Geoscience ›› 2025, Vol. 39 ›› Issue (04): 1039-1058.DOI: 10.19657/j.geoscience.1000-8527.2025.020
• Ore Deposit and Petrology • Previous Articles Next Articles
LI Furong1,2,3(), PAN Jiayong1,*(
), ZHONG Fujun1, ZENG Renyu1, YAN Jie1, Huang Di4, DANG Feipeng4
Online:
2025-08-10
Published:
2025-08-27
Contact:
PAN Jiayong
CLC Number:
LI Furong, PAN Jiayong, ZHONG Fujun, ZENG Renyu, YAN Jie, Huang Di, DANG Feipeng. Petrogenesis and Uranium Mineralization Potential of Granites Hosting the Xiaoshan Deposit in the Lujing Uranium Ore Field, Jiangxi Province[J]. Geoscience, 2025, 39(04): 1039-1058.
Fig.1 Tectonic location (a), geological sketch of the Zhuguang-Guidong ore concentration area (b) (modified from reference [4]), and geological sketch of the Lujing uranium ore field (c) (modified from reference [16])
Fig.4 Cathodoluminescence (CL) images of some zircons from granites in the Xiaoshan deposit (solid circles indicate zircon dating positions, dashed circles indicate Lu-Hf analysis positions)
测点号 | 含量(10-6) | Th/U | 同位素比值 | 同位素年龄(Ma) | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/ 206Pb | 2σ | 207Pb/ 235U | 2σ | 206Pb/ 238U | 2σ | 207Pb/ 206Pb | 2σ | 207Pb/ 235U | 2σ | 206Pb/ 238U | 2σ | |||
样品22XSZ08 | ||||||||||||||||
1 | 262 | 644 | 0.41 | 0.0465 | 0.0029 | 0.2372 | 0.0152 | 0.0367 | 0.0009 | 20 | 144 | 216 | 12 | 233 | 5 | |
2 | 1349 | 884 | 1.53 | 0.0466 | 0.0027 | 0.2432 | 0.0142 | 0.0377 | 0.0009 | 28 | 139 | 221 | 12 | 239 | 5 | |
3 | 253 | 209 | 1.21 | 0.0549 | 0.0060 | 0.2841 | 0.0335 | 0.0372 | 0.0012 | 409 | 246 | 254 | 26 | 235 | 7 | |
4 | 152 | 309 | 0.49 | 0.0437 | 0.0047 | 0.2422 | 0.0191 | 0.0381 | 0.0012 | 368 | 106 | 220 | 16 | 241 | 7 | |
5 | 446 | 509 | 0.88 | 0.0514 | 0.0031 | 0.2686 | 0.0167 | 0.0379 | 0.0009 | 261 | 136 | 242 | 13 | 240 | 6 | |
6* | 243 | 174 | 1.39 | 0.0690 | 0.0033 | 1.5691 | 0.0763 | 0.1658 | 0.0047 | 898 | 100 | 958 | 30 | 989 | 26 | |
7 | 1570 | 917 | 1.71 | 0.0493 | 0.0026 | 0.2580 | 0.0149 | 0.0380 | 0.0011 | 161 | 126 | 233 | 12 | 240 | 7 | |
8 | 381 | 398 | 0.96 | 0.0528 | 0.0043 | 0.2734 | 0.0216 | 0.0376 | 0.0008 | 320 | 185 | 245 | 17 | 238 | 5 | |
9 | 169 | 343 | 0.49 | 0.0522 | 0.0038 | 0.2697 | 0.0195 | 0.0376 | 0.0009 | 295 | 168 | 242 | 16 | 238 | 6 | |
10 | 275 | 239 | 1.15 | 0.0517 | 0.0055 | 0.2640 | 0.0258 | 0.0362 | 0.0009 | 333 | 246 | 238 | 21 | 229 | 6 | |
11* | 125 | 181 | 0.69 | 0.1621 | 0.0067 | 9.8812 | 0.4439 | 0.4406 | 0.0106 | 2480 | 70 | 2424 | 41 | 2353 | 48 | |
12 | 173 | 511 | 0.34 | 0.0530 | 0.0036 | 0.2758 | 0.0192 | 0.0376 | 0.0010 | 328 | 156 | 247 | 15 | 238 | 6 | |
13 | 190 | 837 | 0.23 | 0.0535 | 0.0028 | 0.2786 | 0.0159 | 0.0376 | 0.0009 | 350 | 119 | 250 | 13 | 238 | 6 | |
14* | 345 | 1500 | 0.23 | 0.0568 | 0.0026 | 0.2728 | 0.0128 | 0.0347 | 0.0007 | 483 | 97 | 245 | 10 | 220 | 4 | |
15 | 147 | 107 | 1.37 | 0.0535 | 0.0083 | 0.3188 | 0.0386 | 0.0375 | 0.0015 | 350 | 383 | 281 | 30 | 238 | 10 | |
16 | 236 | 923 | 0.26 | 0.0595 | 0.0039 | 0.3091 | 0.0205 | 0.0375 | 0.0008 | 587 | 144 | 273 | 16 | 237 | 5 | |
17 | 288 | 312 | 0.92 | 0.0513 | 0.0042 | 0.2690 | 0.0220 | 0.0376 | 0.0010 | 257 | 189 | 242 | 18 | 238 | 6 | |
18 | 345 | 321 | 1.07 | 0.0594 | 0.0046 | 0.3141 | 0.0267 | 0.0377 | 0.0011 | 589 | 168 | 277 | 21 | 239 | 7 | |
19* | 53 | 317 | 0.17 | 0.0610 | 0.0037 | 0.5652 | 0.0368 | 0.0666 | 0.0020 | 639 | 130 | 455 | 24 | 416 | 12 | |
20 | 121 | 722 | 0.17 | 0.0520 | 0.0036 | 0.2715 | 0.0182 | 0.0377 | 0.0010 | 283 | 157 | 244 | 15 | 238 | 6 | |
21* | 173 | 546 | 0.32 | 0.0631 | 0.0038 | 0.4503 | 0.0412 | 0.0498 | 0.0028 | 711 | 130 | 377 | 29 | 313 | 17 | |
样品22XSZ17 | ||||||||||||||||
1 | 1083 | 707 | 1.53 | 0.0506 | 0.0032 | 0.2580 | 0.0170 | 0.0369 | 0.0009 | 220 | 142 | 233 | 14 | 234 | 6 | |
2 | 171 | 416 | 0.41 | 0.0477 | 0.0034 | 0.2442 | 0.0183 | 0.0370 | 0.0009 | 83 | 172 | 222 | 15 | 235 | 5 | |
3 | 231 | 677 | 0.34 | 0.0488 | 0.0034 | 0.2508 | 0.0169 | 0.0375 | 0.0010 | 139 | 156 | 227 | 14 | 238 | 6 | |
4 | 661 | 935 | 0.71 | 0.0509 | 0.0028 | 0.2576 | 0.0141 | 0.0367 | 0.0007 | 235 | 132 | 233 | 11 | 232 | 4 | |
5 | 306 | 1508 | 0.20 | 0.0475 | 0.0038 | 0.2640 | 0.0156 | 0.0373 | 0.0013 | 72 | 181 | 238 | 12 | 236 | 8 | |
6 | 691 | 813 | 0.85 | 0.0505 | 0.0028 | 0.2618 | 0.0164 | 0.0375 | 0.0010 | 220 | 130 | 236 | 13 | 237 | 6 | |
7 | 123 | 107 | 1.16 | 0.0505 | 0.0069 | 0.3028 | 0.0334 | 0.0381 | 0.0013 | 217 | 289 | 269 | 26 | 241 | 8 | |
8 | 310 | 394 | 0.79 | 0.0479 | 0.0036 | 0.2498 | 0.0189 | 0.0380 | 0.0011 | 100 | 157 | 226 | 15 | 240 | 7 | |
9 | 509 | 867 | 0.59 | 0.0501 | 0.0030 | 0.2624 | 0.0168 | 0.0377 | 0.0010 | 211 | 145 | 237 | 13 | 239 | 6 | |
