Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (4): 358-370.DOI: 10.13745/j.esf.sf.2021.10.1
Previous Articles Next Articles
KANG Huan1,2(), CHEN Yuelong2,*(), LI Dapeng2, ZHANG Huiping1, YANG Yi3, XUE Guoliang4, LIU Wei1
Received:
2020-12-31
Revised:
2021-05-07
Online:
2022-07-25
Published:
2022-07-28
Contact:
CHEN Yuelong
CLC Number:
KANG Huan, CHEN Yuelong, LI Dapeng, ZHANG Huiping, YANG Yi, XUE Guoliang, LIU Wei. Late Triassic Mg andesite of Juluotage, eastern Tianshan: Identification and tectonic implications[J]. Earth Science Frontiers, 2022, 29(4): 358-370.
点号 | Th/U | 同位素比值及误差 | 同位素年龄及误差/Ma | 谐和度 | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | |||
X13-7-01 | 0.24 | 0.057 373 | 0.002 365 | 0.417 526 | 0.023 298 | 0.053 330 | 0.002 433 | 506 | 44 | 354 | 8 | 335 | 7 | 94% |
X13-7-02 | 0.71 | 0.052 147 | 0.017 437 | 0.253 333 | 0.086 994 | 0.036 135 | 0.002 756 | 300 | 335 | 229 | 35 | 229 | 9 | 99% |
X13-7-04 | 0.55 | 0.052 103 | 0.003 396 | 0.269 417 | 0.017 671 | 0.037 713 | 0.000 801 | 300 | 74 | 242 | 7 | 239 | 2 | 98% |
X13-7-05 | 0.55 | 0.052 657 | 0.003 618 | 0.270 367 | 0.018 879 | 0.037 384 | 0.000 811 | 322 | 78 | 243 | 8 | 237 | 3 | 97% |
X13-7-06 | 1.29 | 0.051 660 | 0.008 490 | 0.253 090 | 0.038 878 | 0.036 029 | 0.001 235 | 333 | 186 | 229 | 16 | 228 | 4 | 99% |
X13-7-07 | 1.35 | 0.053 506 | 0.006 003 | 0.262 879 | 0.028 213 | 0.036 196 | 0.001 036 | 350 | 128 | 237 | 11 | 229 | 3 | 96% |
X13-7-08 | 0.59 | 0.051 497 | 0.001 973 | 0.265 711 | 0.010 643 | 0.037 447 | 0.000 647 | 265 | 44 | 239 | 4 | 237 | 2 | 99% |
X13-7-09 | 0.60 | 0.051 602 | 0.002 043 | 0.264 393 | 0.010 610 | 0.037 222 | 0.000 625 | 333 | 51 | 238 | 4 | 236 | 2 | 98% |
X13-7-11 | 0.81 | 0.053 987 | 0.006 006 | 0.278 562 | 0.030 109 | 0.038 064 | 0.001 090 | 372 | 131 | 250 | 12 | 241 | 3 | 96% |
X13-7-12 | 0.82 | 0.050 914 | 0.011 049 | 0.259 358 | 0.059 099 | 0.036 898 | 0.001 652 | 235 | 243 | 234 | 24 | 234 | 5 | 99% |
X13-7-13 | 0.53 | 0.056 223 | 0.010 844 | 0.278 892 | 0.049 480 | 0.036 182 | 0.001 579 | 461 | 215 | 250 | 20 | 229 | 5 | 91% |
X13-7-14 | 1.03 | 0.053 052 | 0.006 962 | 0.273 297 | 0.037 821 | 0.037 287 | 0.001 328 | 332 | 148 | 245 | 15 | 236 | 4 | 96% |
X13-7-15 | 1.05 | 0.051 304 | 0.004 904 | 0.260 538 | 0.022 196 | 0.036 873 | 0.001 301 | 254 | 111 | 235 | 9 | 233 | 4 | 99% |
X13-7-20 | 1.32 | 0.057 785 | 0.006 162 | 0.407 489 | 0.042 453 | 0.051 907 | 0.001 755 | 520 | 84 | 347 | 15 | 326 | 5 | 93% |
X13-7-21 | 0.58 | 0.053 930 | 0.005 637 | 0.391 467 | 0.039 063 | 0.052 954 | 0.002 376 | 369 | 114 | 335 | 14 | 333 | 7 | 99% |
X13-7-22 | 0.42 | 0.051 796 | 0.004 066 | 0.271 037 | 0.021 403 | 0.038 010 | 0.000 783 | 276 | 91 | 244 | 9 | 240 | 2 | 98% |
X13-7-23 | 0.47 | 0.051 106 | 0.003 960 | 0.259 571 | 0.020 961 | 0.036 872 | 0.000 906 | 256 | 89 | 234 | 8 | 233 | 3 | 99% |
Table 1 Zircon LA-ICP-MS U-Pb age data of Aqishan andesites, eastern Tianshan
点号 | Th/U | 同位素比值及误差 | 同位素年龄及误差/Ma | 谐和度 | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | |||
X13-7-01 | 0.24 | 0.057 373 | 0.002 365 | 0.417 526 | 0.023 298 | 0.053 330 | 0.002 433 | 506 | 44 | 354 | 8 | 335 | 7 | 94% |
X13-7-02 | 0.71 | 0.052 147 | 0.017 437 | 0.253 333 | 0.086 994 | 0.036 135 | 0.002 756 | 300 | 335 | 229 | 35 | 229 | 9 | 99% |
X13-7-04 | 0.55 | 0.052 103 | 0.003 396 | 0.269 417 | 0.017 671 | 0.037 713 | 0.000 801 | 300 | 74 | 242 | 7 | 239 | 2 | 98% |
