Geoscience ›› 2021, Vol. 35 ›› Issue (02): 504-513.DOI: 10.19657/j.geoscience.1000-8527.2020.069
• Petrology • Previous Articles Next Articles
ZHANG Baotao1,2(), HU Zhaoguo1(
), JIANG Xiaoping1, WANG Xiangwei3, SUN Luwei3, ZHANG Yang1, WANG Xiaoyu1, ZHAO Xiaobo1, GUO Wei1
Received:
2019-07-19
Revised:
2020-06-22
Online:
2021-04-25
Published:
2021-05-25
Contact:
HU Zhaoguo
CLC Number:
ZHANG Baotao, HU Zhaoguo, JIANG Xiaoping, WANG Xiangwei, SUN Luwei, ZHANG Yang, WANG Xiaoyu, ZHAO Xiaobo, GUO Wei. Geochronological and Geochemical Characteristics of Tuanbaoshan Granite Pluton in Qinghai and Geological Implications[J]. Geoscience, 2021, 35(02): 504-513.
点 号 | 同位素比值 | 相关度 | 年龄/Ma | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | 238U/ 232Th | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | ||
1 | 0.063 | 0.002 | 1.115 | 0.041 | 0.128 | 0.002 | 0.49 | 0.92 | 718 | 78 | 760 | 20 | 774 | 13 |
2 | 0.066 | 0.002 | 1.165 | 0.038 | 0.128 | 0.002 | 0.54 | 0.80 | 806 | 64 | 785 | 18 | 779 | 13 |
3 | 0.086 | 0.002 | 1.109 | 0.038 | 0.092 | 0.002 | 0.57 | 19.33 | 1 344 | 48 | 758 | 18 | 566 | 11 |
4 | 0.072 | 0.002 | 1.280 | 0.033 | 0.128 | 0.002 | 0.55 | 1.89 | 991 | 50 | 837 | 15 | 775 | 10 |
5 | 0.065 | 0.001 | 1.104 | 0.025 | 0.122 | 0.002 | 0.6 | 1.37 | 776 | 46 | 755 | 12 | 742 | 10 |
6 | 0.062 | 0.002 | 1.112 | 0.034 | 0.128 | 0.002 | 0.61 | 1.12 | 687 | 54 | 759 | 16 | 775 | 14 |
7 | 0.066 | 0.003 | 1.169 | 0.046 | 0.128 | 0.004 | 0.70 | 0.84 | 809 | 91 | 786 | 21 | 774 | 20 |
8 | 0.116 | 0.003 | 2.061 | 0.085 | 0.127 | 0.004 | 0.81 | 2.96 | 1 894 | 43 | 1 136 | 28 | 772 | 24 |
9 | 0.134 | 0.003 | 1.730 | 0.060 | 0.092 | 0.002 | 0.76 | 1.76 | 2 152 | 43 | 1 020 | 22 | 570 | 14 |
10 | 0.152 | 0.003 | 4.957 | 0.162 | 0.233 | 0.006 | 0.78 | 2.75 | 2 366 | 32 | 1 812 | 28 | 1 352 | 31 |
11 | 0.067 | 0.003 | 1.200 | 0.066 | 0.128 | 0.003 | 0.42 | 1.23 | 844 | 101 | 801 | 31 | 777 | 17 |
12 | 0.094 | 0.004 | 0.947 | 0.038 | 0.073 | 0.001 | 0.50 | 1.58 | 1 517 | 75 | 677 | 20 | 451 | 9 |
13 | 0.085 | 0.003 | 1.463 | 0.036 | 0.128 | 0.002 | 0.58 | 4.35 | 1 322 | 73 | 915 | 15 | 775 | 11 |
14 | 0.069 | 0.005 | 1.221 | 0.086 | 0.129 | 0.003 | 0.36 | 1.93 | 894 | 150 | 810 | 40 | 781 | 19 |
15 | 0.070 | 0.002 | 1.244 | 0.044 | 0.129 | 0.003 | 0.68 | 0.52 | 939 | 69 | 821 | 20 | 779 | 18 |