10 | 938 | 740 | 1.27 | 0.0523 | 0.0030 | 0.2649 | 0.0153 | 0.0366 | 0.0008 | 298 | 136 | 239 | 12 | 232 | 5 | |
11 | 352 | 777 | 0.45 | 0.0521 | 0.0028 | 0.2774 | 0.0163 | 0.0384 | 0.0012 | 287 | 122 | 249 | 13 | 243 | 7 | |
12 | 278 | 1354 | 0.21 | 0.0543 | 0.0068 | 0.2773 | 0.0334 | 0.0371 | 0.0007 | 389 | 282 | 248 | 27 | 235 | 5 | |
13 | 185 | 399 | 0.46 | 0.0505 | 0.0052 | 0.2842 | 0.0257 | 0.0382 | 0.0012 | 217 | 226 | 254 | 20 | 242 | 7 | |
14* | 310 | 692 | 0.45 | 0.0704 | 0.0026 | 1.1543 | 0.0490 | 0.1182 | 0.0026 | 939 | 76 | 779 | 23 | 720 | 15 | |
15 | 365 | 488 | 0.75 | 0.0487 | 0.0034 | 0.2529 | 0.0175 | 0.0378 | 0.0009 | 132 | 156 | 229 | 14 | 239 | 6 | |
16 | 1183 | 1094 | 1.08 | 0.0507 | 0.0032 | 0.2630 | 0.0170 | 0.0376 | 0.0010 | 233 | 148 | 237 | 14 | 238 | 6 | |
17 | 354 | 2406 | 0.15 | 0.0508 | 0.0023 | 0.2636 | 0.0133 | 0.0373 | 0.0009 | 232 | 110 | 238 | 11 | 236 | 5 | |
18 | 558 | 438 | 1.27 | 0.0499 | 0.0038 | 0.2553 | 0.0192 | 0.0372 | 0.0011 | 191 | -17 | 231 | 16 | 235 | 7 | |
19 | 538 | 325 | 1.65 | 0.0541 | 0.0045 | 0.2837 | 0.0258 | 0.0374 | 0.0011 | 376 | 189 | 254 | 20 | 237 | 7 | |
20 | 1153 | 1160 | 0.99 | 0.0481 | 0.0030 | 0.2539 | 0.0152 | 0.0379 | 0.0010 | 106 | 137 | 230 | 12 | 240 | 6 | |
21 | 1071 | 1206 | 0.89 | 0.0489 | 0.0026 | 0.2619 | 0.0146 | 0.0386 | 0.0010 | 143 | 126 | 236 | 12 | 244 | 6 | |
22* | 332 | 365 | 0.91 | 0.0684 | 0.0035 | 1.4895 | 0.0837 | 0.1561 | 0.0041 | 880 | 107 | 926 | 34 | 935 | 23 |
Table 1 LA-ICP-MS zircon U-Pb dating results of the uranium-hosting granites in the Xiaoshan deposit
测点号 | 含量(10-6) | Th/U | 同位素比值 | 同位素年龄(Ma) | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/ 206Pb | 2σ | 207Pb/ 235U | 2σ | 206Pb/ 238U | 2σ | 207Pb/ 206Pb | 2σ | 207Pb/ 235U | 2σ | 206Pb/ 238U | 2σ | |||
样品22XSZ08 | ||||||||||||||||
1 | 262 | 644 | 0.41 | 0.0465 | 0.0029 | 0.2372 | 0.0152 | 0.0367 | 0.0009 | 20 | 144 | 216 | 12 | 233 | 5 | |
2 | 1349 | 884 | 1.53 | 0.0466 | 0.0027 | 0.2432 | 0.0142 | 0.0377 | 0.0009 | 28 | 139 | 221 | 12 | 239 | 5 | |
3 | 253 | 209 | 1.21 | 0.0549 | 0.0060 | 0.2841 | 0.0335 | 0.0372 | 0.0012 | 409 | 246 | 254 | 26 | 235 | 7 | |
4 | 152 | 309 | 0.49 | 0.0437 | 0.0047 | 0.2422 | 0.0191 | 0.0381 | 0.0012 | 368 | 106 | 220 | 16 | 241 | 7 | |
5 | 446 | 509 | 0.88 | 0.0514 | 0.0031 | 0.2686 | 0.0167 | 0.0379 | 0.0009 | 261 | 136 | 242 | 13 | 240 | 6 | |
6* | 243 | 174 | 1.39 | 0.0690 | 0.0033 | 1.5691 | 0.0763 | 0.1658 | 0.0047 | 898 | 100 | 958 | 30 | 989 | 26 | |
7 | 1570 | 917 | 1.71 | 0.0493 | 0.0026 | 0.2580 | 0.0149 | 0.0380 | 0.0011 | 161 | 126 | 233 | 12 | 240 | 7 | |
8 | 381 | 398 | 0.96 | 0.0528 | 0.0043 | 0.2734 | 0.0216 | 0.0376 | 0.0008 | 320 | 185 | 245 | 17 | 238 | 5 | |
9 | 169 | 343 | 0.49 | 0.0522 | 0.0038 | 0.2697 | 0.0195 | 0.0376 | 0.0009 | 295 | 168 | 242 | 16 | 238 | 6 | |
10 | 275 | 239 | 1.15 | 0.0517 | 0.0055 | 0.2640 | 0.0258 | 0.0362 | 0.0009 | 333 | 246 | 238 | 21 | 229 | 6 | |
11* | 125 | 181 | 0.69 | 0.1621 | 0.0067 | 9.8812 | 0.4439 | 0.4406 | 0.0106 | 2480 | 70 | 2424 | 41 | 2353 | 48 | |
12 | 173 | 511 | 0.34 | 0.0530 | 0.0036 | 0.2758 | 0.0192 | 0.0376 | 0.0010 | 328 | 156 | 247 | 15 | 238 | 6 | |
13 | 190 | 837 | 0.23 | 0.0535 | 0.0028 | 0.2786 | 0.0159 | 0.0376 | 0.0009 | 350 | 119 | 250 | 13 | 238 | 6 | |
14* | 345 | 1500 | 0.23 | 0.0568 | 0.0026 | 0.2728 | 0.0128 | 0.0347 | 0.0007 | 483 | 97 | 245 | 10 | 220 | 4 | |
15 | 147 | 107 | 1.37 | 0.0535 | 0.0083 | 0.3188 | 0.0386 | 0.0375 | 0.0015 | 350 | 383 | 281 | 30 | 238 | 10 | |
16 | 236 | 923 | 0.26 | 0.0595 | 0.0039 | 0.3091 | 0.0205 | 0.0375 | 0.0008 | 587 | 144 | 273 | 16 | 237 | 5 | |
17 | 288 | 312 | 0.92 | 0.0513 | 0.0042 | 0.2690 | 0.0220 | 0.0376 | 0.0010 | 257 | 189 | 242 | 18 | 238 | 6 | |
18 | 345 | 321 | 1.07 | 0.0594 | 0.0046 | 0.3141 | 0.0267 | 0.0377 | 0.0011 | 589 | 168 | 277 | 21 | 239 | 7 | |
19* | 53 | 317 | 0.17 | 0.0610 | 0.0037 | 0.5652 | 0.0368 | 0.0666 | 0.0020 | 639 | 130 | 455 | 24 | 416 | 12 | |
20 | 121 | 722 | 0.17 | 0.0520 | 0.0036 | 0.2715 | 0.0182 | 0.0377 | 0.0010 | 283 | 157 | 244 | 15 | 238 | 6 | |
21* | 173 | 546 | 0.32 | 0.0631 | 0.0038 | 0.4503 | 0.0412 | 0.0498 | 0.0028 | 711 | 130 | 377 | 29 | 313 | 17 | |
样品22XSZ17 | ||||||||||||||||
1 | 1083 | 707 | 1.53 | 0.0506 | 0.0032 | 0.2580 | 0.0170 | 0.0369 | 0.0009 | 220 | 142 | 233 | 14 | 234 | 6 | |
2 | 171 | 416 | 0.41 | 0.0477 | 0.0034 | 0.2442 | 0.0183 | 0.0370 | 0.0009 | 83 | 172 | 222 | 15 | 235 | 5 | |
3 | 231 | 677 | 0.34 | 0.0488 | 0.0034 | 0.2508 | 0.0169 | 0.0375 | 0.0010 | 139 | 156 | 227 | 14 | 238 | 6 | |
4 | 661 | 935 | 0.71 | 0.0509 | 0.0028 | 0.2576 | 0.0141 | 0.0367 | 0.0007 | 235 | 132 | 233 | 11 | 232 | 4 | |
5 | 306 | 1508 | 0.20 | 0.0475 | 0.0038 | 0.2640 | 0.0156 | 0.0373 | 0.0013 | 72 | 181 | 238 | 12 | 236 | 8 | |
