORT J D, BLICHERT-TOFT J. Evolution of the depleted mantle: Hf isotope evidence from juvenile rocks through time[J]. Geochimica et Cosmochimica Acta, 1999,63(3/4):533-556.
DOI URL |
[24] |
GRIFFIN W L, WANG X, JACKSON S E, et al. Zircon chemistry and magma mixing, SE China: In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes[J]. Lithos, 2002,61(3/4):237-269.
DOI URL |
[25] |
BELOUSOVA E A, GRIFFIN W L, O’REILLY S Y,et al. Igneous zircon: trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 2002,143(5):602-622.
DOI URL |
[26] |
CHEN F, HEGNER E, TODT W. Zircon ages and Nd isotopic and chemical compositions of orthogneisses from the Black Forest, Germany: evidence for a Cambrian magmatic arc[J]. International Journal of Earth Sciences, 2000,88(4):791-802.
DOI URL |
[27] | BARROS C E D, NARDI L V S, DILLENBURG S R, et al. Detrital minerals of modern beach sediments in southern Brazil: a provenance study based on the chemistry of zircon.[J]. Journal of Coastal Research, 2010,26(1):80-93. |
[28] | MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth Science Reviews, 1994,37(3/4):224. |
[29] |
PECCERILLO A, TAYLOR S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976,58(1):63-81.
DOI URL |
[30] | MIDDLEMOST E A K. Magmas and Magmatic Rocks: An Introduction to Igneous Petrology[M]. London:Longman, 1985. |
[31] |
SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society,London, Special Publication, 1989,42:313-345.
DOI URL |
[32] | 许华, 倪战旭, 潘艺文, 等. 1∶25万贵县幅(F49C001002)区域地质调查成果报告[R]. 南宁:广西壮族自治区地质调查院, 2013. |
[33] | 广西壮族自治区地质局区域普查大队. 广西1∶20万桂平幅区域地质测量报告[R]. 南宁:广西壮族自治区地质局, 1964. |
[34] | 广西壮族自治区地质矿产局. 广西壮族自治区区域地质志[M]. 北京: 地质出版社, 1985. |
[35] | 李江, 张耿, 周娟华, 等. 广西1∶50万数字地质图说明书[R]. 南宁:广西壮族自治区地质矿产勘查开发局, 2006. |
[36] | WYLLIE P J, SEKINE T. The formation of mantle phlogopite in subduction zone hybridization[J]. Contributions to Mineralogy & Petrology, 1982,79(4):375-380. |
[37] |
MENZIES M. Alkaline rocks and their inclusions: a window on the Earth’s interior[J]. Geological Society, London, Special Publications, 1987,30(1):15-27.
DOI URL |
[38] | ROGERS N W. Potassic magmatism as a key to trace-element enrichment processes in the upper mantle[J]. Journal of Volcano-logy & Geothermal Research, 1992,50(1):85-99. |
[39] | MÜLLER D, ROCK N M S, GROVES D I. Geochemical discrimination between shoshonitic and potassic volcanic rocks in different tectonic settings: A pilot study[J]. Mineralogy & Petrology, 1992,46(4):259-289. |
[40] |
MCKENZIE D, BICKLE M J. The volume and composition of melt generated by extension of the lithosphere[J]. Journal of Petrology, 1988,29(3):625-679.
DOI URL |
[41] | 刘彬, 马昌前, 蒋红安, 等. 东昆仑早古生代洋壳俯冲与碰撞造山作用的转换:来自胡晓钦镁铁质岩石的证据[J]. 岩石学报, 2013,29(6):2093-2106. |
[42] |
HUANG Y, HAWKESWORTH C, SMITH I, et al. Geochemistry of Late Cenozoic basaltic volcanism in Northland and Coromandel, New Zealand: implications for mantle enrichment processes[J]. Chemical Geology, 2000,164(3/4):219-238.
DOI URL |
[43] |
PEARCE J A. Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust[J]. Lithos, 2008,100(1/4):14-48.
DOI URL |
[44] | XU Xisheng, XIN X. Late Mesozoic-Cenozoic basaltic rocks and crust-mantle interaction, SE China[J]. Geological Journal of China Universities, 2005,11(3):318-334. |
[45] | 王冠, 孙丰月, 李碧乐, 等. 东昆仑夏日哈木铜镍矿镁铁质-超镁铁质岩体岩相学、锆石U-Pb年代学、地球化学及其构造意义[J]. 地学前缘, 2014,21(6):381-401. |
[46] | 吴福元, 李献华, 郑永飞, 等. Lu-Hf同位素体系及其岩石学应用[J]. 岩石学报, 2007,23(2):185-220. |
[47] |
ANDERSON D L. Large Igneous Provinces, Delamination, and Fertile Mantle[J]. Elements, 2005,1(5):271-275.
DOI URL |
[48] |
WANG Y, ZHANG A, FAN W, et al. Origin of paleosubduction-modified mantle for Silurian gabbro in the Cathaysia Block: Geochronological and geochemical evidence[J]. Lithos, 2013,160/161(1):37-54.
DOI URL |
[49] |
FLÈCHE M R L, CAMIRÉ G, JENNER G A. Geochemistry of post-Acadian, Carboniferous continental intraplate basalts from the Maritimes Basin, Magdalen Islands, Québec, Canada[J]. Chemical Geology, 1998,148(3/4):115-136.
DOI URL |
[50] |
WILSON M. Review of igneous petrogenesis: a global tectonic approach[J]. Terra Nova, 2010,1(2):218-222.
DOI URL |
[51] | 郭新生, 陈江峰, 张巽, 等. 桂东南富钾岩浆杂岩的Nd同位素组成:华南中生代地幔物质上涌事件[J]. 岩石学报, 2001,17(1):19-27. |
[52] |
ROGERS N W, JAMES D, KELLEY S P, et al. The generation of potassic lavas from the eastern Virunga Province, Rwanda[J]. Journal of Petrology, 1998,39(6):1223-1247.
DOI URL |
[53] |
MESCHEDE M. A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram[J]. Chemical Geology, 56(3/4):207-218.
DOI URL |
[54] |
WOOD D A. Avariably veined suboceanic upper mantle-genetic significance for mid-ocean ridge basalts from geochemical evidence[J]. Geology, 1979,7:499-503.
DOI URL |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||