16 | 0.066 | 0.002 | 1.169 | 0.039 | 0.128 | 0.004 | 0.82 | 2.43 | 813 | 59 | 786 | 18 | 778 | 20 |
17 | 0.111 | 0.006 | 1.996 | 0.127 | 0.129 | 0.003 | 0.34 | 0.66 | 1 809 | 99 | 1 114 | 43 | 780 | 16 |
18 | 0.181 | 0.019 | 2.678 | 0.364 | 0.093 | 0.004 | 0.28 | 5.61 | 2 665 | 172 | 1 322 | 101 | 571 | 21 |
Table 1 LA-ICP-MS zircon U-Pb dating results of the Tuanbaoshan granite
点 号 | 同位素比值 | 相关度 | 年龄/Ma | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | 238U/ 232Th | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | ||
1 | 0.063 | 0.002 | 1.115 | 0.041 | 0.128 | 0.002 | 0.49 | 0.92 | 718 | 78 | 760 | 20 | 774 | 13 |
2 | 0.066 | 0.002 | 1.165 | 0.038 | 0.128 | 0.002 | 0.54 | 0.80 | 806 | 64 | 785 | 18 | 779 | 13 |
3 | 0.086 | 0.002 | 1.109 | 0.038 | 0.092 | 0.002 | 0.57 | 19.33 | 1 344 | 48 | 758 | 18 | 566 | 11 |
4 | 0.072 | 0.002 | 1.280 | 0.033 | 0.128 | 0.002 | 0.55 | 1.89 | 991 | 50 | 837 | 15 | 775 | 10 |
5 | 0.065 | 0.001 | 1.104 | 0.025 | 0.122 | 0.002 | 0.6 | 1.37 | 776 | 46 | 755 | 12 | 742 | 10 |
6 | 0.062 | 0.002 | 1.112 | 0.034 | 0.128 | 0.002 | 0.61 | 1.12 | 687 | 54 | 759 | 16 | 775 | 14 |
7 | 0.066 | 0.003 | 1.169 | 0.046 | 0.128 | 0.004 | 0.70 | 0.84 | 809 | 91 | 786 | 21 | 774 | 20 |
8 | 0.116 | 0.003 | 2.061 | 0.085 | 0.127 | 0.004 | 0.81 | 2.96 | 1 894 | 43 | 1 136 | 28 | 772 | 24 |
9 | 0.134 | 0.003 | 1.730 | 0.060 | 0.092 | 0.002 | 0.76 | 1.76 | 2 152 | 43 | 1 020 | 22 | 570 | 14 |
10 | 0.152 | 0.003 | 4.957 | 0.162 | 0.233 | 0.006 | 0.78 | 2.75 | 2 366 | 32 | 1 812 | 28 | 1 352 | 31 |
11 | 0.067 | 0.003 | 1.200 | 0.066 | 0.128 | 0.003 | 0.42 | 1.23 | 844 | 101 | 801 | 31 | 777 | 17 |
12 | 0.094 | 0.004 | 0.947 | 0.038 | 0.073 | 0.001 | 0.50 | 1.58 | 1 517 | 75 | 677 | 20 | 451 | 9 |
13 | 0.085 | 0.003 | 1.463 | 0.036 | 0.128 | 0.002 | 0.58 | 4.35 | 1 322 | 73 | 915 | 15 | 775 | 11 |
14 | 0.069 | 0.005 | 1.221 | 0.086 | 0.129 | 0.003 | 0.36 | 1.93 | 894 | 150 | 810 | 40 | 781 | 19 |
15 | 0.070 | 0.002 | 1.244 | 0.044 | 0.129 | 0.003 | 0.68 | 0.52 | 939 | 69 | 821 | 20 | 779 | 18 |
16 | 0.066 | 0.002 | 1.169 | 0.039 | 0.128 | 0.004 | 0.82 | 2.43 | 813 | 59 | 786 | 18 | 778 | 20 |
17 | 0.111 | 0.006 | 1.996 | 0.127 | 0.129 | 0.003 | 0.34 | 0.66 | 1 809 | 99 | 1 114 | 43 | 780 | 16 |
18 | 0.181 | 0.019 | 2.678 | 0.364 | 0.093 | 0.004 | 0.28 | 5.61 | 2 665 | 172 | 1 322 | 101 | 571 | 21 |