6 | 691 | 813 | 0.85 | 0.0505 | 0.0028 | 0.2618 | 0.0164 | 0.0375 | 0.0010 | 220 | 130 | 236 | 13 | 237 | 6 | |
7 | 123 | 107 | 1.16 | 0.0505 | 0.0069 | 0.3028 | 0.0334 | 0.0381 | 0.0013 | 217 | 289 | 269 | 26 | 241 | 8 | |
8 | 310 | 394 | 0.79 | 0.0479 | 0.0036 | 0.2498 | 0.0189 | 0.0380 | 0.0011 | 100 | 157 | 226 | 15 | 240 | 7 | |
9 | 509 | 867 | 0.59 | 0.0501 | 0.0030 | 0.2624 | 0.0168 | 0.0377 | 0.0010 | 211 | 145 | 237 | 13 | 239 | 6 | |
10 | 938 | 740 | 1.27 | 0.0523 | 0.0030 | 0.2649 | 0.0153 | 0.0366 | 0.0008 | 298 | 136 | 239 | 12 | 232 | 5 | |
11 | 352 | 777 | 0.45 | 0.0521 | 0.0028 | 0.2774 | 0.0163 | 0.0384 | 0.0012 | 287 | 122 | 249 | 13 | 243 | 7 | |
12 | 278 | 1354 | 0.21 | 0.0543 | 0.0068 | 0.2773 | 0.0334 | 0.0371 | 0.0007 | 389 | 282 | 248 | 27 | 235 | 5 | |
13 | 185 | 399 | 0.46 | 0.0505 | 0.0052 | 0.2842 | 0.0257 | 0.0382 | 0.0012 | 217 | 226 | 254 | 20 | 242 | 7 | |
14* | 310 | 692 | 0.45 | 0.0704 | 0.0026 | 1.1543 | 0.0490 | 0.1182 | 0.0026 | 939 | 76 | 779 | 23 | 720 | 15 | |
15 | 365 | 488 | 0.75 | 0.0487 | 0.0034 | 0.2529 | 0.0175 | 0.0378 | 0.0009 | 132 | 156 | 229 | 14 | 239 | 6 | |
16 | 1183 | 1094 | 1.08 | 0.0507 | 0.0032 | 0.2630 | 0.0170 | 0.0376 | 0.0010 | 233 | 148 | 237 | 14 | 238 | 6 | |
17 | 354 | 2406 | 0.15 | 0.0508 | 0.0023 | 0.2636 | 0.0133 | 0.0373 | 0.0009 | 232 | 110 | 238 | 11 | 236 | 5 | |
18 | 558 | 438 | 1.27 | 0.0499 | 0.0038 | 0.2553 | 0.0192 | 0.0372 | 0.0011 | 191 | -17 | 231 | 16 | 235 | 7 | |
19 | 538 | 325 | 1.65 | 0.0541 | 0.0045 | 0.2837 | 0.0258 | 0.0374 | 0.0011 | 376 | 189 | 254 | 20 | 237 | 7 | |
20 | 1153 | 1160 | 0.99 | 0.0481 | 0.0030 | 0.2539 | 0.0152 | 0.0379 | 0.0010 | 106 | 137 | 230 | 12 | 240 | 6 | |
21 | 1071 | 1206 | 0.89 | 0.0489 | 0.0026 | 0.2619 | 0.0146 | 0.0386 | 0.0010 | 143 | 126 | 236 | 12 | 244 | 6 | |
22* | 332 | 365 | 0.91 | 0.0684 | 0.0035 | 1.4895 | 0.0837 | 0.1561 | 0.0041 | 880 | 107 | 926 | 34 | 935 | 23 |
测点号 | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | (176Hf/177Hf)ini | εHf(t) | 2σ | tDM1 (Ga) | tDM2 (Ga) |
---|---|---|---|---|---|---|---|---|---|---|---|
样品22XSZ08 | |||||||||||
08-1 | 0.051752 | 0.002320 | 0.001343 | 0.000062 | 0.282228 | 0.000015 | 0.282221855 | -14.75 | 0.54 | 1.46 | 2.16 |
08-3 | 0.030282 | 0.000478 | 0.000755 | 0.000010 | 0.282319 | 0.000016 | 0.282315972 | -11.36 | 0.56 | 1.31 | 1.95 |
08-5 | 0.083336 | 0.003800 | 0.002476 | 0.000146 | 0.282426 | 0.000022 | 0.2824144 | -7.78 | 0.78 | 1.22 | 1.73 |
08-7 | 0.039806 | 0.001776 | 0.001082 | 0.000042 | 0.282387 | 0.000014 | 0.282382336 | -8.90 | 0.49 | 1.22 | 1.80 |
08-8 | 0.070908 | 0.001860 | 0.001748 | 0.000048 | 0.282478 | 0.000016 | 0.282470115 | -5.85 | 0.55 | 1.12 | 1.61 |
08-9 | 0.029698 | 0.000920 | 0.000792 | 0.000026 | 0.282290 | 0.000017 | 0.28228637 | -12.35 | 0.61 | 1.35 | 2.01 |
08-12 | 0.052881 | 0.000892 | 0.001395 | 0.000024 | 0.282306 | 0.000015 | 0.282300182 | -11.86 | 0.53 | 1.35 | 1.98 |
08-13 | 0.051805 | 0.001582 | 0.001466 | 0.000059 | 0.282424 | 0.000017 | 0.28241717 | -7.72 | 0.59 | 1.19 | 1.73 |
08-14 | 0.072667 | 0.001446 | 0.001817 | 0.000031 | 0.282370 | 0.000016 | 0.282362723 | -10.05 | 0.58 | 1.27 | 1.86 |
08-20 | 0.057078 | 0.002420 | 0.001622 | 0.000089 | 0.282341 | 0.000015 | 0.282333367 | -10.68 | 0.54 | 1.31 | 1.91 |
样品22XSZ17 | |||||||||||
17-1 | 0.051379 | 0.001300 | 0.001575 | 0.000039 | 0.282474 | 0.000022 | 0.282467009 | -6.05 | 0.79 | 1.12 | 1.62 |
17-2 | 0.034197 | 0.000474 | 0.000904 | 0.000016 | 0.282309 | 0.000015 | 0.282304734 | -11.78 | 0.53 | 1.33 | 1.98 |
17-4 | 0.057237 | 0.001354 | 0.001501 | 0.000030 | 0.282459 | 0.000016 | 0.28245258 | -6.60 | 0.58 | 1.14 | 1.65 |
17-5 | 0.053680 | 0.000866 | 0.001422 | 0.000025 | 0.282415 | 0.000014 | 0.282409118 | -8.05 | 0.49 | 1.20 | 1.74 |
17-6 | 0.044582 | 0.001632 | 0.001305 | 0.000053 | 0.282401 | 0.000018 | 0.282395303 | -8.51 | 0.62 | 1.21 | 1.77 |
17-8 | 0.057156 | 0.002640 | 0.001541 | 0.000049 | 0.282530 | 0.000015 | 0.282523369 | -3.91 | 0.52 | 1.04 | 1.49 |
17-10 | 0.034131 | 0.001036 | 0.000915 | 0.000022 | 0.282402 | 0.000017 | 0.282398128 | -8.53 | 0.59 | 1.20 | 1.77 |
17-12 | 0.040529 | 0.000932 | 0.001094 | 0.000020 | 0.282440 | 0.000017 | 0.282435599 | -7.14 | 0.59 | 1.15 | 1.69 |
17-16 | 0.055642 | 0.001728 | 0.001475 | 0.000024 | 0.282360 | 0.000017 | 0.282353732 | -9.97 | 0.60 | 1.26 | 1.87 |
17-18 | 0.052761 | 0.002420 | 0.001563 | 0.000084 | 0.282483 | 0.000022 | 0.28247562 | -5.71 | 0.79 | 1.10 | 1.60 |
Table 2 Zircon Hf isotopic composition of the uranium-hosting granites in the Xiaoshan deposit
测点号 | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | (176Hf/177Hf)ini | εHf(t) | 2σ | tDM1 (Ga) | tDM2 (Ga) |
