Geoscience ›› 2017, Vol. 31 ›› Issue (06): 1095-1113.
• Ore Deposits • Previous Articles Next Articles
YU Chao1(), LIU Zhenjiang1(
), MI Kuifeng1, WANG Changbo2, ZHANG Jie2, WANG Jianping1, LIU Jiajun1, ZHANG Mei3
Received:
2017-03-15
Revised:
2017-07-07
Online:
2017-12-10
Published:
2017-12-25
CLC Number:
YU Chao, LIU Zhenjiang, MI Kuifeng, WANG Changbo, ZHANG Jie, WANG Jianping, LIU Jiajun, ZHANG Mei. U-Pb Zircon, Geochemical and Hf Isotopic Constraints on Origin of the Bayandulan Copper Deposit, Inner Mongolia, China[J]. Geoscience, 2017, 31(06): 1095-1113.
样品编号 | 岩性 | SiO2 | TiO2 | Al2O3 | FeO | Fe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
BL1-1 | 黑云母二 长花岗岩 | 70.39 | 0.41 | 14.99 | 2.26 | 0.46 | 0.05 | 0.79 | 0.48 | 4.50 | 4.28 | 0.11 | (0.06) | 98.66 | |||||||||||
BL1-2 | 69.16 | 0.38 | 15.32 | 2.07 | 0.46 | 0.05 | 0.71 | 1.20 | 4.09 | 4.36 | 0.10 | 0.84 | 98.74 | ||||||||||||
BL-Z1 | 68.33 | 0.40 | 15.44 | 2.29 | 0.58 | 0.05 | 0.51 | 1.20 | 4.16 | 4.77 | 0.09 | 1.26 | 99.06 | ||||||||||||
BL-Z2 | 68.69 | 0.44 | 15.55 | 2.20 | 0.93 | 0.08 | 0.93 | 2.00 | 3.94 | 4.01 | 0.11 | 0.87 | 99.75 | ||||||||||||
BL-Z1BT | 暗色微粒 包体 | 52.49 | 1.34 | 17.54 | 8.35 | 2.33 | 0.22 | 3.45 | 3.35 | 4.33 | 2.07 | 0.35 | 2.82 | 97.15 | |||||||||||
BL-Z2BT | 52.65 | 1.34 | 17.57 | 8.20 | 2.51 | 0.23 | 3.46 | 3.35 | 4.33 | 2.07 | 0.35 | 2.77 | 97.38 | ||||||||||||
4437-1 | 二长花岗 岩 | 72.44 | 0.15 | 15.52 | 0.12 | 0.74 | 0.10 | 0.24 | 0.67 | 4.83 | 4.26 | 0.07 | 0.67 | 99.81 | |||||||||||
4437-2 | 74.22 | 0.13 | 14.71 | 0.20 | 0.54 | 0.08 | 0.20 | 0.59 | 4.35 | 4.28 | 0.06 | 0.52 | 99.88 | ||||||||||||
4437-3 | 73.59 | 0.17 | 14.56 | 0.47 | 0.92 | 0.10 | 0.36 | 1.01 | 4.48 | 3.57 | 0.09 | 0.65 | 99.97 | ||||||||||||
4437-4 | 71.56 | 0.15 | 16.38 | 0.18 | 0.65 | 0.07 | 0.21 | 0.58 | 4.94 | 4.35 | 0.05 | 0.74 | 99.86 | ||||||||||||
样品编号 | 岩性 | Rb | Ba | Th | U | Nb | Ta | La | Ce | Pr | Sr | Nd | Sm | ||||||||||||
BL1-1 | 黑云母二 长花岗岩 | 113.50 | 892.00 | 14.10 | 2.30 | 10.20 | 1.20 | 24.50 | 52.20 | 5.93 | 205.00 | 22.10 | 5.56 | ||||||||||||
BL1-2 | 122.00 | 917.00 | 13.95 | 2.71 | 9.90 | 1.20 | 34.20 | 69.70 | 7.44 | 354.00 | 27.60 | 5.88 | |||||||||||||
BL-Z1 | 117.50 | 817.00 | 10.55 | 7.76 | 8.90 | 0.70 | 48.50 | 95.40 | 10.80 | 229.00 | 39.80 | 6.85 | |||||||||||||
BL-Z2 | 165.50 | 615.00 | 14.90 | 8.17 | 11.90 | 1.70 | 26.70 | 51.20 | 6.38 | 256.00 | 24.60 | 5.05 | |||||||||||||
BL-Z1BT | 暗色微粒 包体 | 212.00 | 161.50 | 11.25 | 20.20 | 23.70 | 1.30 | 45.60 | 102.00 | 13.90 | 383.00 | 57.20 | 13.95 | ||||||||||||
BL-Z2BT | 251.00 | 187.00 | 13.30 | 25.20 | 28.60 | 1.50 | 53.00 | 116.00 | 16.20 | 441.00 | 66.50 | 16.15 | |||||||||||||
4437-1 | 二长花岗 岩 | 177.00 | 706.00 | 6.63 | 3.18 | 10.50 | 0.97 | 5.50 | 17.20 | 1.28 | 203.00 | 4.39 | 0.86 | ||||||||||||
4437-2 | 162.00 | 298.00 | 12.40 | 5.33 | 10.50 | 2.31 | 16.90 | 31.40 | 3.65 | 135.00 | 12.90 | 2.47 | |||||||||||||
4437-3 | 190.00 | 475.00 | 15.50 | 4.65 | 7.91 | 1.51 | 14.10 | 28.60 | 2.70 | 101.00 | 9.11 | 1.61 | |||||||||||||
4437-4 | 174.00 | 468.00 | 14.80 | 4.47 | 9.51 | 1.85 | 31.50 | 60.40 | 6.26 | 110.00 | 21.30 | 3.66 | |||||||||||||
样品编号 | 岩性 | Zr | Hf | Eu | Gd | Tb | Dy | Y | Ho | Er | Tm | Yb | Lu | ||||||||||||
BL1-1 | 黑云母二 长花岗岩 | 386.00 | 10.50 | 1.29 | 4.67 | 0.79 | 4.17 | 24.30 | 0.94 | 2.84 | 0.47 | 3.05 | 0.55 | ||||||||||||
BL1-2 | 369.00 | 10.00 | 1.36 | 4.73 | 0.78 | 4.43 | 25.70 | 0.97 | 2.71 | 0.49 | 2.96 | 0.53 | |||||||||||||
BL-Z1 | 493.00 | 10.70 | 1.31 | 5.23 | 0.73 | 4.06 | 28.20 | 0.85 | 2.20 | 0.31 | 2.08 | 0.35 | |||||||||||||
BL-Z2 | 316.00 | 7.50 | 0.88 | 4.35 | 0.72 | 4.15 | 30.20 | 0.88 | 2.63 | 0.42 | 2.78 | 0.44 | |||||||||||||
BL-Z1BT | 暗色微粒 包体 | 306.00 | 7.40 | 1.37 | 11.95 | 1.92 | 10.60 | 68.00 | 2.23 | 6.14 | 0.89 | 6.17 | 0.92 | ||||||||||||
BL-Z2BT | 336.00 | 8.40 | 1.56 | 14.40 | 2.42 | 13.30 | 78.00 | 2.68 | 7.56 | 1.08 | 7.03 | 1.11 | |||||||||||||