样号 | SiO2 | Al2O3 | Fe2O3 | FeO | MgO | CaO | Na2O | K2O | TiO2 | P2O5 | MnO | Na2O+ K2O | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
HF-1 | 74.33 | 13.81 | 1.73 | 1.45 | 0.24 | 0.80 | 3.42 | 4.99 | 0.07 | 0.15 | 0.05 | 8.41 | |||||||||||||
HF-2 | 72.93 | 13.30 | 2.05 | 1.69 | 0.30 | 1.41 | 3.17 | 5.65 | 0.14 | 0.08 | 0.04 | 8.82 | |||||||||||||
HF-3 | 74.14 | 13.81 | 1.76 | 1.47 | 0.21 | 0.91 | 3.29 | 5.14 | 0.08 | 0.06 | 0.04 | 8.43 | |||||||||||||
HF-4 | 74.11 | 13.72 | 1.75 | 1.59 | 0.19 | 0.93 | 3.21 | 4.72 | 0.07 | 0.14 | 0.05 | 7.93 | |||||||||||||
HF-5 | 74.55 | 13.59 | 1.45 | 1.21 | 0.15 | 0.47 | 4.71 | 4.46 | 0.03 | 0.28 | 0.13 | 9.17 | |||||||||||||
HF-6 | 73.18 | 13.41 | 2.31 | 1.69 | 0.38 | 0.83 | 2.84 | 6.11 | 0.19 | 0.11 | 0.04 | 8.95 | |||||||||||||
样号 | 里特曼 指数 | A/NK | A/CNK | FeOT | 固结指数 (SI) | 碱度率 (AR) | La | Ce | Pr | Nd | Sm | Eu | |||||||||||||
HF-1 | 2.27 | 1.64 | 1.50 | 2.98 | 2.03 | 3.71 | 11.74 | 30.61 | 3.15 | 10.20 | 2.72 | 0.39 | |||||||||||||
HF-2 | 2.61 | 1.51 | 1.30 | 3.51 | 2.33 | 3.99 | 28.73 | 78.80 | 8.23 | 26.65 | 5.54 | 0.62 | |||||||||||||
HF-3 | 2.29 | 1.64 | 1.48 | 3.03 | 1.73 | 3.68 | 17.34 | 39.22 | 4.16 | 13.50 | 2.61 | 0.44 | |||||||||||||
HF-4 | 2.02 | 1.73 | 1.55 | 3.16 | 1.64 | 3.36 | 10.44 | 25.05 | 2.69 | 9.15 | 1.96 | 0.46 | |||||||||||||
HF-5 | 2.68 | 1.48 | 1.41 | 2.49 | 1.25 | 4.75 | 2.07 | 4.74 | 0.57 | 2.00 | 0.60 | 0.14 | |||||||||||||
HF-6 | 2.67 | 1.50 | 1.37 | 3.73 | 2.85 | 4.38 | 35.09 | 98.49 | 10.46 | 34.97 | 7.63 | 0.70 | |||||||||||||
样号 | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | δEu | δCe | (Sm/ Nd)N | LREE | |||||||||||||
HF-1 | 2.97 | 0.54 | 3.27 | 0.61 | 1.75 | 0.25 | 1.83 | 0.25 | 2.72 | 1.19 | 0.82 | 137.83 | |||||||||||||
HF-2 | 5.15 | 0.70 | 3.55 | 0.65 | 1.79 | 0.26 | 1.80 | 0.25 | 5.54 | 1.22 | 0.64 | 338.93 | |||||||||||||
HF-3 | 2.63 | 0.41 | 2.40 | 0.46 | 1.34 | 0.21 | 1.37 | 0.20 | 2.61 | 1.08 | 0.59 | 180.41 | |||||||||||||
HF-4 | 2.11 | 0.38 | 2.27 | 0.43 | 1.22 | 0.19 | 1.18 | 0.17 | 1.96 | 1.11 | 0.66 | 118.28 | |||||||||||||
HF-5 | 0.69 | 0.13 | 0.73 | 0.11 | 0.32 | 0.05 | 0.41 | 0.06 | 0.60 | 1.03 | 0.93 | 25.52 | |||||||||||||
HF-6 | 6.63 | 0.84 | 3.89 | 0.66 | 1.76 | 0.24 | 1.57 | 0.21 | 7.63 | 1.23 | 0.67 | 427.67 | |||||||||||||
