Earth Science Frontiers ›› 2020, Vol. 27 ›› Issue (2): 332-352.DOI: 10.13745/j.esf.sf.2020.3.25
Previous Articles Next Articles
LI Yongsheng(), ZHEN Shimin, YU Xiaofei, GONG Fanying, DU Zezhong
Received:
2020-02-09
Revised:
2020-03-10
Online:
2020-03-25
Published:
2020-03-25
CLC Number:
LI Yongsheng, ZHEN Shimin, YU Xiaofei, GONG Fanying, DU Zezhong. Zircon U-Pb geochronology and Hf isotopic compositions of igneous rocks from the Shuikoushan Pb-Zn deposit, Hunan Province, and their geological significance[J]. Earth Science Frontiers, 2020, 27(2): 332-352.
测点编号 | 元素含量/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb | 232Th | 238U | 232Th/238U | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||
SKC-5-1 | 5.63 | 120.87 | 231.98 | 0.52 | 0.047 1 | 0.00 | 0.172 5 | 0.00 | 0.025 4 | 0.00 | 52.0 | 13.0 | 162.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-2 | 4.73 | 93.88 | 190.15 | 0.49 | 0.046 9 | 0.00 | 0.174 3 | 0.00 | 0.025 8 | 0.00 | 44.0 | 14.0 | 163.0 | 2.0 | 164.2 | 1.0 | |
SKC-5-3 | 6.53 | 98.23 | 265.51 | 0.37 | 0.047 6 | 0.00 | 0.173 5 | 0.00 | 0.025 3 | 0.00 | 77.0 | 12.0 | 162.0 | 1.0 | 161.2 | 0.9 | |
SKC-5-4 | 3.71 | 84.78 | 150.46 | 0.56 | 0.047 0 | 0.00 | 0.172 4 | 0.00 | 0.025 5 | 0.00 | 50.0 | 14.0 | 162.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-6 | 5.03 | 106.68 | 205.31 | 0.52 | 0.046 9 | 0.00 | 0.170 5 | 0.00 | 0.025 2 | 0.00 | 46.0 | 12.0 | 160.0 | 1.0 | 160.5 | 1.0 | |
SKC-5-7 | 5.14 | 93.99 | 207.28 | 0.45 | 0.047 1 | 0.00 | 0.172 8 | 0.00 | 0.025 5 | 0.00 | 56.0 | 12.0 | 162.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-8 | 3.59 | 70.20 | 145.59 | 0.48 | 0.049 2 | 0.00 | 0.180 3 | 0.00 | 0.025 4 | 0.00 | 157.0 | 21.0 | 168.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-9 | 8.05 | 132.21 | 325.67 | 0.41 | 0.048 0 | 0.00 | 0.175 5 | 0.00 | 0.025 4 | 0.00 | 100.0 | 14.0 | 164.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-10 | 4.84 | 127.53 | 200.27 | 0.64 | 0.049 5 | 0.00 | 0.181 2 | 0.00 | 0.025 4 | 0.00 | 171.0 | 16.0 | 169.0 | 2.0 | 162.0 | 2.0 | |
SKC-5-11 | 6.80 | 139.53 | 273.60 | 0.51 | 0.047 9 | 0.00 | 0.172 9 | 0.00 | 0.025 8 | 0.00 | 93.0 | 12.0 | 162.0 | 2.0 | 164.0 | 2.0 | |
SKC-5-12 | 5.56 | 117.00 | 224.15 | 0.52 | 0.047 1 | 0.00 | 0.169 3 | 0.00 | 0.025 7 | 0.00 | 56.0 | 15.0 | 159.0 | 2.0 | 163.0 | 1.0 | |
SKC-5-13 | 6.68 | 183.19 | 269.70 | 0.68 | 0.048 0 | 0.00 | 0.174 6 | 0.00 | 0.026 0 | 0.00 | 98.0 | 15.0 | 163.0 | 2.0 | 165.0 | 2.0 | |
SKC-5-14 | 7.30 | 198.29 | 295.68 | 0.67 | 0.049 3 | 0.00 | 0.176 0 | 0.00 | 0.025 5 | 0.00 | 161.0 | 12.0 | 165.0 | 2.0 | 163.0 | 1.0 | |