X13-7-05 | 0.55 | 0.052 657 | 0.003 618 | 0.270 367 | 0.018 879 | 0.037 384 | 0.000 811 | 322 | 78 | 243 | 8 | 237 | 3 | 97% |
X13-7-06 | 1.29 | 0.051 660 | 0.008 490 | 0.253 090 | 0.038 878 | 0.036 029 | 0.001 235 | 333 | 186 | 229 | 16 | 228 | 4 | 99% |
X13-7-07 | 1.35 | 0.053 506 | 0.006 003 | 0.262 879 | 0.028 213 | 0.036 196 | 0.001 036 | 350 | 128 | 237 | 11 | 229 | 3 | 96% |
X13-7-08 | 0.59 | 0.051 497 | 0.001 973 | 0.265 711 | 0.010 643 | 0.037 447 | 0.000 647 | 265 | 44 | 239 | 4 | 237 | 2 | 99% |
X13-7-09 | 0.60 | 0.051 602 | 0.002 043 | 0.264 393 | 0.010 610 | 0.037 222 | 0.000 625 | 333 | 51 | 238 | 4 | 236 | 2 | 98% |
X13-7-11 | 0.81 | 0.053 987 | 0.006 006 | 0.278 562 | 0.030 109 | 0.038 064 | 0.001 090 | 372 | 131 | 250 | 12 | 241 | 3 | 96% |
X13-7-12 | 0.82 | 0.050 914 | 0.011 049 | 0.259 358 | 0.059 099 | 0.036 898 | 0.001 652 | 235 | 243 | 234 | 24 | 234 | 5 | 99% |
X13-7-13 | 0.53 | 0.056 223 | 0.010 844 | 0.278 892 | 0.049 480 | 0.036 182 | 0.001 579 | 461 | 215 | 250 | 20 | 229 | 5 | 91% |
X13-7-14 | 1.03 | 0.053 052 | 0.006 962 | 0.273 297 | 0.037 821 | 0.037 287 | 0.001 328 | 332 | 148 | 245 | 15 | 236 | 4 | 96% |
X13-7-15 | 1.05 | 0.051 304 | 0.004 904 | 0.260 538 | 0.022 196 | 0.036 873 | 0.001 301 | 254 | 111 | 235 | 9 | 233 | 4 | 99% |
X13-7-20 | 1.32 | 0.057 785 | 0.006 162 | 0.407 489 | 0.042 453 | 0.051 907 | 0.001 755 | 520 | 84 | 347 | 15 | 326 | 5 | 93% |
X13-7-21 | 0.58 | 0.053 930 | 0.005 637 | 0.391 467 | 0.039 063 | 0.052 954 | 0.002 376 | 369 | 114 | 335 | 14 | 333 | 7 | 99% |
X13-7-22 | 0.42 | 0.051 796 | 0.004 066 | 0.271 037 | 0.021 403 | 0.038 010 | 0.000 783 | 276 | 91 | 244 | 9 | 240 | 2 | 98% |
X13-7-23 | 0.47 | 0.051 106 | 0.003 960 | 0.259 571 | 0.020 961 | 0.036 872 | 0.000 906 | 256 | 89 | 234 | 8 | 233 | 3 | 99% |
点号 | wB/(μg·g-1) | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | ||
X13-7-01 | 18.22 | 130.83 | 24.13 | 149.75 | 98.56 | 35.29 | 153.24 | 38.39 | 301.19 | 80.45 | 303.53 | 59.95 | 545.15 | 88.82 | |
X13-7-02 | 97.46 | 192.27 | 19.28 | 75.84 | 17.31 | 1.54 | 29.90 | 7.64 | 78.37 | 30.27 | 137.27 | 31.76 | 325.61 | 63.13 | |
X13-7-04 | 0.24 | 24.86 | 0.18 | 2.27 | 4.52 | 1.27 | 26.49 | 9.30 | 117.75 | 46.58 | 212.97 | 51.24 | 512.89 | 87.81 | |
X13-7-05 | 0.03 | 24.48 | 0.13 | 1.98 | 4.67 | 1.21 | 27.23 | 9.51 | 119.18 | 47.23 | 215.24 | 51.80 | 519.80 | 88.99 | |
X13-7-06 | 0.15 | 49.77 | 0.39 | 6.75 | 11.22 | 4.64 | 50.73 | 14.18 | 150.77 | 50.18 | 204.66 | 42.77 | 386.32 | 65.77 | |
X13-7-07 | 0.16 | 50.02 | 0.44 | 7.00 | 11.66 | 4.97 | 51.10 | 14.30 | 153.54 | 50.86 | 204.62 | 42.85 | 382.61 | 66.16 | |
X13-7-08 | 0.06 | 21.86 | 0.10 | 2.13 | 5.27 | 0.71 | 38.13 | 13.70 | 171.14 | 67.12 | 298.42 | 67.53 | 661.17 | 111.62 | |
X13-7-09 | 0.05 | 21.77 | 0.10 | 2.20 | 5.17 | 0.71 | 38.13 | 13.63 | 169.96 | 66.39 | 294.41 | 66.72 | 653.99 | 109.95 | |
X13-7-11 | 0.01 | 14.70 | 0.18 | 3.11 | 4.89 | 1.82 | 24.14 | 7.50 | 83.41 | 30.23 | 130.08 | 29.68 | 292.11 | 50.31 | |
X13-7-12 | 0.01 | 15.15 | 0.23 | 3.56 | 4.83 | 1.77 | 23.54 | 8.47 | 87.46 | 32.69 | 141.49 | 31.86 | 314.79 | 55.11 | |
X13-7-13 | 0.55 | 12.18 | 0.78 | 5.50 | 4.16 | 1.06 | 26.61 | 9.12 | 112.99 | 47.22 | 220.98 | 47.97 | 456.08 | 80.78 | |
X13-7-14 | 2.12 | 91.98 | 0.57 | 4.31 | 6.42 | 1.99 | 32.97 | 10.22 | 118.75 | 42.42 | 183.30 | 42.39 | 406.49 | 71.33 | |
X13-7-15 | 2.83 | 103.42 | 0.77 | 4.91 | 5.45 | 2.07 | 35.31 | 11.61 | 124.09 | 45.35 | 193.52 | 44.58 | 431.26 | 74.75 | |