样号 | δCe | (Sm/ Nd)N | HREE | REE | LREE/ HREE | (La/ Yb)N | Rb | Ba | Th | Ta | Hf | Zr | Sr | Y | |||||||||||
HF-1 | 1.19 | 0.82 | 73.95 | 211.78 | 1.86 | 4.34 | 292 | 373 | 25.20 | 3.00 | 3.23 | 99.10 | 82.50 | 23.60 | |||||||||||
HF-2 | 1.22 | 0.64 | 87.41 | 426.34 | 3.88 | 10.76 | 304 | 185 | 9.23 | 4.04 | 2.33 | 41.60 | 44.00 | 16.50 | |||||||||||
HF-3 | 1.08 | 0.59 | 58.30 | 238.71 | 3.09 | 8.55 | 163 | 217 | 13.43 | 3.39 | 4.46 | 62.13 | 63.84 | — | |||||||||||
HF-4 | 1.11 | 0.66 | 51.58 | 169.87 | 2.29 | 5.94 | 211 | 320 | 9.48 | 3.13 | 3.57 | 59.47 | 58.55 | — | |||||||||||
HF-5 | 1.03 | 0.93 | 16.14 | 41.66 | 1.58 | 3.38 | 281 | 29 | 0.94 | 5.06 | 2.54 | 12.30 | 13.00 | 6.02 | |||||||||||
HF-6 | 1.23 | 0.67 | 94.24 | 521.91 | 4.54 | 15.05 | 359 | 331 | 28.60 | 3.23 | 2.64 | 128.00 | 81.70 | 21.40 | |||||||||||
HF-7 | — | — | — | — | — | — | 211 | 817 | 20.40 | 2.02 | 4.09 | 211.00 | 125.00 | 24.10 |
Table 2 Major (%), rare earth element and trace (10-6) analysis results for the Tuanbaoshan granite
样号 | SiO2 | Al2O3 | Fe2O3 | FeO | MgO | CaO | Na2O | K2O | TiO2 | P2O5 | MnO | Na2O+ K2O | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
HF-1 | 74.33 | 13.81 | 1.73 | 1.45 | 0.24 | 0.80 | 3.42 | 4.99 | 0.07 | 0.15 | 0.05 | 8.41 | |||||||||||||
HF-2 | 72.93 | 13.30 | 2.05 | 1.69 | 0.30 | 1.41 | 3.17 | 5.65 | 0.14 | 0.08 | 0.04 | 8.82 | |||||||||||||
HF-3 | 74.14 | 13.81 | 1.76 | 1.47 | 0.21 | 0.91 | 3.29 | 5.14 | 0.08 | 0.06 | 0.04 | 8.43 | |||||||||||||
HF-4 | 74.11 | 13.72 | 1.75 | 1.59 | 0.19 | 0.93 | 3.21 | 4.72 | 0.07 | 0.14 | 0.05 | 7.93 | |||||||||||||
HF-5 | 74.55 | 13.59 | 1.45 | 1.21 | 0.15 | 0.47 | 4.71 | 4.46 | 0.03 | 0.28 | 0.13 | 9.17 | |||||||||||||
HF-6 | 73.18 | 13.41 | 2.31 | 1.69 | 0.38 | 0.83 | 2.84 | 6.11 | 0.19 | 0.11 | 0.04 | 8.95 | |||||||||||||
样号 | 里特曼 指数 | A/NK | A/CNK | FeOT | 固结指数 (SI) | 碱度率 (AR) | La | Ce | Pr | Nd | Sm | Eu | |||||||||||||
HF-1 | 2.27 | 1.64 | 1.50 | 2.98 | 2.03 | 3.71 | 11.74 | 30.61 | 3.15 | 10.20 | 2.72 | 0.39 | |||||||||||||
HF-2 | 2.61 | 1.51 | 1.30 | 3.51 | 2.33 | 3.99 | 28.73 | 78.80 | 8.23 | 26.65 | 5.54 | 0.62 | |||||||||||||
HF-3 | 2.29 | 1.64 | 1.48 | 3.03 | 1.73 | 3.68 | 17.34 | 39.22 | 4.16 | 13.50 | 2.61 | 0.44 | |||||||||||||
HF-4 | 2.02 | 1.73 | 1.55 | 3.16 | 1.64 | 3.36 | 10.44 | 25.05 | 2.69 | 9.15 | 1.96 | 0.46 | |||||||||||||