4437-1 | 二长花岗 岩 | 149.00 | 11.50 | 0.33 | 0.85 | 0.16 | 1.02 | 5.30 | 0.23 | 0.70 | 0.11 | 0.77 | 0.12 | ||||||||||||
4437-2 | 68.90 | 2.70 | 0.32 | 2.19 | 0.34 | 1.89 | 11.00 | 0.40 | 1.15 | 0.19 | 1.24 | 0.19 | |||||||||||||
4437-3 | 73.80 | 2.86 | 0.30 | 1.58 | 0.23 | 1.23 | 6.39 | 0.25 | 0.71 | 0.10 | 0.66 | 0.09 | |||||||||||||
4437-4 | 62.60 | 2.70 | 0.44 | 3.21 | 0.41 | 1.92 | 9.54 | 0.37 | 1.00 | 0.15 | 0.92 | 0.14 |
Table 2 Major elements(%)and trace elements(10-6) for monzogranite and its enclaves from Bayandulan area
样品编号 | 岩性 | SiO2 | TiO2 | Al2O3 | FeO | Fe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
BL1-1 | 黑云母二 长花岗岩 | 70.39 | 0.41 | 14.99 | 2.26 | 0.46 | 0.05 | 0.79 | 0.48 | 4.50 | 4.28 | 0.11 | (0.06) | 98.66 | |||||||||||
BL1-2 | 69.16 | 0.38 | 15.32 | 2.07 | 0.46 | 0.05 | 0.71 | 1.20 | 4.09 | 4.36 | 0.10 | 0.84 | 98.74 | ||||||||||||
BL-Z1 | 68.33 | 0.40 | 15.44 | 2.29 | 0.58 | 0.05 | 0.51 | 1.20 | 4.16 | 4.77 | 0.09 | 1.26 | 99.06 | ||||||||||||
BL-Z2 | 68.69 | 0.44 | 15.55 | 2.20 | 0.93 | 0.08 | 0.93 | 2.00 | 3.94 | 4.01 | 0.11 | 0.87 | 99.75 | ||||||||||||
BL-Z1BT | 暗色微粒 包体 | 52.49 | 1.34 | 17.54 | 8.35 | 2.33 | 0.22 | 3.45 | 3.35 | 4.33 | 2.07 | 0.35 | 2.82 | 97.15 | |||||||||||
BL-Z2BT | 52.65 | 1.34 | 17.57 | 8.20 | 2.51 | 0.23 | 3.46 | 3.35 | 4.33 | 2.07 | 0.35 | 2.77 | 97.38 | ||||||||||||
4437-1 | 二长花岗 岩 | 72.44 | 0.15 | 15.52 | 0.12 | 0.74 | 0.10 | 0.24 | 0.67 | 4.83 | 4.26 | 0.07 | 0.67 | 99.81 | |||||||||||
4437-2 | 74.22 | 0.13 | 14.71 | 0.20 | 0.54 | 0.08 | 0.20 | 0.59 | 4.35 | 4.28 | 0.06 | 0.52 | 99.88 | ||||||||||||
4437-3 | 73.59 | 0.17 | 14.56 | 0.47 | 0.92 | 0.10 | 0.36 | 1.01 | 4.48 | 3.57 | 0.09 | 0.65 | 99.97 | ||||||||||||
4437-4 | 71.56 | 0.15 | 16.38 | 0.18 | 0.65 | 0.07 | 0.21 | 0.58 | 4.94 | 4.35 | 0.05 | 0.74 | 99.86 | ||||||||||||
样品编号 | 岩性 | Rb | Ba | Th | U | Nb | Ta | La | Ce | Pr | Sr | Nd | Sm | ||||||||||||
BL1-1 | 黑云母二 长花岗岩 | 113.50 | 892.00 | 14.10 | 2.30 | 10.20 | 1.20 | 24.50 | 52.20 | 5.93 | 205.00 | 22.10 | 5.56 | ||||||||||||
BL1-2 | 122.00 | 917.00 | 13.95 | 2.71 | 9.90 | 1.20 | 34.20 | 69.70 | 7.44 | 354.00 | 27.60 | 5.88 | |||||||||||||
BL-Z1 | 117.50 | 817.00 | 10.55 | 7.76 | 8.90 | 0.70 | 48.50 | 95.40 | 10.80 | 229.00 | 39.80 | 6.85 | |||||||||||||
BL-Z2 | 165.50 | 615.00 | 14.90 | 8.17 | 11.90 | 1.70 | 26.70 | 51.20 | 6.38 | 256.00 | 24.60 | 5.05 | |||||||||||||
BL-Z1BT | 暗色微粒 包体 | 212.00 | 161.50 | 11.25 | 20.20 | 23.70 | 1.30 | 45.60 | 102.00 | 13.90 | 383.00 | 57.20 | 13.95 | ||||||||||||
BL-Z2BT | 251.00 | 187.00 | 13.30 | 25.20 | 28.60 | 1.50 | 53.00 | 116.00 | 16.20 | 441.00 | 66.50 | 16.15 | |||||||||||||
4437-1 | 二长花岗 岩 | 177.00 | 706.00 | 6.63 | 3.18 | 10.50 | 0.97 | 5.50 | 17.20 | 1.28 | 203.00 | 4.39 | 0.86 | ||||||||||||
4437-2 | 162.00 | 298.00 | 12.40 | 5.33 | 10.50 | 2.31 | 16.90 | 31.40 | 3.65 | 135.00 | 12.90 | 2.47 | |||||||||||||
4437-3 | 190.00 | 475.00 | 15.50 | 4.65 | 7.91 | 1.51 | 14.10 | 28.60 | 2.70 | 101.00 | 9.11 | 1.61 | |||||||||||||
4437-4 | 174.00 | 468.00 | 14.80 | 4.47 | 9.51 | 1.85 | 31.50 | 60.40 | 6.26 | 110.00 | 21.30 | 3.66 | |||||||||||||
样品编号 | 岩性 | Zr | Hf | Eu | Gd | Tb | Dy | Y | Ho | Er | Tm | Yb | Lu | ||||||||||||
BL1-1 | 黑云母二 长花岗岩 | 386.00 | 10.50 | 1.29 | 4.67 | 0.79 | 4.17 | 24.30 | 0.94 | 2.84 | 0.47 | 3.05 | 0.55 | ||||||||||||
BL1-2 | 369.00 | 10.00 | 1.36 | 4.73 | 0.78 | 4.43 | 25.70 | 0.97 | 2.71 | 0.49 | 2.96 | 0.53 | |||||||||||||
BL-Z1 | 493.00 | 10.70 | 1.31 | 5.23 | 0.73 | 4.06 | 28.20 | 0.85 | 2.20 | 0.31 | 2.08 | 0.35 | |||||||||||||
BL-Z2 | 316.00 | 7.50 | 0.88 | 4.35 | 0.72 | 4.15 | 30.20 | 0.88 | 2.63 | 0.42 | 2.78 | 0.44 | |||||||||||||
BL-Z1BT | 暗色微粒 包体 | 306.00 | 7.40 | 1.37 | 11.95 | 1.92 | 10.60 | 68.00 | 2.23 | 6.14 | 0.89 | 6.17 | 0.92 | ||||||||||||
BL-Z2BT | 336.00 | 8.40 | 1.56 | 14.40 | 2.42 | 13.30 | 78.00 | 2.68 | 7.56 | 1.08 | 7.03 | 1.11 | |||||||||||||