X13-7-20 | 4.19 | 36.61 | 1.91 | 12.76 | 10.21 | 3.48 | 58.38 | 20.26 | 260.53 | 100.84 | 444.84 | 96.06 | 892.23 | 147.59 | |
X13-7-21 | 0.01 | 13.50 | 0.08 | 0.76 | 1.75 | 0.52 | 15.14 | 6.48 | 86.72 | 38.95 | 196.53 | 51.47 | 576.62 | 100.48 | |
X13-7-22 | 1.78 | 17.54 | 0.83 | 5.71 | 7.00 | 1.34 | 28.25 | 9.27 | 101.64 | 35.31 | 153.45 | 33.32 | 309.06 | 53.77 | |
X13-7-23 | 1.32 | 18.49 | 0.75 | 5.55 | 7.49 | 1.62 | 31.42 | 10.15 | 113.27 | 38.81 | 160.78 | 35.82 | 331.86 | 54.58 |
Table 2 Zircon LA-ICP-MS REE data of Aqishan andesites, eastern Tianshan
点号 | wB/(μg·g-1) | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | ||
X13-7-01 | 18.22 | 130.83 | 24.13 | 149.75 | 98.56 | 35.29 | 153.24 | 38.39 | 301.19 | 80.45 | 303.53 | 59.95 | 545.15 | 88.82 | |
X13-7-02 | 97.46 | 192.27 | 19.28 | 75.84 | 17.31 | 1.54 | 29.90 | 7.64 | 78.37 | 30.27 | 137.27 | 31.76 | 325.61 | 63.13 | |
X13-7-04 | 0.24 | 24.86 | 0.18 | 2.27 | 4.52 | 1.27 | 26.49 | 9.30 | 117.75 | 46.58 | 212.97 | 51.24 | 512.89 | 87.81 | |
X13-7-05 | 0.03 | 24.48 | 0.13 | 1.98 | 4.67 | 1.21 | 27.23 | 9.51 | 119.18 | 47.23 | 215.24 | 51.80 | 519.80 | 88.99 | |
X13-7-06 | 0.15 | 49.77 | 0.39 | 6.75 | 11.22 | 4.64 | 50.73 | 14.18 | 150.77 | 50.18 | 204.66 | 42.77 | 386.32 | 65.77 | |
X13-7-07 | 0.16 | 50.02 | 0.44 | 7.00 | 11.66 | 4.97 | 51.10 | 14.30 | 153.54 | 50.86 | 204.62 | 42.85 | 382.61 | 66.16 | |
X13-7-08 | 0.06 | 21.86 | 0.10 | 2.13 | 5.27 | 0.71 | 38.13 | 13.70 | 171.14 | 67.12 | 298.42 | 67.53 | 661.17 | 111.62 | |
X13-7-09 | 0.05 | 21.77 | 0.10 | 2.20 | 5.17 | 0.71 | 38.13 | 13.63 | 169.96 | 66.39 | 294.41 | 66.72 | 653.99 | 109.95 | |
X13-7-11 | 0.01 | 14.70 | 0.18 | 3.11 | 4.89 | 1.82 | 24.14 | 7.50 | 83.41 | 30.23 | 130.08 | 29.68 | 292.11 | 50.31 | |
X13-7-12 | 0.01 | 15.15 | 0.23 | 3.56 | 4.83 | 1.77 | 23.54 | 8.47 | 87.46 | 32.69 | 141.49 | 31.86 | 314.79 | 55.11 | |
X13-7-13 | 0.55 | 12.18 | 0.78 | 5.50 | 4.16 | 1.06 | 26.61 | 9.12 | 112.99 | 47.22 | 220.98 | 47.97 | 456.08 | 80.78 | |
X13-7-14 | 2.12 | 91.98 | 0.57 | 4.31 | 6.42 | 1.99 | 32.97 | 10.22 | 118.75 | 42.42 | 183.30 | 42.39 | 406.49 | 71.33 | |
X13-7-15 | 2.83 | 103.42 | 0.77 | 4.91 | 5.45 | 2.07 | 35.31 | 11.61 | 124.09 | 45.35 | 193.52 | 44.58 | 431.26 | 74.75 | |
X13-7-20 | 4.19 | 36.61 | 1.91 | 12.76 | 10.21 | 3.48 | 58.38 | 20.26 | 260.53 | 100.84 | 444.84 | 96.06 | 892.23 | 147.59 | |
X13-7-21 | 0.01 | 13.50 | 0.08 | 0.76 | 1.75 | 0.52 | 15.14 | 6.48 | 86.72 | 38.95 | 196.53 | 51.47 | 576.62 | 100.48 | |
X13-7-22 | 1.78 | 17.54 | 0.83 | 5.71 | 7.00 | 1.34 | 28.25 | 9.27 | 101.64 | 35.31 | 153.45 | 33.32 | 309.06 | 53.77 | |
X13-7-23 | 1.32 | 18.49 | 0.75 | 5.55 | 7.49 | 1.62 | 31.42 | 10.15 | 113.27 | 38.81 | 160.78 | 35.82 | 331.86 | 54.58 |
点号 | Age/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | 2σ | (176Hf/177Hf)i | εHf(0) | εHf(t) | TDM/Ga | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|
X13-7-01 | 335 | 0.047 718 | 0.000 813 | 0.282 307 | 0.000 039 | 0.282 302 | -16.4 | -9.3 | 1.3 | -0.95 |
X13-7-08 | 237 | 0.116 360 | 0.002 023 | 0.282 267 | 0.000 044 | 0.282 258 | -17.9 | -13.0 | 1.4 | -0.87 |
X13-7-13 | 229 | 0.079 906 | 0.001 279 | 0.282 525 | 0.000 038 | 0.282 520 | -8.7 | -8.1 | 1.0 | -0.91 |
X13-7-14 | 236 | 0.132 003 | 0.002 149 | 0.282 421 | 0.000 039 | 0.282 412 | -12.4 | -7.6 | 1.2 | -0.86 |
X13-7-15 | 233 | 0.109 646 | 0.001 994 | 0.281 740 | 0.000 079 | 0.281 731 | -36.5 | -31.7 | 2.2 | -0.87 |
X13-7-20 | 326 | 0.288 233 | 0.004 642 | 0.282 796 | 0.000 060 | 0.282 768 | 0.8 | 7.0 | 0.7 | -0.69 |