HF-5 | 2.68 | 1.48 | 1.41 | 2.49 | 1.25 | 4.75 | 2.07 | 4.74 | 0.57 | 2.00 | 0.60 | 0.14 | |||||||||||||
HF-6 | 2.67 | 1.50 | 1.37 | 3.73 | 2.85 | 4.38 | 35.09 | 98.49 | 10.46 | 34.97 | 7.63 | 0.70 | |||||||||||||
样号 | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | δEu | δCe | (Sm/ Nd)N | LREE | |||||||||||||
HF-1 | 2.97 | 0.54 | 3.27 | 0.61 | 1.75 | 0.25 | 1.83 | 0.25 | 2.72 | 1.19 | 0.82 | 137.83 | |||||||||||||
HF-2 | 5.15 | 0.70 | 3.55 | 0.65 | 1.79 | 0.26 | 1.80 | 0.25 | 5.54 | 1.22 | 0.64 | 338.93 | |||||||||||||
HF-3 | 2.63 | 0.41 | 2.40 | 0.46 | 1.34 | 0.21 | 1.37 | 0.20 | 2.61 | 1.08 | 0.59 | 180.41 | |||||||||||||
HF-4 | 2.11 | 0.38 | 2.27 | 0.43 | 1.22 | 0.19 | 1.18 | 0.17 | 1.96 | 1.11 | 0.66 | 118.28 | |||||||||||||
HF-5 | 0.69 | 0.13 | 0.73 | 0.11 | 0.32 | 0.05 | 0.41 | 0.06 | 0.60 | 1.03 | 0.93 | 25.52 | |||||||||||||
HF-6 | 6.63 | 0.84 | 3.89 | 0.66 | 1.76 | 0.24 | 1.57 | 0.21 | 7.63 | 1.23 | 0.67 | 427.67 | |||||||||||||
样号 | δCe | (Sm/ Nd)N | HREE | REE | LREE/ HREE | (La/ Yb)N | Rb | Ba | Th | Ta | Hf | Zr | Sr | Y | |||||||||||
HF-1 | 1.19 | 0.82 | 73.95 | 211.78 | 1.86 | 4.34 | 292 | 373 | 25.20 | 3.00 | 3.23 | 99.10 | 82.50 | 23.60 | |||||||||||
HF-2 | 1.22 | 0.64 | 87.41 | 426.34 | 3.88 | 10.76 | 304 | 185 | 9.23 | 4.04 | 2.33 | 41.60 | 44.00 | 16.50 | |||||||||||
HF-3 | 1.08 | 0.59 | 58.30 | 238.71 | 3.09 | 8.55 | 163 | 217 | 13.43 | 3.39 | 4.46 | 62.13 | 63.84 | — | |||||||||||
HF-4 | 1.11 | 0.66 | 51.58 | 169.87 | 2.29 | 5.94 | 211 | 320 | 9.48 | 3.13 | 3.57 | 59.47 | 58.55 | — | |||||||||||
HF-5 | 1.03 | 0.93 | 16.14 | 41.66 | 1.58 | 3.38 | 281 | 29 | 0.94 | 5.06 | 2.54 | 12.30 | 13.00 | 6.02 | |||||||||||
HF-6 | 1.23 | 0.67 | 94.24 | 521.91 | 4.54 | 15.05 | 359 | 331 | 28.60 | 3.23 | 2.64 | 128.00 | 81.70 | 21.40 | |||||||||||
HF-7 | — | — | — | — | — | — | 211 | 817 | 20.40 | 2.02 | 4.09 | 211.00 | 125.00 | 24.10 |
[1] | 雍拥, 肖文交, 袁超, 等. 中祁连东段古生代花岗岩的年代学、地球化学特征及其大地构造意义[J]. 岩石学报, 2008,24(4):855-866. |
[2] | 许志琴, 徐惠芬, 张建新, 等. 北祁连走廊南山加里东俯冲杂岩增生地体及其动力学[J]. 地质学报, 1994,68(1):1-14. |
[3] | 冯益民, 何世平. 北祁连蛇绿岩的地质地球化学研究[J]. 岩石学报, 1995,11(增):125-146. |
[4] | 冯益民, 何世平. 祁连山大地构造与造山作用[M]. 北京: 地质出版社, 1996. |
[5] |
SOBEL E R, ARNAUD N. A possible Middle Paleozoic suture in the Altyn Tagh, NW China[J]. Tectonics, 1999,18(1):64-74.