---|---|---|---|---|---|---|---|---|---|---|---|
样品22XSZ08 | |||||||||||
08-1 | 0.051752 | 0.002320 | 0.001343 | 0.000062 | 0.282228 | 0.000015 | 0.282221855 | -14.75 | 0.54 | 1.46 | 2.16 |
08-3 | 0.030282 | 0.000478 | 0.000755 | 0.000010 | 0.282319 | 0.000016 | 0.282315972 | -11.36 | 0.56 | 1.31 | 1.95 |
08-5 | 0.083336 | 0.003800 | 0.002476 | 0.000146 | 0.282426 | 0.000022 | 0.2824144 | -7.78 | 0.78 | 1.22 | 1.73 |
08-7 | 0.039806 | 0.001776 | 0.001082 | 0.000042 | 0.282387 | 0.000014 | 0.282382336 | -8.90 | 0.49 | 1.22 | 1.80 |
08-8 | 0.070908 | 0.001860 | 0.001748 | 0.000048 | 0.282478 | 0.000016 | 0.282470115 | -5.85 | 0.55 | 1.12 | 1.61 |
08-9 | 0.029698 | 0.000920 | 0.000792 | 0.000026 | 0.282290 | 0.000017 | 0.28228637 | -12.35 | 0.61 | 1.35 | 2.01 |
08-12 | 0.052881 | 0.000892 | 0.001395 | 0.000024 | 0.282306 | 0.000015 | 0.282300182 | -11.86 | 0.53 | 1.35 | 1.98 |
08-13 | 0.051805 | 0.001582 | 0.001466 | 0.000059 | 0.282424 | 0.000017 | 0.28241717 | -7.72 | 0.59 | 1.19 | 1.73 |
08-14 | 0.072667 | 0.001446 | 0.001817 | 0.000031 | 0.282370 | 0.000016 | 0.282362723 | -10.05 | 0.58 | 1.27 | 1.86 |
08-20 | 0.057078 | 0.002420 | 0.001622 | 0.000089 | 0.282341 | 0.000015 | 0.282333367 | -10.68 | 0.54 | 1.31 | 1.91 |
样品22XSZ17 | |||||||||||
17-1 | 0.051379 | 0.001300 | 0.001575 | 0.000039 | 0.282474 | 0.000022 | 0.282467009 | -6.05 | 0.79 | 1.12 | 1.62 |
17-2 | 0.034197 | 0.000474 | 0.000904 | 0.000016 | 0.282309 | 0.000015 | 0.282304734 | -11.78 | 0.53 | 1.33 | 1.98 |
17-4 | 0.057237 | 0.001354 | 0.001501 | 0.000030 | 0.282459 | 0.000016 | 0.28245258 | -6.60 | 0.58 | 1.14 | 1.65 |
17-5 | 0.053680 | 0.000866 | 0.001422 | 0.000025 | 0.282415 | 0.000014 | 0.282409118 | -8.05 | 0.49 | 1.20 | 1.74 |
17-6 | 0.044582 | 0.001632 | 0.001305 | 0.000053 | 0.282401 | 0.000018 | 0.282395303 | -8.51 | 0.62 | 1.21 | 1.77 |
17-8 | 0.057156 | 0.002640 | 0.001541 | 0.000049 | 0.282530 | 0.000015 | 0.282523369 | -3.91 | 0.52 | 1.04 | 1.49 |
17-10 | 0.034131 | 0.001036 | 0.000915 | 0.000022 | 0.282402 | 0.000017 | 0.282398128 | -8.53 | 0.59 | 1.20 | 1.77 |
17-12 | 0.040529 | 0.000932 | 0.001094 | 0.000020 | 0.282440 | 0.000017 | 0.282435599 | -7.14 | 0.59 | 1.15 | 1.69 |
17-16 | 0.055642 | 0.001728 | 0.001475 | 0.000024 | 0.282360 | 0.000017 | 0.282353732 | -9.97 | 0.60 | 1.26 | 1.87 |
17-18 | 0.052761 | 0.002420 | 0.001563 | 0.000084 | 0.282483 | 0.000022 | 0.28247562 | -5.71 | 0.79 | 1.10 | 1.60 |
样品号 | 22XSZ07 | 22XSZ08 | 22XSZ19 | 22XSZ20 | 22XSZ21 | 20GX02 | 20GX06 | 20GX07 | 22XSZ17 | 22XSZ24 | 22XSZ25 | 22XSZ26 | ||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
中粗粒似斑状黑云母花岗岩 | 细粒二云母花岗岩 | |||||||||||||||
SiO2 | 71.76 | 72.11 | 71.22 | 69.56 | 74.46 | 74.91 | 73.30 | 73.23 | 69.86 | 73.50 | 75.92 | 73.27 | ||||
TiO2 | 0.18 | 0.22 | 0.20 | 0.24 | 0.20 | 0.34 | 0.33 | 0.21 | 0.10 | 0.07 | 0.05 | 0.10 | ||||
Al2O3 | 14.77 | 14.78 | 14.90 | 14.64 | 13.10 | 12.56 | 14.06 | 13.78 | 16.34 | 14.95 | 13.13 | 14.24 | ||||
Fe2O3 | 1.50 | 1.71 | 1.68 | 1.96 | 1.70 | 0.67 | 0.36 | 0.38 | 1.07 | 1.07 | 0.79 | 0.99 | ||||
MnO | 0.04 | 0.04 | 0.05 | 0.08 | 0.04 | 0.06 | 0.05 | 0.05 | 0.04 | 0.04 | 0.02 | 0.03 | ||||
MgO | 0.48 | 0.42 | 0.61 | 0.65 | 0.36 | 0.46 | 0.46 | 0.44 | 0.42 | 0.14 | 0.11 | 0.25 | ||||
CaO | 0.94 | 0.74 | 1.15 | 2.19 | 0.70 | 1.09 | 1.01 | 1.05 | 1.21 | 0.29 | 0.23 | 0.95 | ||||
Na2O | 2.68 | 3.33 | 2.04 | 1.92 | 2.82 | 2.76 | 2.87 | 2.84 | 3.96 | 3.70 | 4.12 | 3.62 | ||||
K2O | 5.42 | 4.98 | 5.17 | 5.09 | 4.87 | 3.90 | 4.79 | 4.71 | 5.11 | 5.04 | 4.31 | 4.78 | ||||
P2O5 | 0.10 | 0.15 | 0.11 | 0.18 | 0.13 | 0.20 | 0.17 | 0.14 | 0.12 | 0.16 | 0.11 | 0.09 | ||||
FeO | 1.08 | 1.26 | 1.24 | 1.48 | 1.30 | 1.83 | 1.69 | 1.50 | 0.68 | 0.78 | 0.44 | 0.76 | ||||
LOI | 1.60 | 1.10 | 2.39 | 3.12 | 1.08 | 1.58 | 0.79 | 1.50 | 1.76 | 0.89 | 0.73 | 1.09 | ||||
Rb | 485.92 | 473.00 | 471.93 | 508.05 | 510.93 | 376.00 | 386.00 | 472.00 | 558.67 | 675.00 | 437.00 | 492.00 | ||||
Ba | 240.18 | 181.09 | 226.94 | 217.02 | 186.07 | 207.00 | 258.00 | 224.00 | 32.73 | 17.90 | 25.20 | 26.50 | ||||
Sr | 75.03 | 67.25 | 97.47 | 83.08 | 52.86 | 73.30 | 76.90 | 65.90 | 37.27 | 18.30 | 24.40 | 23.30 | ||||
Pb | 46.05 | 40.93 | 44.41 | 45.36 | 41.46 | 34.30 | 45.10 | 42.50 | 57.97 | 31.30 | 35.10 | 53.30 | ||||
U | 17.90 | 27.86 | 16.59 | 20.18 | 18.16 | 22.40 | 24.30 | 18.30 | 45.39 | 36.70 | 33.40 | 28.90 | ||||
Zr | 115.02 | 122.59 | 130.88 | 133.25 | 118.03 | 158.00 | 121.00 | 129.00 | 49.58 | 51.20 | 34.80 | 51.60 | ||||
Hf | 3.62 | 3.91 | 4.10 | 4.17 | 3.93 | 4.50 | 3.50 | 3.70 | 2.55 | 2.99 | 1.92 | 2.29 | ||||
Y | 25.44 | 30.65 | 31.96 | 30.99 | 27.50 | 38.40 | 23.80 | 24.20 | 21.01 | 12.70 | 7.37 | 14.70 | ||||