X13-7-24 | 233 | 0.072 625 | 0.001 241 | 0.282 075 | 0.000 053 | 0.282 070 | -24.6 | -19.7 | 1.7 | -0.92 |
Table 3 Zircon LA-ICP-MS Hf isotopic data of Aqishan andesites, eastern Tianshan
点号 | Age/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | 2σ | (176Hf/177Hf)i | εHf(0) | εHf(t) | TDM/Ga | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|
X13-7-01 | 335 | 0.047 718 | 0.000 813 | 0.282 307 | 0.000 039 | 0.282 302 | -16.4 | -9.3 | 1.3 | -0.95 |
X13-7-08 | 237 | 0.116 360 | 0.002 023 | 0.282 267 | 0.000 044 | 0.282 258 | -17.9 | -13.0 | 1.4 | -0.87 |
X13-7-13 | 229 | 0.079 906 | 0.001 279 | 0.282 525 | 0.000 038 | 0.282 520 | -8.7 | -8.1 | 1.0 | -0.91 |
X13-7-14 | 236 | 0.132 003 | 0.002 149 | 0.282 421 | 0.000 039 | 0.282 412 | -12.4 | -7.6 | 1.2 | -0.86 |
X13-7-15 | 233 | 0.109 646 | 0.001 994 | 0.281 740 | 0.000 079 | 0.281 731 | -36.5 | -31.7 | 2.2 | -0.87 |
X13-7-20 | 326 | 0.288 233 | 0.004 642 | 0.282 796 | 0.000 060 | 0.282 768 | 0.8 | 7.0 | 0.7 | -0.69 |
X13-7-24 | 233 | 0.072 625 | 0.001 241 | 0.282 075 | 0.000 053 | 0.282 070 | -24.6 | -19.7 | 1.7 | -0.92 |
样品号 | 纬度 | 经度 | wB/% | K2O/Na2O | TFeO/MgO | Mg# | ||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SiO2 | Al2O3 | TFe2O3 | MgO | CaO | Na2O | K2O | MnO | TiO2 | P2O5 | LOI | Total | |||||||||||||||||||
X13-7 | 41°49'03″N | 90°48'46″E | 57.20 | 16.30 | 7.86 | 3.97 | 6.22 | 3.23 | 1.96 | 0.34 | 0.72 | 0.12 | 2.28 | 100.20 | 0.61 | 1.78 | 50.25 | |||||||||||||
X05-04 | 41°48'55″N | 90°48'41″E | 54.40 | 16.61 | 8.12 | 4.70 | 4.78 | 3.96 | 2.62 | 0.37 | 0.74 | 0.11 | 2.83 | 99.23 | 0.66 | 1.55 | 53.65 | |||||||||||||
X11-16 | 41°49'03″N | 90°48'45″E | 58.20 | 15.92 | 7.37 | 3.66 | 6.16 | 2.53 | 2.74 | 0.20 | 0.68 | 0.12 | 2.08 | 99.64 | 1.08 | 1.81 | 49.83 | |||||||||||||
样品号 | wB/(μg·g-1) | (La/Yb)N | δEu | |||||||||||||||||||||||||||
La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | ΣREE | ||||||||||||||||
X13-7 | 11.91 | 26.11 | 3.09 | 12.32 | 3.11 | 0.91 | 3.82 | 0.62 | 4.11 | 0.88 | 2.55 | 0.37 | 2.42 | 0.38 | 72.55 | 3.53 | 0.80 | |||||||||||||
X05-04 | 12.22 | 26.51 | 3.25 | 13.93 | 3.50 | 0.88 | 3.97 | 0.62 | 3.96 | 0.88 | 2.61 | 0.37 | 2.56 | 0.42 | 75.59 | 3.42 | 0.72 | |||||||||||||
X11-16 | 11.50 | 26.10 | 3.21 | 14.12 | 3.41 | 1.02 | 4.02 | 0.66 | 4.21 | 0.87 | 2.53 | 0.37 | 2.37 | 0.35 | 74.59 | 3.48 | 0.85 | |||||||||||||
样品号 | wB/(μg·g-1) | Sr/Y | Nb/Y | Ba/Rb | Rb/Sr | |||||||||||||||||||||||||
Rb | Ba | Th | U | Nb | Ta | Zr | Hf | Sr | Y | Pb | Cr | Ni | ||||||||||||||||||
X13-7 | 87.81 | 254.11 | 3.62 | 1.20 | 5.00 | 0.37 | 106.00 | 2.79 | 293.00 | 23.61 | 9.10 | 39.21 | 14.40 | 12.42 | 0.21 | 2.89 | 0.30 | |||||||||||||
X05-04 | 100.00 | 243.21 | 3.78 | 1.13 | 4.98 | 0.38 | 100.01 | 2.96 | 296.12 | 23.8.3 | 11.51 | 43.90 | 13.73 | 12.44 | 0.21 | 2.43 | 0.34 | |||||||||||||
X11-16 | 127.12 | 264.10 | 4.00 | 1.22 | 5.07 | 0.48 | 114.12 | 2.73 | 291.31 | 25.82 | 32.40 | 33.12 | 12.42 | 11.28 | 0.20 | 2.08 | 0.44 |
Table 4 Analytical results of petrochemical composition of Aqishan andesites, eastern Tianshan
样品号 | 纬度 | 经度 | wB/% | K2O/Na2O | TFeO/MgO | Mg# | ||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SiO2 | Al2O3 | TFe2O3 | MgO | CaO | Na2O | K2O | MnO | TiO2 | P2O5 | LOI | Total | |||||||||||||||||||
X13-7 | 41°49'03″N | 90°48'46″E | 57.20 | 16.30 | 7.86 | 3.97 | 6.22 | 3.23 | 1.96 | 0.34 | 0.72 | 0.12 | 2.28 | 100.20 | 0.61 | 1.78 | 50.25 | |||||||||||||