DOI URL |
[6] |
YIN A, HARRISON T M. Geological evolution of the Himalayan-Tibetan Orogen[J]. Annual Review of Earth and Planetary Sciences, 2000,28(1):211-280.
DOI URL |
[7] |
XIAO W J, WINDLEY B F, LIU D Y, et al. Accretionary tectonics of the western Kunlun orogen, China: A Paleozoic-Early Mesozoic, long-lived active continental margin with implications for the growth of southern Eurasia[J]. Journal of Geology, 2005,113(6):687-705.
DOI URL |
[8] |
YUAN C, SUN M, ZHOU M F, et al. Geochemistry and petrogenesis of the Yishak volcanic sequence, Kudi ophiolite, West Kunlun (NW China): Implications for the magmatic evolution in a subduction zone environment[J]. Contributions to Mineralogy and Petrology, 2005,150(2):195-211.
DOI URL |
[9] | 张宏飞, 靳兰兰, 张利, 等. 基底岩系和花岗岩类Pb-Nd同位素组成限制祁连山带的构造属性[J]. 地球科学, 2006,31(1):57-65. |
[10] |
SONG S G, ZHANG L F, NIU Y, et al. Evolution from oceanic subduction to continental collision: a case study from the Northern Tibetan Plateau based on geochemical and geochronological data[J]. Journal of Petrology, 2006,47(3):435-455.
DOI URL |
[11] | 董国安, 杨怀仁, 杨宏仪, 等. 祁连地块前寒武纪基底锆石SHRIMP U-Pb年代学及其地质意义[J]. 科学通报, 2007,52(13):1572-1585. |
[12] | 李建锋, 张志诚, 韩宝福. 中祁连西段肃北、石包城地区早古生代花岗岩年代学、地球化学特征及其地质意义[J]. 岩石学报, 2010,26(8):2431-2444. |
[13] | 冯益民. 祁连造山带研究概况——历史、现状及展望[J]. 地球科学进展, 1997,12(4):307-314. |
[14] | 肖序常, 陈国铭, 朱志直. 祁连山古蛇绿岩带的地质构造意义[J]. 地质学报, 1978,52(4):281-295. |
[15] | 胡万龙, 贾志磊, 王金荣, 等. 南祁连化石沟花岗岩年代学、地球化学特征及其构造意义[J]. 高校地质学报, 2016,22(2):242-253. |
[16] | 毛景文, 张作衡, 简平, 等. 北祁连西段花岗质岩体的锆石U-Pb年龄报道[J]. 地质论评, 2000,46(6):616-620. |
[17] | 王晓地, 汪雄武, 杨伟, 等. 北祁连西段加里东期花岗岩类与钨成矿作用的关系浅议[J]. 华南地质与矿产, 2004,20(1):17-23. |
[18] | 吴才来, 徐学义, 高前明, 等. 北祁连早古生代花岗质岩浆作用及构造演化[J]. 岩石学报, 2010,26(4):1027-1044. |
[19] | 吴才来, 杨经绥, 杨宏仪, 等. 北祁连东部两类Ⅰ型花岗岩定年及其地质意义[J]. 岩石学报, 2004,20(3):425-432. |
[20] | CHEN Y X, SONG S G, NIU Y L, et al. Melting of continental crust during subduction initiation: A case study from the Chaida-nuo peraluminous granite in the North Qilian suture zone[J]. Geochimica et Cosmochimica Acta, 2014,132:311-336. |
[21] |
CHEN Y X, XIA X H, SONG S G. Petrogenesis of Aoyougou high-silica adakite in the North Qilian orogen, NW China: evidence for decompression melting of oceanic slab[J]. Chinese Science Bulletin, 2012,57(18):2289-2301.