Nb | 16.03 | 20.99 | 20.78 | 23.20 | 19.21 | 21.90 | 19.40 | 19.00 | 25.83 | 20.80 | 12.70 | 17.40 | ||||
Ta | 3.73 | 5.04 | 4.04 | 4.58 | 3.51 | 4.60 | 3.50 | 4.50 | 8.02 | 5.89 | 5.16 | 5.33 | ||||
Th | 18.28 | 21.80 | 22.39 | 25.36 | 20.46 | 28.60 | 24.50 | 23.60 | 9.94 | 5.60 | 4.62 | 7.52 | ||||
Th/U | 1.02 | 0.78 | 1.35 | 1.26 | 1.13 | 40.50 | 35.00 | 34.30 | 8.32 | 0.15 | 0.14 | 0.26 | ||||
La | 28.40 | 30.08 | 32.46 | 35.43 | 30.70 | 85.80 | 74.50 | 72.10 | 18.45 | 4.85 | 3.55 | 8.80 | ||||
Ce | 59.03 | 62.49 | 66.81 | 73.63 | 63.51 | 9.74 | 8.27 | 8.00 | 2.12 | 12.80 | 7.76 | 20.00 | ||||
Pr | 6.55 | 7.01 | 7.48 | 8.22 | 7.16 | 33.60 | 28.80 | 27.50 | 7.64 | 1.21 | 0.91 | 2.19 | ||||
Nd | 23.33 | 25.23 | 26.62 | 29.47 | 25.69 | 7.06 | 6.24 | 5.59 | 2.17 | 4.24 | 3.19 | 7.71 | ||||
Sm | 5.03 | 5.41 | 5.78 | 6.39 | 5.58 | 0.55 | 0.61 | 0.53 | 0.11 | 1.15 | 0.93 | 1.87 | ||||
Eu | 0.52 | 0.47 | 0.53 | 0.57 | 0.50 | 6.31 | 5.13 | 4.70 | 2.17 | 0.04 | 0.05 | 0.11 | ||||
Gd | 4.07 | 4.57 | 5.05 | 5.59 | 4.79 | 0.97 | 0.76 | 0.71 | 0.46 | 1.23 | 0.89 | 1.74 | ||||
Tb | 0.70 | 0.79 | 0.86 | 0.90 | 0.80 | 5.97 | 4.20 | 4.02 | 3.07 | 0.27 | 0.19 | 0.34 | ||||
Dy | 4.02 | 4.80 | 5.14 | 5.12 | 4.44 | 1.27 | 0.79 | 0.76 | 0.62 | 1.88 | 1.27 | 2.19 | ||||
Ho | 0.79 | 0.94 | 0.99 | 0.96 | 0.82 | 3.68 | 2.12 | 2.23 | 1.94 | 0.38 | 0.25 | 0.45 | ||||
Er | 2.32 | 2.77 | 2.81 | 2.65 | 2.36 | 0.60 | 0.31 | 0.35 | 0.39 | 1.17 | 0.76 | 1.45 | ||||
Tm | 0.37 | 0.47 | 0.45 | 0.42 | 0.37 | 3.89 | 1.96 | 2.26 | 2.97 | 0.22 | 0.14 | 0.27 | ||||
Yb | 2.52 | 3.20 | 2.96 | 2.73 | 2.50 | 0.58 | 0.28 | 0.35 | 0.45 | 1.66 | 1.09 | 1.98 | ||||
Lu | 0.38 | 0.47 | 0.44 | 0.40 | 0.37 | 0.58 | 0.28 | 0.35 | 0.85 | 0.24 | 0.16 | 0.29 | ||||
LREE/HREE | 8.10 | 7.25 | 7.47 | 8.20 | 8.09 | 7.62 | 9.87 | 9.62 | 3.22 | 3.44 | 3.45 | 4.67 | ||||
δEu | 0.35 | 0.29 | 0.30 | 0.29 | 0.30 | 0.25 | 0.33 | 0.32 | 0.15 | 0.11 | 0.18 | 0.18 | ||||
来源 | 本文 | 本文 | 本文 | 本文 | 本文 | 文献[31] | 文献[31] | 文献[31] | 本文 | 本文 | 本文 | 本文 |
Table 3 Major elements(%), trace elements and rare earth elements(10 -6) analysis results of the granites in the Xiaoshan deposit
样品号 | 22XSZ07 | 22XSZ08 | 22XSZ19 | 22XSZ20 | 22XSZ21 | 20GX02 | 20GX06 | 20GX07 | 22XSZ17 | 22XSZ24 | 22XSZ25 | 22XSZ26 | ||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
中粗粒似斑状黑云母花岗岩 | 细粒二云母花岗岩 | |||||||||||||||
SiO2 | 71.76 | 72.11 | 71.22 | 69.56 | 74.46 | 74.91 | 73.30 | 73.23 | 69.86 | 73.50 | 75.92 | 73.27 | ||||
TiO2 | 0.18 | 0.22 | 0.20 | 0.24 | 0.20 | 0.34 | 0.33 | 0.21 | 0.10 | 0.07 | 0.05 | 0.10 | ||||
Al2O3 | 14.77 | 14.78 | 14.90 | 14.64 | 13.10 | 12.56 | 14.06 | 13.78 | 16.34 | 14.95 | 13.13 | 14.24 | ||||
Fe2O3 | 1.50 | 1.71 | 1.68 | 1.96 | 1.70 | 0.67 | 0.36 | 0.38 | 1.07 | 1.07 | 0.79 | 0.99 | ||||
MnO | 0.04 | 0.04 | 0.05 | 0.08 | 0.04 | 0.06 | 0.05 | 0.05 | 0.04 | 0.04 | 0.02 | 0.03 | ||||
MgO | 0.48 | 0.42 | 0.61 | 0.65 | 0.36 | 0.46 | 0.46 | 0.44 | 0.42 | 0.14 | 0.11 | 0.25 | ||||
CaO | 0.94 | 0.74 | 1.15 | 2.19 | 0.70 | 1.09 | 1.01 | 1.05 | 1.21 | 0.29 | 0.23 | 0.95 | ||||
Na2O | 2.68 | 3.33 | 2.04 | 1.92 | 2.82 | 2.76 | 2.87 | 2.84 | 3.96 | 3.70 | 4.12 | 3.62 | ||||
K2O | 5.42 | 4.98 | 5.17 | 5.09 | 4.87 | 3.90 | 4.79 | 4.71 | 5.11 | 5.04 | 4.31 | 4.78 | ||||
P2O5 | 0.10 | 0.15 | 0.11 | 0.18 | 0.13 | 0.20 | 0.17 | 0.14 | 0.12 | 0.16 | 0.11 | 0.09 | ||||
FeO | 1.08 | 1.26 | 1.24 | 1.48 | 1.30 | 1.83 | 1.69 | 1.50 | 0.68 | 0.78 | 0.44 | 0.76 | ||||
LOI | 1.60 | 1.10 | 2.39 | 3.12 | 1.08 | 1.58 | 0.79 | 1.50 | 1.76 | 0.89 | 0.73 | 1.09 | ||||
Rb | 485.92 | 473.00 | 471.93 | 508.05 | 510.93 | 376.00 | 386.00 | 472.00 | 558.67 | 675.00 | 437.00 | 492.00 | ||||
Ba | 240.18 | 181.09 | 226.94 | 217.02 | 186.07 | 207.00 | 258.00 | 224.00 | 32.73 | 17.90 | 25.20 | 26.50 | ||||
Sr | 75.03 | 67.25 | 97.47 | 83.08 | 52.86 | 73.30 | 76.90 | 65.90 | 37.27 | 18.30 | 24.40 | 23.30 | ||||
Pb | 46.05 | 40.93 | 44.41 | 45.36 | 41.46 | 34.30 | 45.10 | 42.50 | 57.97 | 31.30 | 35.10 | 53.30 | ||||
U | 17.90 | 27.86 | 16.59 | 20.18 | 18.16 | 22.40 | 24.30 | 18.30 | 45.39 | 36.70 | 33.40 | 28.90 | ||||
Zr | 115.02 | 122.59 | 130.88 | 133.25 | 118.03 | 158.00 | 121.00 | 129.00 | 49.58 | 51.20 | 34.80 | 51.60 | ||||
Hf | 3.62 | 3.91 | 4.10 | 4.17 | 3.93 | 4.50 | 3.50 | 3.70 | 2.55 | 2.99 | 1.92 | 2.29 | ||||
Y | 25.44 | 30.65 | 31.96 | 30.99 | 27.50 | 38.40 | 23.80 | 24.20 | 21.01 | 12.70 | 7.37 | 14.70 | ||||
Nb | 16.03 | 20.99 | 20.78 | 23.20 | 19.21 | 21.90 | 19.40 | 19.00 | 25.83 | 20.80 | 12.70 | 17.40 | ||||
Ta | 3.73 | 5.04 | 4.04 | 4.58 | 3.51 | 4.60 | 3.50 | 4.50 | 8.02 | 5.89 | 5.16 | 5.33 | ||||
Th | 18.28 | 21.80 | 22.39 | 25.36 | 20.46 | 28.60 | 24.50 | 23.60 | 9.94 | 5.60 | 4.62 | 7.52 | ||||