X05-04 | 41°48'55″N | 90°48'41″E | 54.40 | 16.61 | 8.12 | 4.70 | 4.78 | 3.96 | 2.62 | 0.37 | 0.74 | 0.11 | 2.83 | 99.23 | 0.66 | 1.55 | 53.65 | |||||||||||||
X11-16 | 41°49'03″N | 90°48'45″E | 58.20 | 15.92 | 7.37 | 3.66 | 6.16 | 2.53 | 2.74 | 0.20 | 0.68 | 0.12 | 2.08 | 99.64 | 1.08 | 1.81 | 49.83 | |||||||||||||
样品号 | wB/(μg·g-1) | (La/Yb)N | δEu | |||||||||||||||||||||||||||
La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | ΣREE | ||||||||||||||||
X13-7 | 11.91 | 26.11 | 3.09 | 12.32 | 3.11 | 0.91 | 3.82 | 0.62 | 4.11 | 0.88 | 2.55 | 0.37 | 2.42 | 0.38 | 72.55 | 3.53 | 0.80 | |||||||||||||
X05-04 | 12.22 | 26.51 | 3.25 | 13.93 | 3.50 | 0.88 | 3.97 | 0.62 | 3.96 | 0.88 | 2.61 | 0.37 | 2.56 | 0.42 | 75.59 | 3.42 | 0.72 | |||||||||||||
X11-16 | 11.50 | 26.10 | 3.21 | 14.12 | 3.41 | 1.02 | 4.02 | 0.66 | 4.21 | 0.87 | 2.53 | 0.37 | 2.37 | 0.35 | 74.59 | 3.48 | 0.85 | |||||||||||||
样品号 | wB/(μg·g-1) | Sr/Y | Nb/Y | Ba/Rb | Rb/Sr | |||||||||||||||||||||||||
Rb | Ba | Th | U | Nb | Ta | Zr | Hf | Sr | Y | Pb | Cr | Ni | ||||||||||||||||||
X13-7 | 87.81 | 254.11 | 3.62 | 1.20 | 5.00 | 0.37 | 106.00 | 2.79 | 293.00 | 23.61 | 9.10 | 39.21 | 14.40 | 12.42 | 0.21 | 2.89 | 0.30 | |||||||||||||
X05-04 | 100.00 | 243.21 | 3.78 | 1.13 | 4.98 | 0.38 | 100.01 | 2.96 | 296.12 | 23.8.3 | 11.51 | 43.90 | 13.73 | 12.44 | 0.21 | 2.43 | 0.34 | |||||||||||||
X11-16 | 127.12 | 264.10 | 4.00 | 1.22 | 5.07 | 0.48 | 114.12 | 2.73 | 291.31 | 25.82 | 32.40 | 33.12 | 12.42 | 11.28 | 0.20 | 2.08 | 0.44 |
[1] | XIAO W J, WINDLEY B F, HAN C M, et al. Late Paleozoic to early Triassic multiple roll-back and oroclinal bending of the Mongolia collage in Central Asia[J]. Earth-Science Reviews, 2018, 186: 94-128. |
[2] | XIAO W J, WINDLEY B F, SUN S, et al. A tale of amalgamation of three Permo-Triassic collage systems in Central Asia: oroclines, sutures, and terminal accretion[J]. Annual Review of Earth and Planetary Sciences, 2015, 43(1): 477-507. |
[3] | JAHN B M, GRIFFIN W L, WINDLEY B. Continental growth in the Phanerozoic: evidence from Central Asia[J]. Tectonophysics, 2000, 328(1/2): 7-10. |
[4] | CHEN Y J, CHEN H L, KHIN Z, et al. Geodynamic settings and tectonic model of skarn gold deposits in China: an overview[J]. Ore Geology Reviews, 2007, 31(1/2/3/4): 139-169. |
[5] | BUSLOV M M, WATANABE T, FUJIWARA Y, et al. Late Paleozoic faults of the Altai region, Central Asia: tectonic pattern and model of formation[J]. Journal of Asian Earth Sciences, 2004, 23(5): 655-671. |
[6] | CHARVET J, SHU L S, LAURENT-CHARVET S, et al. Palaeozoic tectonic evolution of the Tianshan belt, NW China[J]. Science China: Earth Sciences, 2011, 54(2): 166-184. |
[7] | HAN B F, HE G Q, WANG X C, et al. Late Carboniferous collision between the Tarim and Kazakhstan-Yili terranes in the western segment of the South Tian Shan Orogen, Central Asia, and implications for the Northern Xinjiang, western China[J]. Earth-Science Reviews, 2011, 109(3/4): 74-93. |
[8] | ZHANG F F, LIU J J, WANG Y H, et al. Zircon U-Pb and molybdenite Re-Os geochronology, Hf isotope analyses, and whole-rock geochemistry of the Donggebi Mo deposit, eastern Tianshan, Northwest China, and their geological significance[J]. International Geology Review, 2015, 57(4): 446-462. |
[9] | KAY R W. Aleutian magnesian andesites: melts from subducted Pacific ocean crust[J]. Journal of Volcanology and Geothermal Research, 1978, 4(1/2): 117-132. |