4437-1 | 二长花岗 岩 | 149.00 | 11.50 | 0.33 | 0.85 | 0.16 | 1.02 | 5.30 | 0.23 | 0.70 | 0.11 | 0.77 | 0.12 | ||||||||||||
4437-2 | 68.90 | 2.70 | 0.32 | 2.19 | 0.34 | 1.89 | 11.00 | 0.40 | 1.15 | 0.19 | 1.24 | 0.19 | |||||||||||||
4437-3 | 73.80 | 2.86 | 0.30 | 1.58 | 0.23 | 1.23 | 6.39 | 0.25 | 0.71 | 0.10 | 0.66 | 0.09 | |||||||||||||
4437-4 | 62.60 | 2.70 | 0.44 | 3.21 | 0.41 | 1.92 | 9.54 | 0.37 | 1.00 | 0.15 | 0.92 | 0.14 |
Fig.7 Chondrite-normalized REE patterns(a) and primitive mantle-normalized trace elements patterns(b) of monzogranite and its enclaves in Bayandulan area(chondrite-normalized values and primitive mantle-normalized values after reference[33])
测试 点号 | Th/10-6 | U/10-6 | Pb/10-6 | Th/U | 同位素比值 | 年龄/Ma | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/235U | 206Pb/238U | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||||||||
BL1-02 | 158.56 | 381.55 | 19.10 | 0.42 | 0.343 92 | 0.012 05 | 0.047 90 | 0.000 66 | 300 | 9 | 302 | 4 | |
BL1-03 | 103.84 | 228.17 | 11.61 | 0.46 | 0.343 24 | 0.020 28 | 0.047 67 | 0.000 75 | 300 | 15 | 300 | 5 | |
BL1-04 | 141.01 | 361.77 | 17.98 | 0.39 | 0.340 40 | 0.012 07 | 0.047 28 | 0.000 63 | 297 | 9 | 298 | 4 | |
BL1-05 | 113.38 | 236.93 | 12.11 | 0.48 | 0.340 96 | 0.015 88 | 0.047 61 | 0.000 70 | 298 | 12 | 300 | 4 | |
BL1-08 | 226.42 | 383.68 | 20.25 | 0.59 | 0.345 99 | 0.011 48 | 0.047 71 | 0.000 63 | 302 | 9 | 300 | 4 | |
BL1-10 | 75.99 | 276.89 | 14.18 | 0.27 | 0.367 37 | 0.015 50 | 0.047 09 | 0.000 63 | 318 | 12 | 297 | 4 | |
BL1-11 | 119.22 | 242.37 | 13.04 | 0.49 | 0.363 79 | 0.018 47 | 0.047 82 | 0.000 70 | 315 | 14 | 301 | 4 | |
BL1-12 | 109.67 | 166.53 | 9.73 | 0.66 | 0.358 41 | 0.020 61 | 0.047 14 | 0.000 75 | 311 | 15 | 297 | 5 | |
BL1-18 | 382.47 | 1 420.89 | 72.04 | 0.27 | 0.352 21 | 0.010 35 | 0.048 27 | 0.000 59 | 306 | 8 | 304 | 4 | |
BL1-20 | 65.31 | 629.05 | 30.57 | 0.10 | 0.349 42 | 0.009 16 | 0.048 35 | 0.000 60 | 304 | 7 | 304 | 4 | |
BL1-26 | 110.78 | 356.60 | 17.93 | 0.31 | 0.354 06 | 0.010 52 | 0.047 31 | 0.000 60 | 308 | 8 | 298 | 4 | |
BL1-27 | 48.78 | 124.22 | 6.40 | 0.39 | 0.344 00 | 0.015 79 | 0.047 38 | 0.000 67 | 300 | 12 | 298 | 4 | |
BL1-28 | 58.24 | 153.42 | 7.94 | 0.38 | 0.343 43 | 0.011 69 | 0.047 77 | 0.000 64 | 300 | 9 | 301 | 4 | |
BL1-29 | 76.28 | 214.89 | 11.12 | 0.35 | 0.346 31 | 0.011 11 | 0.047 92 | 0.000 62 | 302 | 8 | 302 | 4 | |
BL2-01 | 390.64 | 1241.56 | 75.02 | 0.31 | 0.336 86 | 0.016 23 | 0.046 02 | 0.000 56 | 295 | 12 | 290 | 3 | |
BL2-06 | 45.92 | 118.34 | 5.86 | 0.39 | 0.348 09 | 0.021 83 | 0.048 38 | 0.000 83 | 303 | 16 | 305 | 5 | |
BL2-07 | 95.76 | 209.94 | 24.94 | 0.46 | 0.339 91 | 0.018 41 | 0.047 21 | 0.000 77 | 297 | 14 | 297 | 5 | |
BL2-08 | 38.33 | 101.05 | 5.14 | 0.38 | 0.344 18 | 0.030 08 | 0.047 65 | 0.000 85 | 300 | 23 | 300 | 5 | |
BL2-09 | 91.05 | 267.87 | 13.83 | 0.34 | 0.345 68 | 0.012 33 | 0.047 76 | 0.000 65 | 301 | 9 | 301 | 4 | |
BL2-10 | 98.96 | 291.63 | 14.47 | 0.34 | 0.347 12 | 0.017 65 | 0.048 00 | 0.000 66 | 303 | 13 | 302 | 4 | |
BL2-11 | 79.50 | 181.09 | 9.38 | 0.44 | 0.342 00 | 0.022 42 | 0.047 46 | 0.000 71 | 299 | 17 | 299 | 4 | |
BL2-13 | 102.03 | 236.30 | 13.85 | 0.43 | 0.340 33 | 0.022 64 | 0.046 14 | 0.000 67 | 297 | 17 | 291 | 4 | |
BL2-15 | 136.33 | 288.44 | 14.74 | 0.47 | 0.346 03 | 0.013 20 | 0.047 81 | 0.000 63 | 302 | 10 | 301 | 4 | |
BL2-17 | 65.25 | 162.95 | 8.35 | 0.40 | 0.343 77 | 0.024 67 | 0.047 63 | 0.000 83 | 300 | 19 | 300 | 5 | |
BL2-18 | 61.13 | 163.36 | 8.41 | 0.37 | 0.347 48 | 0.015 44 | 0.047 97 | 0.000 65 | 303 | 12 | 302 | 4 | |
BL2-19 | 249.00 | 798.83 | 40.19 | 0.31 | 0.355 07 | 0.006 89 | 0.049 12 | 0.000 56 | 309 | 5 | 309 | 3 | |
BL2-21 | 189.26 | 405.58 | 22.24 | 0.47 | 0.341 33 | 0.013 57 | 0.047 08 | 0.000 58 | 298 | 10 | 297 | 4 | |