Th/U | 1.02 | 0.78 | 1.35 | 1.26 | 1.13 | 40.50 | 35.00 | 34.30 | 8.32 | 0.15 | 0.14 | 0.26 | ||||
La | 28.40 | 30.08 | 32.46 | 35.43 | 30.70 | 85.80 | 74.50 | 72.10 | 18.45 | 4.85 | 3.55 | 8.80 | ||||
Ce | 59.03 | 62.49 | 66.81 | 73.63 | 63.51 | 9.74 | 8.27 | 8.00 | 2.12 | 12.80 | 7.76 | 20.00 | ||||
Pr | 6.55 | 7.01 | 7.48 | 8.22 | 7.16 | 33.60 | 28.80 | 27.50 | 7.64 | 1.21 | 0.91 | 2.19 | ||||
Nd | 23.33 | 25.23 | 26.62 | 29.47 | 25.69 | 7.06 | 6.24 | 5.59 | 2.17 | 4.24 | 3.19 | 7.71 | ||||
Sm | 5.03 | 5.41 | 5.78 | 6.39 | 5.58 | 0.55 | 0.61 | 0.53 | 0.11 | 1.15 | 0.93 | 1.87 | ||||
Eu | 0.52 | 0.47 | 0.53 | 0.57 | 0.50 | 6.31 | 5.13 | 4.70 | 2.17 | 0.04 | 0.05 | 0.11 | ||||
Gd | 4.07 | 4.57 | 5.05 | 5.59 | 4.79 | 0.97 | 0.76 | 0.71 | 0.46 | 1.23 | 0.89 | 1.74 | ||||
Tb | 0.70 | 0.79 | 0.86 | 0.90 | 0.80 | 5.97 | 4.20 | 4.02 | 3.07 | 0.27 | 0.19 | 0.34 | ||||
Dy | 4.02 | 4.80 | 5.14 | 5.12 | 4.44 | 1.27 | 0.79 | 0.76 | 0.62 | 1.88 | 1.27 | 2.19 | ||||
Ho | 0.79 | 0.94 | 0.99 | 0.96 | 0.82 | 3.68 | 2.12 | 2.23 | 1.94 | 0.38 | 0.25 | 0.45 | ||||
Er | 2.32 | 2.77 | 2.81 | 2.65 | 2.36 | 0.60 | 0.31 | 0.35 | 0.39 | 1.17 | 0.76 | 1.45 | ||||
Tm | 0.37 | 0.47 | 0.45 | 0.42 | 0.37 | 3.89 | 1.96 | 2.26 | 2.97 | 0.22 | 0.14 | 0.27 | ||||
Yb | 2.52 | 3.20 | 2.96 | 2.73 | 2.50 | 0.58 | 0.28 | 0.35 | 0.45 | 1.66 | 1.09 | 1.98 | ||||
Lu | 0.38 | 0.47 | 0.44 | 0.40 | 0.37 | 0.58 | 0.28 | 0.35 | 0.85 | 0.24 | 0.16 | 0.29 | ||||
LREE/HREE | 8.10 | 7.25 | 7.47 | 8.20 | 8.09 | 7.62 | 9.87 | 9.62 | 3.22 | 3.44 | 3.45 | 4.67 | ||||
δEu | 0.35 | 0.29 | 0.30 | 0.29 | 0.30 | 0.25 | 0.33 | 0.32 | 0.15 | 0.11 | 0.18 | 0.18 | ||||
来源 | 本文 | 本文 | 本文 | 本文 | 本文 | 文献[31] | 文献[31] | 文献[31] | 本文 | 本文 | 本文 | 本文 |
Fig.7 TAS diagram (a) (base map after reference [32]), K2O-SiO2 diagram (b) (base map after reference[33]), and A/NK-A/CNK diagram (c) (base map after reference [34]) of the Xiaoshan granite
Fig.9 Primitive mantle-normalized trace element spider diagram(a) and chondrite-normalized REE distribution pattern (b) of granites in the Xiaoshan deposit (normalization values from reference [37])
序号 | 地区 | 岩体名称 | 岩性 | 定年方法 | 年龄(Ma) | 点数 | 资料来源 |
---|---|---|---|---|---|---|---|
1 | 牛尾岭矿床 | 文英岩体 | 细粒二云母花岗岩 | LA-ICPMS锆石U-Pb法 | 236.9±1.8 | 14 | 李杰等[ |
2 | 仙人洞地段 | 文英岩体 | 中粒黑云母花岗岩 | LA-ICPMS锆石U-Pb法 | 227.0±1.1 | 15 | 李杰等[ |
3 | 1011矿点 | 文英岩体 | 中粗粒斑状黑云母花岗岩 | LA-ICPMS锆石U-Pb法 | 235.8±1.5 | 15 | 李杰等[ |
4 | 梨花开矿床 | 文英岩体 | 中粗粒斑状黑云母花岗岩 | LA-ICPMS锆石U-Pb法 | 236.5±1.7 | 17 | 李杰等[ |
5 | 大场坪矿床 | 大场坪岩体 | 中粒花岗碎裂岩 | LA-ICPMS锆石U-Pb法 | 238.0±1.4 | 16 | 李杰等[ |
6 | 官庄地段 | 官庄岩体 | 细粒二长花岗岩 | LA-ICPMS锆石U-Pb法 | 235.7±1.0 | 17 | 李杰等[ |
7 | 黄峰岭矿床 | 文英岩体 | 中粒黑云母花岗岩 | SHRIMP锆石U-Pb法 | 235.4±1.1 | 6 | 韩娟等[ |
8 | 蕉叶垅地区 | 蕉叶垅岩体 | 中粗粒花岗岩 | LA-ICPMS锆石U-Pb法 | 247±2.2 | 10 | 张万良等[ |
Table 4 Isotopic ages of the granites in the Lujing ore field
序号 | 地区 | 岩体名称 | 岩性 | 定年方法 | 年龄(Ma) | 点数 | 资料来源 |
---|---|---|---|---|---|---|---|
1 | 牛尾岭矿床 | 文英岩体 | 细粒二云母花岗岩 | LA-ICPMS锆石U-Pb法 | 236.9±1.8 | 14 | 李杰等[ |
2 | 仙人洞地段 | 文英岩体 | 中粒黑云母花岗岩 | LA-ICPMS锆石U-Pb法 | 227.0±1.1 | 15 | 李杰等[ |
3 | 1011矿点 | 文英岩体 | 中粗粒斑状黑云母花岗岩 | LA-ICPMS锆石U-Pb法 | 235.8±1.5 | 15 | 李杰等[ |
4 | 梨花开矿床 | 文英岩体 | 中粗粒斑状黑云母花岗岩 | LA-ICPMS锆石U-Pb法 | 236.5±1.7 | 17 | 李杰等[ |
5 | 大场坪矿床 | 大场坪岩体 | 中粒花岗碎裂岩 | LA-ICPMS锆石U-Pb法 | 238.0±1.4 | 16 | 李杰等[ |
6 | 官庄地段 | 官庄岩体 | 细粒二长花岗岩 | LA-ICPMS锆石U-Pb法 | 235.7±1.0 | 17 | 李杰等[ |
7 | 黄峰岭矿床 | 文英岩体 | 中粒黑云母花岗岩 | SHRIMP锆石U-Pb法 | 235.4±1.1 | 6 | 韩娟等[ |
8 | 蕉叶垅地区 | 蕉叶垅岩体 | 中粗粒花岗岩 | LA-ICPMS锆石U-Pb法 | 247±2.2 | 10 | 张万良等[ |
Fig.10 (Zr+Nd+Ce+Y)-(K2O+Na2O)/CaO diagram (a) (base map after reference[47]), ACF diagram of granite (b) (base map after reference[49]), Rb-Th (c), and Rb-Y (d) diagrams (trends of I-type and S-type granites in the figures are from reference[49])
Fig.13 Hand specimen of alkali metasomatic rock (a), microscopic photo of K-feldspathization (b), and hand specimen of uranium ore (c) from the Xiaoshan deposit
[1] | 蔡煜琦, 张金带, 李子颖, 等. 中国铀矿资源特征及成矿规律概要[J]. 地质学报, 2015, 89(6): 1051-1069. |
[2] | 杜乐天. 花岗岩型铀矿文集[M]. 北京: 原子能出版社, 1982. |
[3] | 李杰, 黄宏业, 刘子杰, 等. 诸广中段印支期花岗岩LA-ICP-MS锆石U-Pb年龄及微量元素特征[J]. 大地构造与成矿学, 2021, 45(6): 1216-1239. |
[4] | 陶继华, 李武显, 杨跃贵, 等. 南岭东段龙源坝燕山期黑云母花岗岩的锆石微量元素特征及地质意义[J]. 东华理工大学学报(自然科学版), 2024, 47(5):431-441. |
[5] | 李响, 王令占, 涂兵, 等. 粤西北印支期太保岩体的锆石U-Pb年代学、地球化学及岩石成因[J]. 地球科学, 2021, 464: 1199-1216. |
[6] | 冯明月, 何德宝. 富铀花岗岩源岩特征[J]. 世界核地质科学, 2012, 29(1): 1-8. |
[7] | 夏宗强, 肖敏. 南岭南带河源地区花岗岩LA-ICP-MS锆石U-Pb年代学、地球化学及其地质意义[J]. 东华理工大学学报(自然科学版), 2024, 47(4):349-361. |
[8] | 吴佳, 巫建华, 刘晓东. 桃山—诸广铀成矿带成岩成矿年代学研究进展及存在问题[J]. 矿床地质, 2022, 41(2): 241-254. |
[9] | 杜乐天. 中国热液铀矿基本成矿规律和一般热液成矿学[M]. 中国热液铀矿基本成矿规律和一般热液成矿学, 2001. |
[10] |
张舒, 张赞赞, 胡召齐, 等. 长江中下游成矿带庐枞矿集区花岗岩型铀矿床成矿作用研究进展[J]. 现代地质, 2023, 37: 1435-1448.