SKC-5-15 | 7.04 | 166.20 | 280.12 | 0.59 | 0.048 2 | 0.00 | 0.175 4 | 0.00 | 0.026 0 | 0.00 | 110.0 | 12.0 | 164.0 | 2.0 | 165.0 | 1.0 | |
SKC-5-16 | 6.36 | 140.55 | 253.76 | 0.55 | 0.047 7 | 0.00 | 0.173 0 | 0.00 | 0.026 0 | 0.00 | 82.0 | 12.0 | 162.0 | 2.0 | 165.0 | 1.0 | |
SKC-5-17 | 6.11 | 137.03 | 248.71 | 0.55 | 0.047 7 | 0.00 | 0.171 1 | 0.00 | 0.025 6 | 0.00 | 86.0 | 11.0 | 160.0 | 1.0 | 163.0 | 1.0 | |
SKC-5-18 | 8.64 | 168.49 | 347.55 | 0.48 | 0.047 4 | 0.00 | 0.169 9 | 0.00 | 0.025 6 | 0.00 | 69.0 | 11.0 | 159.0 | 1.0 | 163.0 | 1.0 | |
SKC-5-19 | 5.98 | 158.51 | 237.47 | 0.67 | 0.047 3 | 0.00 | 0.171 6 | 0.00 | 0.025 9 | 0.00 | 65.0 | 14.0 | 161.0 | 2.0 | 165.0 | 1.0 | |
SKC-4-1 | 8.26 | 362.00 | 346.85 | 1.04 | 0.047 7 | 0.00 | 0.173 5 | 0.00 | 0.024 9 | 0.00 | 84.0 | 10.0 | 162.0 | 1.0 | 158.5 | 1.0 | |
SKC-4-2 | 6.45 | 181.83 | 280.59 | 0.65 | 0.047 9 | 0.00 | 0.169 7 | 0.00 | 0.024 2 | 0.00 | 93.0 | 11.0 | 159.0 | 1.0 | 154.4 | 0.9 | |
SKC-4-3 | 6.05 | 137.12 | 258.10 | 0.53 | 0.046 7 | 0.00 | 0.169 6 | 0.00 | 0.024 8 | 0.00 | 36.0 | 10.0 | 159.0 | 1.0 | 158.0 | 1.0 | |
SKC-4-4 | 4.89 | 146.97 | 208.03 | 0.71 | 0.047 9 | 0.00 | 0.173 7 | 0.00 | 0.024 7 | 0.00 | 93.0 | 24.0 | 163.0 | 2.0 | 158.0 | 1.0 | |
SKC-4-5 | 6.66 | 111.07 | 283.48 | 0.39 | 0.047 0 | 0.00 | 0.170 2 | 0.00 | 0.024 7 | 0.00 | 51.0 | 12.0 | 160.0 | 2.0 | 158.0 | 1.0 | |
SKC-4-6 | 4.57 | 126.63 | 195.96 | 0.65 | 0.047 4 | 0.00 | 0.170 3 | 0.00 | 0.024 6 | 0.00 | 72.0 | 13.0 | 160.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-7 | 4.09 | 93.62 | 175.43 | 0.53 | 0.046 7 | 0.00 | 0.168 7 | 0.00 | 0.024 7 | 0.00 | 32.0 | 13.0 | 158.0 | 2.0 | 157.0 | 1.0 | |
SKC-4-8 | 7.54 | 137.37 | 327.21 | 0.42 | 0.047 7 | 0.00 | 0.169 7 | 0.00 | 0.024 4 | 0.00 | 84.0 | 9.0 | 159.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-9 | 3.48 | 85.91 | 150.59 | 0.57 | 0.047 3 | 0.00 | 0.169 6 | 0.00 | 0.024 6 | 0.00 | 62.0 | 14.0 | 159.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-10 | 6.25 | 121.29 | 271.77 | 0.45 | 0.047 7 | 0.00 | 0.169 2 | 0.00 | 0.024 7 | 0.00 | 86.0 | 13.0 | 159.0 | 1.0 | 157.5 | 1.0 | |
SKC-4-11 | 7.67 | 183.40 | 327.68 | 0.56 | 0.047 5 | 0.00 | 0.177 0 | 0.00 | 0.024 8 | 0.00 | 73.0 | 9.0 | 166.0 | 1.0 | 158.0 | 1.0 | |
SKC-4-12 | 5.05 | 80.55 | 213.60 | 0.38 | 0.047 0 | 0.00 | 0.175 0 | 0.00 | 0.024 7 | 0.00 | 51.0 | 11.0 | 164.0 | 1.0 | 157.4 | 1.0 | |
SKC-4-13 | 4.91 | 84.25 | 209.23 | 0.40 | 0.047 5 | 0.00 | 0.177 8 | 0.00 | 0.024 9 | 0.00 | 74.0 | 11.0 | 166.0 | 1.0 | 158.0 | 1.0 | |