BL2-23 | 82.87 | 227.96 | 10.89 | 0.36 | 0.335 95 | 0.018 47 | 0.047 03 | 0.000 74 | 294 | 14 | 296 | 5 | |
BL2-24 | 268.72 | 1 029.77 | 51.11 | 0.26 | 0.376 44 | 0.009 93 | 0.047 55 | 0.000 56 | 324 | 7 | 299 | 3 | |
BL2-27 | 316.44 | 741.82 | 40.68 | 0.43 | 0.342 46 | 0.014 46 | 0.047 48 | 0.000 60 | 299 | 11 | 299 | 4 | |
BL2-29 | 112.13 | 449.76 | 24.43 | 0.25 | 0.362 19 | 0.009 63 | 0.047 96 | 0.000 56 | 314 | 7 | 302 | 3 | |
BL2-30 | 103.47 | 278.62 | 15.14 | 0.37 | 0.352 11 | 0.013 71 | 0.047 71 | 0.000 61 | 306 | 10 | 300 | 4 | |
BL2-31 | 91.25 | 290.46 | 13.06 | 0.31 | 0.379 16 | 0.012 64 | 0.048 10 | 0.000 65 | 326 | 9 | 303 | 4 |
Table 3 Zircon LA-ICP-MS U-Pb data for biotite monzogranite samples from the Bayandulan copper deposit
测试 点号 | Th/10-6 | U/10-6 | Pb/10-6 | Th/U | 同位素比值 | 年龄/Ma | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/235U | 206Pb/238U | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||||||||
BL1-02 | 158.56 | 381.55 | 19.10 | 0.42 | 0.343 92 | 0.012 05 | 0.047 90 | 0.000 66 | 300 | 9 | 302 | 4 | |
BL1-03 | 103.84 | 228.17 | 11.61 | 0.46 | 0.343 24 | 0.020 28 | 0.047 67 | 0.000 75 | 300 | 15 | 300 | 5 | |
BL1-04 | 141.01 | 361.77 | 17.98 | 0.39 | 0.340 40 | 0.012 07 | 0.047 28 | 0.000 63 | 297 | 9 | 298 | 4 | |
BL1-05 | 113.38 | 236.93 | 12.11 | 0.48 | 0.340 96 | 0.015 88 | 0.047 61 | 0.000 70 | 298 | 12 | 300 | 4 | |
BL1-08 | 226.42 | 383.68 | 20.25 | 0.59 | 0.345 99 | 0.011 48 | 0.047 71 | 0.000 63 | 302 | 9 | 300 | 4 | |
BL1-10 | 75.99 | 276.89 | 14.18 | 0.27 | 0.367 37 | 0.015 50 | 0.047 09 | 0.000 63 | 318 | 12 | 297 | 4 | |
BL1-11 | 119.22 | 242.37 | 13.04 | 0.49 | 0.363 79 | 0.018 47 | 0.047 82 | 0.000 70 | 315 | 14 | 301 | 4 | |
BL1-12 | 109.67 | 166.53 | 9.73 | 0.66 | 0.358 41 | 0.020 61 | 0.047 14 | 0.000 75 | 311 | 15 | 297 | 5 | |
BL1-18 | 382.47 | 1 420.89 | 72.04 | 0.27 | 0.352 21 | 0.010 35 | 0.048 27 | 0.000 59 | 306 | 8 | 304 | 4 | |
BL1-20 | 65.31 | 629.05 | 30.57 | 0.10 | 0.349 42 | 0.009 16 | 0.048 35 | 0.000 60 | 304 | 7 | 304 | 4 | |
BL1-26 | 110.78 | 356.60 | 17.93 | 0.31 | 0.354 06 | 0.010 52 | 0.047 31 | 0.000 60 | 308 | 8 | 298 | 4 | |
BL1-27 | 48.78 | 124.22 | 6.40 | 0.39 | 0.344 00 | 0.015 79 | 0.047 38 | 0.000 67 | 300 | 12 | 298 | 4 | |
BL1-28 | 58.24 | 153.42 | 7.94 | 0.38 | 0.343 43 | 0.011 69 | 0.047 77 | 0.000 64 | 300 | 9 | 301 | 4 | |
BL1-29 | 76.28 | 214.89 | 11.12 | 0.35 | 0.346 31 | 0.011 11 | 0.047 92 | 0.000 62 | 302 | 8 | 302 | 4 | |
BL2-01 | 390.64 | 1241.56 | 75.02 | 0.31 | 0.336 86 | 0.016 23 | 0.046 02 | 0.000 56 | 295 | 12 | 290 | 3 | |
BL2-06 | 45.92 | 118.34 | 5.86 | 0.39 | 0.348 09 | 0.021 83 | 0.048 38 | 0.000 83 | 303 | 16 | 305 | 5 | |
BL2-07 | 95.76 | 209.94 | 24.94 | 0.46 | 0.339 91 | 0.018 41 | 0.047 21 | 0.000 77 | 297 | 14 | 297 | 5 | |
BL2-08 | 38.33 | 101.05 | 5.14 | 0.38 | 0.344 18 | 0.030 08 | 0.047 65 | 0.000 85 | 300 | 23 | 300 | 5 | |
BL2-09 | 91.05 | 267.87 | 13.83 | 0.34 | 0.345 68 | 0.012 33 | 0.047 76 | 0.000 65 | 301 | 9 | 301 | 4 | |
BL2-10 | 98.96 | 291.63 | 14.47 | 0.34 | 0.347 12 | 0.017 65 | 0.048 00 | 0.000 66 | 303 | 13 | 302 | 4 | |
BL2-11 | 79.50 | 181.09 | 9.38 | 0.44 | 0.342 00 | 0.022 42 | 0.047 46 | 0.000 71 | 299 | 17 | 299 | 4 | |
BL2-13 | 102.03 | 236.30 | 13.85 | 0.43 | 0.340 33 | 0.022 64 | 0.046 14 | 0.000 67 | 297 | 17 | 291 | 4 | |
BL2-15 | 136.33 | 288.44 | 14.74 | 0.47 | 0.346 03 | 0.013 20 | 0.047 81 | 0.000 63 | 302 | 10 | 301 | 4 | |
BL2-17 | 65.25 | 162.95 | 8.35 | 0.40 | 0.343 77 | 0.024 67 | 0.047 63 | 0.000 83 | 300 | 19 | 300 | 5 | |
BL2-18 | 61.13 | 163.36 | 8.41 | 0.37 | 0.347 48 | 0.015 44 | 0.047 97 | 0.000 65 | 303 | 12 | 302 | 4 | |
BL2-19 | 249.00 | 798.83 | 40.19 | 0.31 | 0.355 07 | 0.006 89 | 0.049 12 | 0.000 56 | 309 | 5 | 309 | 3 | |
BL2-21 | 189.26 | 405.58 | 22.24 | 0.47 | 0.341 33 | 0.013 57 | 0.047 08 | 0.000 58 | 298 | 10 | 297 | 4 | |