DOI |
[11] | 孙岳, 潘家永, 肖振华, 等. 诸广山中部鹿井铀矿田构造解析与找矿远景探讨[J]. 中国地质, 2020, 47(2): 362-374. |
[12] | 孙立强. 南岭诸广山地区中生代花岗岩成因及其对铀成矿作用的启示[D]. 南京: 南京大学, 2018. |
[13] | 李冉, 王全涛. 湖南鹿井地区铀成矿地质背景及找矿思路分析[J]. 中国锰业, 2016, 34(3): 26-28. |
[14] | 潘春蓉. 湖南羊角脑铀矿床地质特征及成因探讨[D]. 昆明: 昆明理工大学, 2017. |
[15] | 许谱林, 唐湘生, 郭福生, 等. 华南鹿井铀矿田NE向QF_(2)断裂特征及其与铀成矿关系探讨[J]. 大地构造与成矿学, 2023, 47: 98-114. |
[16] | 黄宏业, 黄思东, 蔡松峰. 湖南鹿井地区铀成矿地质背景及找矿思路分析[J]. 世界核地质科学, 2008, 25(2): 63-67. |
[17] | WIEDENBECK M. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards Newsletter, 1995, 19(1):1-23. |
[18] | SLÁMA J, KOLER J, CONDON D J, et al. Pleovice zircon—A new natural reference material for U-Pb and Hf isotopic microanalysis[J]. CHEMICAL GEOLOGY, 2008. |
[19] | 杨爱雪, 吕水, 许曼, 等. 冀东高家店岩体锆石年代学和微量元素地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2025, 55(02):503-524. |
[20] | ZHANG R X, WANG L, LIU B, et al. Mu opioid receptor-containing neurons mediate electroacupuncture-produced anti-hyperalgesia in rats with hind paw inflammation[J]. Brain Research, 2005, 1048(1/2):235-240. |
[21] | PAUL W O, HOSKIN. Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia-ScienceDirect[J]. Geochimica et Cosmochimica Acta, 2005, 69(3): 637-648. |
[22] | RUBATTO D, GEBAUER D. Use of cathodoluminescence for U-Pb zircon dating by ion microprobe: Some examples from the Western Alps[M]//Dating of ultrahigh pressure metamorphism:Proceedings of the 3rd International Workshop on Ultrahigh Pressure Metamorphism. Berlin: Springer, 2000: 373-400. |
[23] | PATCHETT P J, VERVOORT J D, SÖDERLUND U, et al. Lu-Hf and Sm-Nd isotopic systematics in chondrites and their constraints on the Lu-Hf properties of the Earth[J]. Earth and Planetary Science Letters, 2004, 222(1): 29-41. |
[24] | 程顺波, 付建明, 马丽艳, 等. 桂东北越城岭岩体加里东期成岩作用:锆石U-Pb年代学,地球化学和Nd-Hf同位素制约[J]. 大地构造与成矿学, 2016, 40(4): 853-872. |
[25] | 郭春丽, 毛景文, 陈毓川. 赣南营前岩体的年代学、地球化学、Sr-Nd-Hf同位素组成及其地质意义[J]. 岩石学报, 2010, 26(3): 919-937. |
[26] | 黄孔文, 郭敏, 汤珂, 等. 粤北黄岗镇侧塘早志留世具似大陆弧特征S型花岗岩成因及地质意义[J]. 地球学报, 2021, 42(4): 487-501. |
[27] | 李光来, 华仁民, 胡东泉, 等. 赣南地区石雷石英闪长岩的成因:岩石化学、副矿物微量元素、锆石U-Pb年代学与Sr-Nd-Hf同位素制约[J]. 岩石学报, 2010, 26: 903-918. |
[28] | 刘文泉, 江卫兵, 李海东, 等. 粤北竹筒尖铀矿床特富矿赋矿花岗岩锆石U-Pb年代学,地球化学,Hf同位素及成因研究[J]. 地质学报, 2019, 93(7): 1720-1737. |
[29] | 孙海瑞, 吕志成, 韩志锐, 等. 湖南大义山晚侏罗世富硼型成锡矿A型花岗岩成因及地质意义[J]. 岩石学报, 2021, 37(6): 1749-1764. |
[30] | 郑佳浩, 郭春丽. 湘南王仙岭花岗岩体的锆石U-Pb年代学、地球化学、锆石Hf同位素特征及其地质意义[J]. 岩石学报, 2012, 28(1): 75-90. |
[31] | 李志鹏, 夏菲, 党飞鹏, 等. 鹿井铀矿田庙背垅地区赋矿碱交代岩岩石学、地球化学特征[J]. 铀矿地质, 2022, 38(1): 46-57. |
[32] | MIDDLEMOST E. A. K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4): 215-224. |
[33] | ANGELOPECCERILLO, 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. |
[34] | PAPU D, MANIAR, et al. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989. |
[35] | BOR-MING, JAHN, and, et al. Highly evolved juvenile granites with tetrad REE patterns: the Woduhe and Baerzhe granites from the Great Xing’an Mountains in NE China[J]. Lithos, 2001, 59(4): 171-98. |
[36] | FLYNN R T, BURNHAM C. W. An experimental determination of rare earth partition coefficients between a chloride containing vapor phase and silicate melts[J]. Geochimica Et Cosmochimica Acta, 1978, 42(6): 685-701. |
[37] | SUN S S, MCDONOUGH W F. Chemical and isotopic systematic of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society of London, Special Publications, 1989, 42(1): 313-345. |
[38] | WANG Y, FAN W, SUN M, et al. Geochronological, geochemical and geothermal constraints on petrogenesis of the Indosinian peraluminous granites in the South China Block: A case study in the Hunan Province[J]. Lithos, 2007, 96(3): 475-502. |
[39] | ZHAO K D, JIANG S Y, CHEN W F, et al. Zircon U-Pb chronology and elemental and Sr-Nd-Hf isotope geochemistry of two Triassic A-type granites in South China: Implication for petrogenesis and Indosinian transtensional tectonism[J]. Lithos, 2013, 160: 292-306. |
[40] | SONG M, SHU L, SANTOSH M. Early Mesozoic granites in the Nanling Belt, South China: Implications for intracontinental tectonics associated with stress regime transformation[J]. Tectonophysics, 2016,676: 148-69. |
[41] | LONG, ZHANG, ZHENYU, et al. Zircon U-Pb geochronology and geochemistry of granites in the Zhuguangshan complex, South China: Implications for uranium mineralization[J]. Lithos An International Journal of Mineralogy Petrology & Geochemistry, 2018,308/309:19-33. |
[42] | 韩娟, 王彦斌, 王登红, 等. 江西黄蜂岭铀矿床花岗岩时代,成因:锆石U-Pb年龄和Hf同位素证据[J]. 地质与勘探, 2011, 47(2): 284-293. |
[43] | 黄迪, 吕川, 周文俊. 高昔铀矿床地质特征及碱交代对铀成矿的影响[J]. 东华理工大学学报:自然科学版, 2017, 40(4): 342-347. |