[10] | GAO S, RUDNICK R L, YUAN H L, et al. Recycling lower continental crust in the North China craton[J]. Nature, 2004, 432(7019): 892-897. |
[11] | SUN H S, LI H, DANIŠÍK M, et al. U-Pb and Re-Os geochronology and geochemistry of the Donggebi Mo deposit, Eastern Tianshan, NW China: insights into mineralization and tectonic setting[J]. Ore Geology Reviews, 2017, 86: 584-599. |
[12] | 肖序常. 新疆北部及其邻区大地构造[M]. 北京: 地质出版社, 1992: 1-178. |
[13] | HUANG X W, QI L, GAO J F, et al. First reliable Re-Os ages of pyrite and stable isotope compositions of Fe(-Cu) deposits in the Hami Region, Eastern Tianshan Orogenic Belt, NW China[J]. Resource Geology, 2013, 63(2): 166-187. |
[14] | 新疆维吾尔自治区地质矿产局. 新疆维吾尔自治区区域地质志[M]. 北京: 地质出版社, 1993: 1-841. |
[15] | XU X W, MA T L, SUN L Q, et al. Characteristics and dynamic origin of the large-scale Jiaoluotage ductile compressional zone in the eastern Tianshan Mountains, China[J]. Journal of Structural Geology, 2003, 25(11): 1901-1915. |
[16] | WANG B, CLUZEL D, JAHN B M, et al. Late Paleozoic pre- and syn-kinematic plutons of the Kangguer-Huangshan Shear zone: inference on the tectonic evolution of the eastern Chinese north Tianshan[J]. American Journal of Science, 2014, 314(1): 43-79. |
[17] | ZHANG L C, QIN K Z, XIAO W J. Multiple mineralization events in the eastern Tianshan district, NW China: isotopic geochronology and geological significance[J]. Journal of Asian Earth Sciences, 2008, 32(2/3/4): 236-246. |
[18] | XIAO W J, ZHANG L C, QIN K Z, et al. Paleozoic accretionary and collisional tectonics of the Eastern Tianshan (China): implications for the continental growth of central Asia[J]. American Journal of Science, 2004, 304(4): 370-395. |
[19] | 莫蒸. 东天山阿奇山地区帘石山火山机构及构造环境研究[D]. 北京: 中国地质大学(北京), 2016: 1-67. |
[20] | HAN C M, XIAO W J, ZHAO G C, et al. Major types, characteristics and geodynamic mechanism of Upper Paleozoic copper deposits in northern Xinjiang, northwestern China[J]. Ore Geology Reviews, 2007, 28(3): 308-328. |
[21] | 罗婷, 陈继平, 廖群安, 等. 东天山觉罗塔格构造带石炭纪弧后盆地: 来自基性火山岩的证据[J]. 地球科学, 2020, 45(1): 198-214. |
[22] | 宋彪, 张玉海, 万渝生, 等. 锆石SHRIMP样品靶制作、 年龄测定及有关现象讨论[J]. 地质论评, 2002, 48(增刊1): 26-30. |
[23] | 侯可军, 李延河, 邹天人, 等. LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用[J]. 岩石学报, 2007, 23(10): 2595-2604. |
[24] | LIU Y S, GAO S, GAO C G, et al. Garnet-rich granulite xenoliths from the Hannuoba basalts, North China: petrogenesis and implications for the Mesozoic crust-mantle interaction[J]. Journal of Earth Science, 2010, 21(5): 669-691. |
[25] | JACKSON S L, MAXWELL A, NEUMEISTER-KEMP H G, et al. Infection,hyperparasitism and conidiogenesis of Mycosphaerella lateralis on Eucalyptus globulus in Western Australia[J]. Australasian Plant Pathology, 2004, 33(1): 49-53. |
[26] | 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, 249(1/2): 1-35. |
[27] | LUDWIG K R. Users manual for ISOPLOT/EX, version 2. A geochronological toolkit for Microsoft Excel[M]. Los Angeles: Berkeley Geochronology Center, 2003: 1-71. |
[28] | CHU N C, TAYLOR R N, CHAVAGNAC V, et al. Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections[J]. Journal of Analytical Atomic Spectrometry, 2002, 17(12): 1567-1574. |
[29] | ELHLOU S, BELOUSOVA E, GRIFFIN W L, et al. Trace element and isotopic composition of GJ-red zircon standard by laser ablation[J]. Geochimica et Cosmochimica Acta, 2006, 70(S18): A158-A158. |
[30] | SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and source processes[J]. Geological Society, London, Special Publication, 1989, 42(1): 313-345. |