BL2-23 | 82.87 | 227.96 | 10.89 | 0.36 | 0.335 95 | 0.018 47 | 0.047 03 | 0.000 74 | 294 | 14 | 296 | 5 | |
BL2-24 | 268.72 | 1 029.77 | 51.11 | 0.26 | 0.376 44 | 0.009 93 | 0.047 55 | 0.000 56 | 324 | 7 | 299 | 3 | |
BL2-27 | 316.44 | 741.82 | 40.68 | 0.43 | 0.342 46 | 0.014 46 | 0.047 48 | 0.000 60 | 299 | 11 | 299 | 4 | |
BL2-29 | 112.13 | 449.76 | 24.43 | 0.25 | 0.362 19 | 0.009 63 | 0.047 96 | 0.000 56 | 314 | 7 | 302 | 3 | |
BL2-30 | 103.47 | 278.62 | 15.14 | 0.37 | 0.352 11 | 0.013 71 | 0.047 71 | 0.000 61 | 306 | 10 | 300 | 4 | |
BL2-31 | 91.25 | 290.46 | 13.06 | 0.31 | 0.379 16 | 0.012 64 | 0.048 10 | 0.000 65 | 326 | 9 | 303 | 4 |
测试点号 | 年龄/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | 2σ | εHf(0) | fLu/Hf | εHf(t) | TDM1 | TDM2 |
---|---|---|---|---|---|---|---|---|---|---|
BL1-02 | 302.00 | 0.02 | 0.000 7 | 0.282 897 | 0.000 009 | 4.4 | -0.98 | 10.9 | 499 | 619 |
BL1-03 | 300.00 | 0.03 | 0.001 0 | 0.282 885 | 0.000 010 | 4.0 | -0.97 | 10.4 | 521 | 652 |
BL1-04 | 298.00 | 0.03 | 0.001 0 | 0.282 829 | 0.000 008 | 2.0 | -0.97 | 8.4 | 599 | 775 |
BL1-05 | 300.00 | 0.02 | 0.000 8 | 0.282 866 | 0.000 007 | 3.3 | -0.98 | 9.8 | 545 | 691 |
BL1-08 | 300.00 | 0.04 | 0.001 3 | 0.282 840 | 0.000 010 | 2.4 | -0.96 | 8.8 | 588 | 754 |
BL1-10 | 297.00 | 0.04 | 0.001 3 | 0.282 836 | 0.000 010 | 2.2 | -0.96 | 8.5 | 595 | 766 |
BL1-11 | 301.00 | 0.03 | 0.000 9 | 0.282 863 | 0.000 009 | 3.2 | -0.97 | 9.7 | 550 | 699 |
BL1-18 | 304.00 | 0.03 | 0.001 0 | 0.282 866 | 0.000 007 | 3.3 | -0.97 | 9.8 | 547 | 693 |
BL1-20 | 304.00 | 0.05 | 0.001 7 | 0.282 761 | 0.000 007 | -0.4 | -0.95 | 6.0 | 709 | 939 |
BL1-26 | 298.00 | 0.02 | 0.000 6 | 0.282 803 | 0.000 009 | 1.1 | -0.98 | 7.5 | 630 | 830 |
BL1-27 | 298.00 | 0.02 | 0.000 7 | 0.282 866 | 0.000 010 | 3.3 | -0.98 | 9.7 | 543 | 690 |
BL1-28 | 301.00 | 0.03 | 0.000 8 | 0.282 851 | 0.000 012 | 2.8 | -0.97 | 9.2 | 566 | 726 |
BL1-29 | 302.00 | 0.02 | 0.000 7 | 0.282 843 | 0.000 008 | 2.5 | -0.98 | 9.0 | 576 | 742 |
BL2-01 | 290.00 | 0.02 | 0.000 7 | 0.282 847 | 0.000 008 | 2.7 | -0.98 | 9.1 | 569 | 732 |
BL2-06 | 305.00 | 0.02 | 0.000 7 | 0.282 867 | 0.000 009 | 3.4 | -0.98 | 9.8 | 541 | 687 |
BL2-09 | 301.00 | 0.02 | 0.000 7 | 0.282 821 | 0.000 010 | 1.7 | -0.98 | 8.2 | 605 | 790 |
BL2-10 | 302.00 | 0.03 | 0.000 8 | 0.282 893 | 0.000 009 | 4.3 | -0.98 | 10.7 | 506 | 629 |
BL2-11 | 299.00 | 0.02 | 0.000 7 | 0.282 859 | 0.000 009 | 3.1 | -0.98 | 9.5 | 552 | 705 |
BL2-13 | 291.00 | 0.03 | 0.001 0 | 0.282 779 | 0.000 012 | 0.2 | -0.97 | 6.6 | 671 | 890 |
BL2-17 | 300.00 | 0.02 | 0.000 6 | 0.282 850 | 0.000 009 | 2.7 | -0.98 | 9.2 | 564 | 725 |
BL2-18 | 302.00 | 0.01 | 0.000 5 | 0.282 881 | 0.000 011 | 3.8 | -0.99 | 10.3 | 519 | 654 |
BL2-19 | 309.00 | 0.02 | 0.000 8 | 0.282 895 | 0.000 008 | 4.3 | -0.98 | 10.8 | 503 | 626 |
BL2-21 | 297.00 | 0.05 | 0.001 5 | 0.282 894 | 0.000 009 | 4.3 | -0.96 | 10.6 | 513 | 635 |
BL2-24 | 299.00 | 0.02 | 0.000 7 | 0.282 846 | 0.000 008 | 2.6 | -0.98 | 9.1 | 570 | 734 |
BL2-27 | 299.00 | 0.04 | 0.001 5 | 0.282 856 | 0.000 022 | 3.0 | -0.95 | 9.3 | 568 | 722 |
BL2-29 | 302.00 | 0.03 | 0.000 9 | 0.282 814 | 0.000 008 | 1.5 | -0.97 | 7.9 | 618 | 808 |
BL2-30 | 300.00 | 0.06 | 0.001 6 | 0.282 831 | 0.000 009 | 2.1 | -0.95 | 8.4 | 605 | 778 |
Table 4 Zircon Lu-Hf isotopic compositions for biotite monzogranite samples from the Bayandulan copper deposit
测试点号 | 年龄/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | 2σ | εHf(0) | fLu/Hf | εHf(t) | TDM1 | TDM2 |
---|---|---|---|---|---|---|---|---|---|---|
BL1-02 | 302.00 | 0.02 | 0.000 7 | 0.282 897 | 0.000 009 | 4.4 | -0.98 | 10.9 | 499 | 619 |
BL1-03 | 300.00 | 0.03 | 0.001 0 | 0.282 885 | 0.000 010 | 4.0 | -0.97 | 10.4 | 521 | 652 |
BL1-04 | 298.00 | 0.03 | 0.001 0 | 0.282 829 | 0.000 008 | 2.0 | -0.97 | 8.4 | 599 | 775 |
BL1-05 | 300.00 | 0.02 | 0.000 8 | 0.282 866 | 0.000 007 | 3.3 | -0.98 | 9.8 | 545 | 691 |