[44] | 张万良, 高梦奇, 吕川, 等. 湘赣边界鹿井地区印支早期花岗岩的发现及意义[J]. 现代地质, 2018, 32(5): 863-873. |
[45] | LOISELLE M C. Characteristics and origin of anorogenic granites[J]. Geological Society of America Abstracts with Programs, 1979, 11(7): 468. |
[46] | CHAPPELL B W, WHITE A. J. R. Two contrasting granite type[J]. Pacific Geology, 1974,8:407-419. |
[47] | JOSEPH B, WHALEN, et al. A-type granites: geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy & Petrology, 1987, 95(4):407-419. |
[48] | CHAPPELL B W, WHITE A J R. Two contrasting granite types: 25 years later[J]. Australian Journal of Earth Sciences, 2001,48:489-499. |
[49] | CHAPPELL B W, WHITE A J R. I- and S-type granites in the Lachlan Fold Belt. Transactions of the Royal Society of Edinburgh: Earth Sciences, 1992, 83: 1-26. |
[50] | 曹锦山, 张新远, 欧阳光文, 等. 松潘—甘孜造山带南缘青海省秋智地区晚三叠世花岗岩体成因及构造背景[J]. 吉林大学学报(地球科学版), 2025, 55(2):483-502. |
[51] | TAYLOR S R, MCLENNAN S M. The Continental Crust:Its Composition and Evolution. An Examination of the Geochemical Record Preserved in Sedimentary Rocks[M]. Oxford: Blackwell Scientific Publications, 1985. |
[52] | 吴胜宝, 孙国胜, 李雪, 等. 青海沟里地区斜长角闪岩锆石U-Pb年代学、Lu-Hf同位素特征及其指示意义[J]. 吉林大学学报(地球科学版), 2024, 54(3):862-876. |
[53] | SYLVESTER P. Post-collisional strongly peraluminous granites[J]. Journal of Petrology, 1998, 45(1/2/3/4):29-44. |
[54] | HARRIS N B W, PEARCE J A, TINDLE A G. Geochemical characteristics of collision-zone magmatism[C]// COWARD M P, RIES A C. Collision Tectonics. Geological Society of London, Special Publications, 1986, 19: 67-81. |
[55] | 张帮禄, 吕志成, 于晓飞, 等. 西昆仑玛尔坎苏锰矿带含锰岩系时代厘定及地质意义[J]. 吉林大学学报(地球科学版), 2023, 53(1):120-139. |
[56] | 朱鹏飞, 徐浩, 蔡煜琦, 等. 华北板块北缘古大洋闭合时间的限定——来自四子王旗西后壕子同碰撞花岗岩的证据[J]. 地质通报, 2013, 32: 1749-59. |
[57] | 张金阳, 马昌前, 佘振兵, 等. 大别造山带北部铁佛寺早古生代同碰撞型花岗岩:地球化学和年代学证据[J]. 中国科学:地球科学, 2007, 37(1): 1-9. |
[58] | 余心起, 吴淦国, 张达, 等. 华南地区中生代大规模成矿作用与岩石圈多阶段伸展[J]. 地学前缘, 2004, 11: 45-55. |
[59] | 华仁民, 李光来, 张文兰, 等. 华南钨和锡大规模成矿作用的差异及其原因初探[J]. 矿床地质, 2010, 29(1): 9-23. |
[60] | 陈毓川, 王登红, 徐志刚, 等. 华南区域成矿和中生代岩浆成矿规律概要[J]. 大地构造与成矿学, 2014, 38(2): 219-229. |
[61] | 余心起, 吴淦国, 张达, 等. 中国东南部中生代构造体制转换作用研究进展[J]. 自然科学进展, 2005, 15(10): 1167-1174. |
[62] | 刘战庆, 刘善宝, 裴荣富, 等. 赣东北珍珠山花岗岩脉地球化学,锆石U-Pb定年及Hf同位素组成研究[J]. 大地构造与成矿学, 2016, 40(4): 808-825. |
[63] | 孔锦涛. 华南陆缘晚三叠世—中侏罗世沉积物物源分析及其对古太平洋板块俯冲的响应[D]. 长春: 吉林大学, 2023. |
[64] | 洪文涛, 余明刚, 赵希林, 等. 西南日本夜久野(Yakuno)蛇绿混杂岩锆石U-Pb定年及其对晚古生代—早中生代华南大地构造演化的指示[J]. 大地构造与成矿学, 2022, 46(4): 728-743. |
[65] | 徐先兵, 梁承华, 陈家驹, 等. 南岭构造带基础地质特征与成矿地质背景[J]. 地球科学, 2021, 46: 1133-1150. |
[66] | 高奕霖, 赵静, 龙晓平. 祁连马衔山岩群新元古代S型花岗岩地球化学特征及其地质意义[J]. 西北大学学报(自然科学版), 2021, 51(6): 969-984. |
[67] | 张泽明, 丁慧霞, 董昕, 等. 俯冲带部分熔融[J]. 岩石学报, 2020, 36: 2589-2615. |
[68] | 许赛华. 滇东南老君山南捞单元花岗岩年代学及地球化学研究[D]. 昆明: 昆明理工大学, 2019. |
[69] | 许赛华, 任涛, 吕昶良, 等. 滇东南白垩纪高分异S型花岗岩研究进展[J]. 矿物学报, 2019, 39(2): 149-165. |
[70] | 杨玉元, 李宁波, 张东, 等. 赣南清溪黑云母花岗岩的成因及演化特征[J]. 地球化学, 2023, 52(4): 475-495. |
[71] | 贾小辉, 谢国刚, 孟德磊, 等. 粤南海宴A型花岗岩与镁铁质包体的成因及意义[J]. 地球科学, 2018, 43(7): 2294-2309. |
[72] | 梁鹤, 郭海峰, 王强, 等. 赣南地区密坑山早白垩世A型花岗岩的锆石U-Pb年代学、地球化学及岩石成因[J]. 大地构造与成矿学, 2018, 42: 746-758. |
[73] | 张德富, 王先广, 何涛, 曹明轩, 吕婷婷, 龚良信, 徐进. 赣南加里东期重稀土矿赋矿母岩岩石成因及地质意义[J]. 现代地质, 2024, 38(4): 959-976. |
[74] | 邓平, 舒良树, 谭正中. 诸广—贵东大型铀矿聚集区富铀矿成矿地质条件. 地质论评, 2003, 49(5): 486-494. |
[75] | CUNEY M. Felsic magmatism and uranium deposits[J]. Bulletin De La Société Géologique De France, 2014, 185(2): 75-92. |
[76] | 徐浩, 张闯, 庞雅庆, 等. 广东长排铀矿床成矿流体特征[J]. 现代地质, 2018, 32(5): 902-912. |
[77] | 胡欢, 王汝成, 陈卫锋, 等. 桂东北豆乍山产铀花岗岩的铀源矿物研究[J]. 地质论评, 2012(6): 1056-1068. |
[78] | LI F R, ZHANG Y, DANG F P, et al. The role of hydrothermal alteration in uranium mineralization at the Xiaoshan uranium deposit, South China[J]. Ore Geology Reviews, 2024,174: 106324. |
[79] | 凌洪飞. 论花岗岩型铀矿床热液来源:来自氧逸度条件的制约[J]. 地质论评, 2011, 57(2): 193-206. |
[80] | KONTONIKAS-CHAROS A, CIOBANU C L, COOK N J, et al. Deuteric coarsening and albitization in Hiltaba granites from the Olympic Dam IOCG deposit, South Australia[C]// Proceedings of the 13th SGA Biennial Meeting. Nancy: SGA, 2015, 3:1099-1102. |
[81] | KOUSKE A P, SUH C E, GHOGOMU R T, et al. Na-Metasomatism and Uranium Mineralization during a Two-Stage Albitization at Kitongo, Northern Cameroon: Structural and Geochemical Evidence[J]. International Journal of Geosciences, 2012, 3(1): 258-279. |
[82] | 李海东, 潘家永, 夏菲, 等. 相山李家岭铀矿床热液蚀变作用地球化学特征[J]. 现代地质, 2016, 30(3): 555-566. |
[83] | 余达淦, 吴仁贵, 陈培荣. 铀资源地质学[M]. 哈尔滨: 哈尔滨工程大学出版社, 2005. |
[84] | 张万良, 李余亮. 华南信江盆地砂岩型铀成矿控矿因素[J]. 现代地质, 2024, 38(4): 1109-1120. |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||