[31] | HOSKIN P W O. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1): 27-62. |
[32] | 雷如雄, 吴昌志, 张遵忠, 等. 东天山雅满苏北岩体的年代学、 地球化学及其构造意义[J]. 岩石学报, 2013, 29(8): 2653-2664. |
[33] | LEI R X, BRZOZOWSKI M J, FENG Y G, et al. Triassic crust-mantle interaction in the Eastern Tianshan, southern Altaids: insights from microgranular enclaves and their host Tianhu granitoids[J]. Lithos, 2020, 402/403: 105879. https://doi.org/10.1016/j.lithos.2020.105879. |
[34] | ZHAO L, CHEN H, HOLLINGS P, et al. Tectonic transition in the Aqishan-Yamansu belt, Eastern Tianshan: constraints from the geochronology and geochemistry of Carboniferous and Triassic igneous rocks[J]. Lithos, 2019, 344/345: 247-264. |
[35] | WANG Y H, ZHANG F F, LIU J J, et al. Carboniferous magmatism and mineralization in the area of the Fuxing Cu deposit, Eastern Tianshan, China: evidence from zircon U-Pb ages, petrogeochemistry, and Sr-Nd-Hf-O isotopic compositions[J]. Gondwana Research, 2016: 109-128. |
[36] | 庞博宸, 李秋根, 陈隽璐, 等. 东天山大南湖—头苏泉岛弧带古生代侵入岩浆活动期次及基底性质[J]. 西北地质, 2020, 53(2): 1-26. |
[37] | 宋鹏, 童英, 王涛, 等. 新疆东天山哈尔里克山石炭纪花岗岩锆石U-Pb年龄, 成因演化及地质意义[J]. 地质通报, 2018, 37(5): 790-804. |
[38] | WINCHESTER J A, FLOYD P A. Geochemical discrimination of different magma series and their differentiation products using immobile elements[J]. Chemical Geology, 1977, 20: 325-343. |
[39] | 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. |
[40] | FAHRIG W F, IRVING E, JACKSON G D. Paleomagnetism of the Franklin Diabases[J]. Canadian Journal of Earth Sciences, 1971, 8(4): 455-467. |
[41] | 邓晋福, 刘翠, 冯艳芳, 等. 高镁安山岩/闪长岩类(HMA)和镁安山岩/闪长岩类(MA): 与洋俯冲作用相关的两类典型的火成岩类[J]. 中国地质, 2010, 37(4): 1112-1118. |
[42] | RUDNICK R L, GAO S. The composition of the continental crust[M]. Oxford: Elsevier, 2003: 1-44. |
[43] | 李玮, 陈隽璐, 董云鹏, 等. 早古生代古亚洲洋俯冲记录: 来自东天山卡拉塔格高镁安山岩的年代学, 地球化学证据[J]. 岩石学报, 2016, 32(2): 505-521. |
[44] | ZHAO J H, ZHOU M F. Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district (Sichuan Province, SW China): implications for subduction-related metasomatism in the upper mantle[J]. Precambrian Research, 2007, 152(1/2): 27-47. |
[45] | POLAT A, HOFMANN A, WROSING M T. Boninite-like volcanic rocks in the 3.7-3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth[J]. Chemical Geology, 2002, 184: 231-254. |
[46] | POLAT A, HOFMANN A W. Alteration and geochemical patterns in the 3.7-3.8 Ga Isua greenstone belt, West Greenland[J]. Precambrian Research, 2003, 126: 197-218. |
[47] | WOOD B J, TURNER S P. Origin of primitive high-Mg andesite: constraints from natural examples and experiments[J]. Earth and Planetary Science Letters, 2009, 283(1/2/3/4): 59-66. |
[48] | GUO F, NAKAMURU E, FAN W, et al. Generation of Palaeocene adakitic andesites by magma mixing, Yanji area, NE China[J]. Journal of Petrology, 2007, 48(4): 661-692. |
[49] | TATSUMI Y, HANYU T. Geochemical modeling of dehydration and partial melting of subducting lithosphere: toward a comprehensive understanding of high-Mg andesite formation in the Setouchi volcanic belt, SW Japan[J]. Geochemistry, Geophysics, Geosystems, 2003, 4(9): 1081. |
[50] | STERN R A, HANSON G N. Archean high-Mg granodiorite: a derivative of light rare earth element-enriched monzodiorite of mantle origin[J]. Journal of Petrology, 1991, 32(1): 201-238. |
[51] | TATSUMI Y. Melting experiments on a high-magnesian andesite[J]. Earth and Planetary Science Letters, 1981, 54(2): 357-365. |