BL1-08 | 300.00 | 0.04 | 0.001 3 | 0.282 840 | 0.000 010 | 2.4 | -0.96 | 8.8 | 588 | 754 |
BL1-10 | 297.00 | 0.04 | 0.001 3 | 0.282 836 | 0.000 010 | 2.2 | -0.96 | 8.5 | 595 | 766 |
BL1-11 | 301.00 | 0.03 | 0.000 9 | 0.282 863 | 0.000 009 | 3.2 | -0.97 | 9.7 | 550 | 699 |
BL1-18 | 304.00 | 0.03 | 0.001 0 | 0.282 866 | 0.000 007 | 3.3 | -0.97 | 9.8 | 547 | 693 |
BL1-20 | 304.00 | 0.05 | 0.001 7 | 0.282 761 | 0.000 007 | -0.4 | -0.95 | 6.0 | 709 | 939 |
BL1-26 | 298.00 | 0.02 | 0.000 6 | 0.282 803 | 0.000 009 | 1.1 | -0.98 | 7.5 | 630 | 830 |
BL1-27 | 298.00 | 0.02 | 0.000 7 | 0.282 866 | 0.000 010 | 3.3 | -0.98 | 9.7 | 543 | 690 |
BL1-28 | 301.00 | 0.03 | 0.000 8 | 0.282 851 | 0.000 012 | 2.8 | -0.97 | 9.2 | 566 | 726 |
BL1-29 | 302.00 | 0.02 | 0.000 7 | 0.282 843 | 0.000 008 | 2.5 | -0.98 | 9.0 | 576 | 742 |
BL2-01 | 290.00 | 0.02 | 0.000 7 | 0.282 847 | 0.000 008 | 2.7 | -0.98 | 9.1 | 569 | 732 |
BL2-06 | 305.00 | 0.02 | 0.000 7 | 0.282 867 | 0.000 009 | 3.4 | -0.98 | 9.8 | 541 | 687 |
BL2-09 | 301.00 | 0.02 | 0.000 7 | 0.282 821 | 0.000 010 | 1.7 | -0.98 | 8.2 | 605 | 790 |
BL2-10 | 302.00 | 0.03 | 0.000 8 | 0.282 893 | 0.000 009 | 4.3 | -0.98 | 10.7 | 506 | 629 |
BL2-11 | 299.00 | 0.02 | 0.000 7 | 0.282 859 | 0.000 009 | 3.1 | -0.98 | 9.5 | 552 | 705 |
BL2-13 | 291.00 | 0.03 | 0.001 0 | 0.282 779 | 0.000 012 | 0.2 | -0.97 | 6.6 | 671 | 890 |
BL2-17 | 300.00 | 0.02 | 0.000 6 | 0.282 850 | 0.000 009 | 2.7 | -0.98 | 9.2 | 564 | 725 |
BL2-18 | 302.00 | 0.01 | 0.000 5 | 0.282 881 | 0.000 011 | 3.8 | -0.99 | 10.3 | 519 | 654 |
BL2-19 | 309.00 | 0.02 | 0.000 8 | 0.282 895 | 0.000 008 | 4.3 | -0.98 | 10.8 | 503 | 626 |
BL2-21 | 297.00 | 0.05 | 0.001 5 | 0.282 894 | 0.000 009 | 4.3 | -0.96 | 10.6 | 513 | 635 |
BL2-24 | 299.00 | 0.02 | 0.000 7 | 0.282 846 | 0.000 008 | 2.6 | -0.98 | 9.1 | 570 | 734 |
BL2-27 | 299.00 | 0.04 | 0.001 5 | 0.282 856 | 0.000 022 | 3.0 | -0.95 | 9.3 | 568 | 722 |
BL2-29 | 302.00 | 0.03 | 0.000 9 | 0.282 814 | 0.000 008 | 1.5 | -0.97 | 7.9 | 618 | 808 |
BL2-30 | 300.00 | 0.06 | 0.001 6 | 0.282 831 | 0.000 009 | 2.1 | -0.95 | 8.4 | 605 | 778 |
构造背景 | 矿床(点) | 矿床类型 | 测试岩石/矿物 | 测试方法 | 成岩/成矿时代 | 参考文献 |
---|---|---|---|---|---|---|
同造山 | 欧玉陶勒盖 | 斑岩型矿床 | 辉石玄武岩 | SHRIMP锆石U-Pb | 371~390 Ma | [ |
辉钼矿 | Re-Os等时线法 | 371~374 Ma | ||||
石英闪长岩 | SHRIMP锆石U-Pb | (374±3) Ma | ||||
石英长石斑岩 | SHRIMP锆石U-Pb | (372±1) Ma | ||||
查干苏布尔加 | 斑岩型矿床 | 正长花岗斑岩 | K-Ar法 | 265~339 Ma | [ | |
辉钼矿 | Re-Os等时线法 | (370.0±0.8) Ma | ||||
绢云母 | 40Ar-39Ar法 | (369.4±7) Ma | ||||
白山 | 块状硫化物矿床 | 无 | 无 | 早—中泥盆世 | [ | |
造山后 | 奥尤特 | 火山-次火山热 液型矿床 | 流纹岩 | 锆石U-Pb | 320 Ma | 未发表 |
绢云母 | 40Ar-39Ar法 | (287±10) Ma | [ | |||
巴彦都兰 | 热液型矿床 | 二长花岗岩 | 锆石U-Pb | 300 Ma | 本文 | |
小坝梁 | 喷流沉积型矿床 | 凝灰岩 | 锆石U-Pb | 314 Ma | 未发表 |
Table 5 The mineralization age of the major copper deposits in Erenhot-East Ujimqin and their adjacent areas
构造背景 | 矿床(点) | 矿床类型 | 测试岩石/矿物 | 测试方法 | 成岩/成矿时代 | 参考文献 |
---|---|---|---|---|---|---|
同造山 | 欧玉陶勒盖 | 斑岩型矿床 | 辉石玄武岩 | SHRIMP锆石U-Pb | 371~390 Ma | [ |
辉钼矿 | Re-Os等时线法 | 371~374 Ma | ||||
石英闪长岩 | SHRIMP锆石U-Pb | (374±3) Ma | ||||
石英长石斑岩 | SHRIMP锆石U-Pb | (372±1) Ma | ||||
查干苏布尔加 | 斑岩型矿床 | 正长花岗斑岩 | K-Ar法 | 265~339 Ma | [ | |
辉钼矿 | Re-Os等时线法 | (370.0±0.8) Ma | ||||
绢云母 | 40Ar-39Ar法 | (369.4±7) Ma | ||||
白山 | 块状硫化物矿床 | 无 | 无 | 早—中泥盆世 | [ | |
造山后 | 奥尤特 | 火山-次火山热 液型矿床 | 流纹岩 | 锆石U-Pb | 320 Ma | 未发表 |
绢云母 | 40Ar-39Ar法 | (287±10) Ma | [ | |||
巴彦都兰 | 热液型矿床 | 二长花岗岩 | 锆石U-Pb | 300 Ma | 本文 | |
小坝梁 | 喷流沉积型矿床 | 凝灰岩 | 锆石U-Pb | 314 Ma | 未发表 |
[1] | 童英, 洪大卫, 王涛, 等. 中蒙边境中段花岗岩时空分布特征及构造和找矿意义[J]. 地球学报, 2010, 31(3): 395-412. |
[2] | 李可, 张志诚, 冯志硕, 等. 兴蒙造山带中段北部晚古生代两期岩浆活动及其构造意义[J]. 地质学报, 2015, 89(2): 272-288. |
[3] |
CHENG Y, TENG X, LI Y, et al. Early Permian East-Ujimqin mafic-ultramafic and granitic rocks from the Xing’an-Mongolian Orogenic Belt, North China: Origin, chronology, and tectonic implications[J]. Journal of Asian Earth Sciences, 2014, 96: 361-373.