DOI URL |
[22] | 马建军, 王珩, 何川, 等. 南祁连造山带新元古代后碰撞岩浆作用:年代学和地球化学证据[J]. 地球科学与环境学报, 2018,40(2):133-154. |
[23] |
ANDERSEN T. Correction of common lead in U-Pb analyses that do not report204Pb[J]. Chemical Geology, 2002,192(1/2):59-79.
DOI URL |
[24] |
SUN S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989,42(1):313-345.
DOI URL |
[25] | CHAPPEL B W, WHITE A J R . Two contrasting granite types[J]. Pacific Geology, 1974,8:173-174. |
[26] | 邱家骧, 林景仟. 岩石化学[M]. 北京: 地质出版社, 1991: 203-210. |
[27] | 康伟浩, 任二峰, 高亮. 青海南祁连东段化隆岩群时代重新厘定及地质意义[J]. 青海大学学报, 2016,34(5):52-57. |
[28] |
MIDDLEMOST E A K. Naming materials in the magma/igneous rocks system[J]. Earth-Science Reviews, 1994,37(3/4):215-224.
DOI URL |
[29] |
MANIAR P D, PICCOLI P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989,101(5):635-643.
DOI URL |
[30] |
SYLVESTER P J. Post-collisional strongly peraluminous granites[J]. Lithos, 1998,45:29-44.
DOI URL |
[31] |
GERDES A, WORNER G, HENK A. Post-collisional granite generation and HT-LP metamorphism by radiogenic heating: the example from the Variscan South Bohemian Batholith[J]. Journal of the Geological Society, London, 2000,157:577-587.
DOI URL |
[32] |
BATCHELOR R A, BOWDEN P. Petrogenetic interpretation of granitoid rock series using multicationic parameters[J]. Chemical Geology, 1985,48:43-55.
DOI URL |
[33] |
PEARCE J A, HARRIS N B W, TINDLE A G . Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984,25(4):956-983.
DOI URL |
[34] | 孟繁聪, 崔美慧, 吴祥珂, 等. 东昆仑祁漫塔格花岗片麻岩记录的岩浆和变质事件[J]. 岩石学报, 2013,29(6):2107-2122. |
[35] | 陈有炘, 裴先治, 李佐臣, 等. 东昆仑东段巴隆花岗质片麻岩年代学、地球化学特征及地质意义[J]. 岩石学报, 2015,31(8):2230-2244. |
[36] | 李冰, 胡道功, 陈宣华, 等. 北祁连缝合带油葫芦沟蛇绿岩中花岗斑岩锆石U-Pb年龄及地质意义[J]. 现代地质, 2017,31(6):1170-1176. |
[37] | 黄汲清. 试论地槽褶皱带的多旋迴发展[J]. 中国科学, 1979,19(4):384-397. |
[38] | 李春昱, 刘仰文, 朱宝清, 等. 秦岭及祁连山构造发展史[J]. 西北地质, 1978, ( 4):1-12. |
[39] | 沈宝坪, 张起振, 沈延忠, 等. 1∶20万湟源幅区域地质说明书[M]. 西宁: 青海省地质局, 1965: 37-50. |
[40] | 拜永山, 王秉璋, 王永文, 等. 1:25万西宁幅区域地质调查报告[M]. 西宁: 青海省地质调查院, 2007: 148-189. |
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