[52] | HONG D W, ZHANG J S, WANG T, et al. Continental crustal growth and the supercontinental cycle: evidence from the Central Asian Orogenic Belt[J]. Journal of Asian Earth Sciences, 2004, 23(5): 799-813. |
[53] | HOU T, ZHANG Z C, SANTOSH M, et al. Geochronology and geochemistry of submarine volcanic rocks in the Yamansu iron deposit, Eastern Tianshan Mountains, NW China: constraints on the metallogenesis[J]. Ore Geology Reviews, 2014, 56: 487-502. |
[54] | LUO T, LIAO Q A, ZHANG X H, et al. Geochronology and geochemistry of Carboniferous metabasalts in eastern Tianshan, Central Asia: evidence of a back-arc basin[J]. International Geology Review, 2016, 58(6): 1-18. |
[55] | XU J F, SHINJO R, DEFANT M J, et al. Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: partial melting of delaminated lower continental crust?[J]. Geology, 2002, 30(12): 1111-1114. |
[56] | CLASS C, MILLER D M, GOLDSTEIN S L, et al. Distinguishing melt and fluid subduction components in Umnak Volcanics, Aleutian Arc[J]. Geochemistry, Geophysics, Geosystems, 2000, 1(6): 1004. |
[57] | IONOV D A, GRIFFIN W L, O’REILLY S Y. Volatile-bearing minerals and lithophile trace elements in the upper mantle[J]. Chemical Geology, 1997, 141(3/4): 153-184. |
[58] | TURNER S, ARNAUD N, LIU J, et al. Post-collision, shoshonitic volcanism on the Tibetan Plateau: implications for convective thinning of the lithosphere and the source of ocean island basalts[J]. Journal of Petrology, 1996, 37(1): 45-71. |
[59] | WILLIAMS H M, TURNER S P, PEARCE J A, et al. Nature of the source regions for post-collisional, potassic magmatism in southern and northern Tibet from geochemical variations and inverse trace element modelling[J]. Journal of Petrology, 2004, 45(3): 555-607. |
[60] | 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. |
[61] | DU L, LONG X, YUAN C, et al. Petrogenesis of Late Paleozoic diorites and A-type granites in the central Eastern Tianshan, NW China: response to post-collisional extension triggered by slab breakoff[J]. Lithos, 2018, 318/319: 47-59. |
[62] | MCKENZIE D, O’NIONS R K. Partial melt distributions from inversion of rare earth element concentrations[J]. Journal of Petrology, 1991, 32(5): 1021-1091. |
[63] | ZHOU M F, LESHER C M, YANG Z, et al. Geochemistry and petrogenesis of 270 Ma Ni-Cu-(PGE) sulfide-bearing mafic intrusions in the Huangshan district, Eastern Xinjiang, Northwest China: implications for the tectonic evolution of the Central Asian orogenic belt[J]. Chemical Geology, 2004, 209(3/4): 233-257. |
[64] | 王银宏, 张方方, 刘家军, 等. 东天山白山钼矿区花岗岩的岩石成因: 锆石U-Pb年代学, 地球化学及Hf同位素约束[J]. 岩石学报, 2015, 31(7): 1962-1976. |
[65] | PEARCE J A, NORRY M J. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks[J]. Contributions to Mineralogy and Petrology, 1979, 69(1): 33-47. |
[66] | 汪云亮, 张成江, 修淑芝. 玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J]. 岩石学报, 2001, 17(3): 413-421. |
[67] | 张维峰, 陈华勇, 江宏君, 等. 新疆东天山多头山铁-铜矿区花岗岩类的年代学、 地球化学、 岩石成因及意义[J]. 大地构造与成矿学, 2017, 41(6): 1171-1191. |
[68] | 张旗, 潘国强, 李承东, 等. 花岗岩构造环境问题: 关于花岗岩研究的思考之三[J]. 岩石学报, 2007, 23(11): 2683-2698. |
[69] | CLEMENS J D, REGMI K, NICHOLLS I A, et al. The Tynong pluton, its mafic synplutonic sheets and igneous microgranular enclaves: the nature of the mantle connection in I-type granitic magmas[J]. Contributions to Mineralogy and Petrology, 2016, 171(4): 1-35. https://doi.org/10.1007/s00410-016-1251-y. |
[70] | 张遵忠, 顾连兴, 吴昌志, 等. 东天山印支早期尾亚石英正长岩: 成岩作用及成岩意义[J]. 岩石学报, 2006, 22(5): 1135-1149. |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||