DOI URL |
[4] | 赵一鸣, 王大畏, 张德全, 等. 内蒙古东南部铜多金属成矿地质条件及找矿模式[M]. 北京: 地震出版社, 1994: 1-234. |
[5] | 赵一鸣, 张德全, 徐志刚. 大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M]. 北京: 地震出版社, 1997: 1-318. |
[6] | 聂凤军, 江思宏, 张义, 等. 中蒙边境中东段金属矿床成矿规律和找矿方向[M]. 北京: 地质出版社, 2007: 1-574. |
[7] |
ZHANG W, NIE F, LIU S, et al. Characteristics and genesis of mineral deposits in East Ujimqin Banner, western segment of the Great Xing’an Mountains, NE China[J]. Journal of Asian Earth Sciences, 2015, 97: 459-471.
DOI URL |
[8] | 王建平. 内蒙古东乌旗铜、银多金属成矿带成矿类型分析[J]. 矿产与地质, 2003, 17(2): 132-135. |
[9] | 王守光, 黄占起, 苏新旭, 等. 一条值得重视的跨国境成矿带——南戈壁—东乌旗铜多金属成矿带[J]. 地学前缘, 2004, 11(1): 249-255. |
[10] | 聂凤军, 江思宏, 白大明, 等. 蒙古国南部及邻区金属矿床类型及其时空分布特征[J]. 地球学报, 2010, 31(3):267-288. |
[11] | 张万益, 聂凤军, 刘树文, 等. 大兴安岭南段西坡金属矿床特征及成矿规律[J]. 中国地质, 2013, 40(5): 1583-1599. |
[12] | 常春郊, 王治华, 王梁, 等. 内蒙东乌珠穆沁旗地区多金属矿床类型与成矿规律[J]. 矿产与地质, 2014(5): 536-545. |
[13] | 张万益, 聂凤军, 刘妍, 等. 内蒙古东乌旗吉林宝力格银(金)矿床地质特征及成因探讨[J]. 矿物学报, 2007, 27(s1): 178-180. |
[14] | 张万益. 内蒙古东乌珠穆沁旗岩浆活动与金属成矿作用[D]. 北京: 中国地质科学院, 2008: 1-169. |
[15] |
JIANG S H, BAGAS L, HU P, et al. Zircon U-Pb ages and Sr-Nd-Hf isotopes of the highly fractionated granite with tetrad REE patterns in the Shamai tungsten deposit in eastern Inner Mongolia, China: Implications for the timing of mineralization and ore genesis[J]. Lithos, 2016, 261: 322-339.
DOI URL |
[16] | 胡朋, 聂凤军, 赫英, 等. 内蒙古沙麦岩体:正εNd(t)值的过铝质花岗岩[J]. 岩石学报, 2006, 22(11): 2781-2790. |
[17] | 许立权, 陈志勇, 陈郑辉, 等. 内蒙古东乌旗朝不楞铁矿区中粗粒花岗岩SHRIMP定年及其意义[J]. 矿床地质, 2010, 29(2): 317-322. |
[18] | 聂秀兰, 侯万荣. 内蒙古迪彦钦阿木大型钼-银矿床的发现及地质意义[J]. 地球学报, 2010, 31(3): 469-472. |
[19] | 孙艳霞, 张达, 张寿庭, 等. 内蒙古小坝梁铜金矿床的硫、铅同位素特征和喷流沉积成因[J]. 地质找矿论丛, 2009, 24(4): 282-285. |
[20] | 张万益, 聂凤军, 刘妍, 等. 内蒙古奥尤特铜-锌矿床绢云母40Ar-39Ar同位素年龄及地质意义[J]. 地球学报, 2008, 29(5): 592-598. |
[21] | 李敏, 程银行, 李艳锋. 内蒙古东乌旗巴彦都兰二长花岗岩年代学、地球化学特征及其地质意义[J]. 地质科技情报, 2015, 34(4): 6-14. |
[22] | 李敏, 程银行, 任邦方, 等. 内蒙古东乌旗晚古生代闪长岩、二长花岗岩年代学特征及岩石成因[J]. 中国地质, 2016, 43(2):380-394. |
[23] | 洪大卫, 王式洸, 谢锡林, 等. 试析地幔来源物质成矿域——以中亚造山带为例[J]. 矿床地质, 2003, 22(1): 41-55. |
[24] |
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 |
[25] |
YUAN H, GAO S, LIU X, et al. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry[J]. Geostandards and Geoanalytical Research, 2004, 28(3): 353-370.
DOI URL |
[26] |
WU F Y, YANG Y H, XIE L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochrono-logy[J]. Chemical Geology, 2006, 234(1): 105-126.
DOI URL |
[27] |
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 |
[28] | MIDDLEMOST E A. Magmatic Rocks[M]. London:Logman, 1995: 1-266. |
[29] |
Middlemost E A. Naming materials in the magma/igneous rock system[J]. Earth Science Reviews, 1994, 37(3/4): 215-224.
DOI URL |
[30] | RUBATTO D, GEBAUER D. Use of cathodoluminescence for U-Pb zircon dating by ion Microprobe: Some examples from the Western Alps[M]// PAGELM, BARBINV, BLANCP, et al.Cathodoluminescence in Geosciences. Berlin, Heidelberg: Springer, 2000: 373-400. |
[31] |
HANCHAR J M, MILLER C F. Zircon zonation patterns as revealed by cathodoluminescence and backscattered electron images: implications for interpretation of complex crustal histories[J]. Chemical Geology, 1993, 110(1): 1-13.
DOI URL |
[32] |
BELOUSOVA E, 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 |
[33] |
SUN S S, MCDONOUGH W F. Chemical and isotopic systema-tics of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society of London, Special Publications, 1989, 42(1): 313-345.
DOI URL |
[34] |
BLICHERT-TOFT J, ALBARÈDE 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): 243-258.
DOI URL |
[35] |
GRIFFIN W L, PEARSON N J, BELOUSOVA E, et al. The Hf isotope composition of cratonic mantle: LA-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1): 133-147.
DOI URL |
[36] | 程银行, 李艳锋, 李敏, 等. 内蒙古东乌旗碱性侵入岩的时代、成因及地质意义[J]. 地质学报, 2014, 88(11): 2086-2096. |
[37] | 王治华, 常春郊, 丛润祥, 等. 内蒙古阿钦楚鲁二长花岗岩锆石SHRIMP U-Pb年龄及地球化学特征[J]. 吉林大学学报(地球科学版), 2015, 45(1): 166-187. |
[38] | 王继春, 王银宏, 张梅, 等. 内蒙古高尔旗银铅锌矿区花岗岩的岩石成因:地球化学、锆石U-Pb年代学及Hf同位素约束[J]. 现代地质, 2016, 30(5): 961-980. |
[39] | 云飞, 聂凤军, 江思宏, 等. 内蒙古莫若格钦地区二长闪长岩锆石SHRIMP U-Pb年龄及其地质意义[J]. 矿床地质, 2011, 30(3): 504-510. |
[40] |
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 |
[41] | 韩宝福. 后碰撞花岗岩类的多样性及其构造环境判别的复杂性[J]. 地学前缘, 2007, 14(3): 64-72. |
[42] |
BATCHELOR R A, BOWDEN P. Petrogenetic interpretation of granitoid rock series using multicationic parameters[J]. Chemical Geology, 1985, 48(1/4): 43-55.
DOI URL |
[43] | XIAO W, WINDLEY B F, HAO J, et al. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the Central Asian orogenic belt[J]. Tectoni-cs, 2003, 22(6): 8-1. |
[44] |
XIAO W J, WINDLEY B F, HUANG B C, et al. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia[J]. International Journal of Earth Sciences, 2009, 98(6): 1189-1217.
DOI URL |
[45] |
WINDLEY B F, ALEXEIEV D, XIAO W, et al. Tectonic models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 2007, 164(1): 31-47.
DOI URL |
[46] |
ROBINSON P T, ZHOU M, HU X F, et al. Geochemical constraints on the origin of the Hegenshan ophiolite, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 1999, 17(4): 423-442.
DOI URL |
[47] |
JIAN P, LIU D, KRÖNER A, et al. Time scale of an early to mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China: implications for continental growth[J]. Lithos, 2008, 101(3): 233-259.
DOI URL |
[48] | 苏美霞, 赵文涛, 张慧聪, 等. 华北板块与西伯利亚板块缝合带之地球物理特征[J]. 物探与化探, 2014, 38(5): 949-955. |
[49] |
EIZENHÖFER P R, ZHAO G, ZHANG J, et al. Final closure of the Paleo-Asian Ocean along the Solonker Suture Zone: Constraints from geochronological and geochemical data of Permian volcanic and sedimentary rocks[J]. Tectonics, 2014, 33(4): 441-463.
DOI URL |
[50] |
JIAN P, KRÖNER A, WINDLEY B F, et al. Carboniferous and Cretaceous mafic-ultramafic massifs in Inner Mongolia (China): A SHRIMP zircon and geochemical study of the previously presumed integral “Hegenshan ophiolite”[J]. Lithos, 2012, 142/143: 48-66.
DOI URL |
[51] |
ZHANG Z, LI K, LI J, et al. Geochronology and geochemistry of the Eastern Erenhot ophiolitic complex: Implications for the tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt[J]. Journal of Asian Earth Sciences, 2015, 97: 279-293.
DOI URL |
[52] | 黄波, 付冬, 李树才, 等. 内蒙古贺根山蛇绿岩形成时代及构造启示[J]. 岩石学报, 2016, 32(1): 158-176. |
[53] | 洪大卫, 王式洸, 韩宝福, 等. 碱性花岗岩的构造环境分类及其鉴别标志[J]. 中国科学:化学, 1995(4):418-426. |
[54] | 辛后田, 滕学建. 内蒙古东乌旗宝力高庙组地层划分及其同位素年代学研究[J]. 地质调查与研究, 2011, 34(1): 1-9. |
[55] | 程银行, 滕学建, 辛后田, 等. 内蒙古东乌旗狠麦温都尔花岗岩SHRIMP锆石U-Pb年龄及其地质意义[J]. 岩石矿物学杂志, 2012, 31(3): 323-334. |
[56] | 邓晋福, 赵海玲, 莫宣学. 中国大陆根-柱构造:大陆动力学的钥匙[M]. 北京: 地质出版社, 1996: 1-110. |
[57] |
BROWN M. The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogens[J]. Earth-Science Reviews, 1994, 36(1/2): 83-130.
DOI URL |
[58] | 张旗, 潘国强, 李承东, 等. 花岗岩结晶分离作用问题——关于花岗岩研究的思考之二[J]. 岩石学报, 2007, 23(6): 1239-1251. |
[59] |
SCHERER E E, CAMERON K L, BLICHERT-TOFT J. Lu-Hf garnet geochronology: closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions[J]. Geochimica et Cosmochimica Acta, 2000, 64(19): 3413-3432.
DOI URL |
[60] | 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. |
[61] |
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): 237-269.
DOI URL |
[62] |
DOBRETSOV N L, BERZIN N A, BUSLOV M M. Opening and tectonic evolution of the Paleo-Asian Ocean[J]. International Geology Review, 1995, 37(4): 335-360.
DOI URL |
[63] | DEBON F. Comparative major element chemistry in various “microgranular enclave-plutonic host” pairs[M]// DIDIERJ, BARBARINB.Enclaves and Granite Petrology. Amsterdam:Elsevier, 1991: 293-312. |
[64] |
KOCAK K, ZEDEF V, KANSUN G. Magma mixing/mingling in the Eocene Horoz (Nigde) granitoids, central southern Turkey: evidence from mafic microgranular enclaves[J]. Mineralogy and Petrology, 2011, 103(1/4): 149-167.
DOI URL |
[65] |
MÜNKER C, PFÄNDER J A, WEYER S, et al. Evolution of planetary cores and the Earth-Moon system from Nb/Ta systema-tics[J]. Science, 2003, 301:84.
DOI URL |
[66] |
ZORPI M J, COULON C, ORSINI J B, et al. Magma mingling, zoning and emplacement in calc-alkaline granitoid plutons[J]. Tectonophysics, 1989, 157(4):315-329.
DOI URL |
[67] | 张旗, 潘国强, 李承东, 等. 花岗岩混合问题:与玄武岩对比的启示——关于花岗岩研究的思考之一[J]. 岩石学报, 2007, 23(5): 1141-1152. |
[68] | 华仁民, 王登红. 关于花岗岩与成矿作用若干基本概念的再认识[J]. 矿床地质, 2012, 31(1): 165-175. |
[69] | 聂凤军, 曹毅, 丁成武, 等. 论兴蒙造山带叠生成矿作用——以锡林浩特和额尔古纳地块为例[J]. 岩石学报, 2014, 30(7): 2063-2080. |
[70] | 葛良胜, 张文钊, 袁士松, 等. 蒙古南戈壁—中国东乌旗跨国境成矿带东段金多金属成矿与找矿[M]. 北京: 地质出版社, 2009: 1-209. |
[71] |
PERELLO J, COX D, GARAMJAV D, et al. Oyu Tolgoi, Mongolia: Siluro-Devonian porphyry Cu-Au-(Mo) and high-sulfidation Cu mineralization with a Cretaceous Chalcocite Blanket[J]. Economic Geology, 2001, 96(6):1407-1428.
DOI URL |
[72] |
KHASHGEREL B E, RYE R O, HEDENQUIST J W, et al. Geology and reconnaissance stable isotope study of the Oyu Tolgoi porphyry Cu-Au system, South Gobi, Mongolia[J]. Economic Geology, 2006, 101(3):503-522.
DOI URL |
[73] |
WAINWRIGHT A J, TOSDAL R M, WOODEN J L, et al. U-Pb (zircon) and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu-Au district, southern Mongolia[J]. Gondwana Research, 2011, 19(3):764-787.
DOI URL |
[74] | WATANABE Y, STEIN H J. Re-Os ages for the Erdenet and Tsagaan Suvarga porphyry Cu-Mo deposits, Mongolia, and tectonic implications[J]. Economic Geology, 2000, 95(7): 1537-1542. |
[75] | 聂凤军, 云飞. 蒙古国南部又发现一处大型铜-锌矿床[J]. 地球学报, 2009, 30(1): 127-128. |
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