测点编号 | 元素含量/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||
206Pb | 232Th | 238U | 232Th/238U | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||
SKC-4-14 | 9.18 | 239.73 | 397.65 | 0.60 | 0.047 3 | 0.00 | 0.173 1 | 0.00 | 0.024 3 | 0.00 | 65.0 | 9.0 | 162.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-15 | 5.18 | 93.07 | 224.58 | 0.41 | 0.048 5 | 0.00 | 0.182 9 | 0.01 | 0.024 6 | 0.00 | 126.0 | 98.0 | 171.0 | 8.0 | 157.0 | 1.0 | |
SKC-4-16 | 3.66 | 91.03 | 158.86 | 0.57 | 0.047 4 | 0.00 | 0.171 7 | 0.00 | 0.024 1 | 0.00 | 70.0 | 12.0 | 161.0 | 1.0 | 153.4 | 0.9 | |
SKC-4-17 | 5.50 | 149.79 | 240.87 | 0.62 | 0.047 2 | 0.00 | 0.171 0 | 0.00 | 0.024 1 | 0.00 | 59.0 | 11.0 | 160.0 | 1.0 | 153.3 | 0.9 | |
SKC-4-20 | 4.94 | 127.20 | 207.89 | 0.61 | 0.047 6 | 0.00 | 0.178 5 | 0.00 | 0.024 9 | 0.00 | 81.0 | 11.0 | 167.0 | 2.0 | 159.0 | 1.0 | |
SKC-4-21 | 5.71 | 178.30 | 244.08 | 0.73 | 0.047 1 | 0.00 | 0.169 0 | 0.00 | 0.024 6 | 0.00 | 52.0 | 10.0 | 159.0 | 1.0 | 156.5 | 0.9 | |
SKC-4-22 | 3.64 | 104.32 | 156.36 | 0.67 | 0.046 7 | 0.00 | 0.159 7 | 0.00 | 0.024 6 | 0.00 | 35.0 | 15.0 | 150.0 | 2.0 | 157.0 | 1.0 | |
SKC-4-23 | 5.16 | 152.47 | 223.85 | 0.68 | 0.047 1 | 0.00 | 0.160 1 | 0.00 | 0.024 4 | 0.00 | 56.0 | 13.0 | 151.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-24 | 8.56 | 317.81 | 363.86 | 0.87 | 0.046 6 | 0.00 | 0.160 0 | 0.00 | 0.024 7 | 0.00 | 31.0 | 10.0 | 151.0 | 1.0 | 157.0 | 0.9 | |
SKC-4-25 | 4.39 | 74.40 | 189.10 | 0.39 | 0.047 7 | 0.00 | 0.162 8 | 0.00 | 0.024 5 | 0.00 | 82.0 | 15.0 | 153.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-26 | 4.68 | 82.39 | 202.70 | 0.41 | 0.047 4 | 0.00 | 0.163 0 | 0.00 | 0.024 7 | 0.00 | 71.0 | 13.0 | 153.0 | 2.0 | 157.0 | 1.0 | |
SKC-4-27 | 4.31 | 82.38 | 187.82 | 0.44 | 0.047 2 | 0.00 | 0.159 9 | 0.00 | 0.024 4 | 0.00 | 62.0 | 12.0 | 151.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-28 | 3.61 | 112.13 | 157.55 | 0.71 | 0.047 5 | 0.00 | 0.162 0 | 0.00 | 0.024 5 | 0.00 | 74.0 | 17.0 | 152.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-29 | 7.76 | 211.75 | 344.34 | 0.61 | 0.047 1 | 0.00 | 0.157 7 | 0.00 | 0.024 0 | 0.00 | 56.0 | 13.0 | 149.0 | 1.0 | 153.0 | 1.0 | |
SKC-4-30 | 4.72 | 94.25 | 201.64 | 0.47 | 0.046 7 | 0.00 | 0.160 4 | 0.00 | 0.024 7 | 0.00 | 32.0 | 13.0 | 151.0 | 2.0 | 157.0 | 1.0 |
Table 1 LA-MC-ICP-MS zircon dating result of the Laoyachao and Yagongtang plutons
测点编号 | 元素含量/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb | 232Th | 238U | 232Th/238U | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||
SKC-5-1 | 5.63 | 120.87 | 231.98 | 0.52 | 0.047 1 | 0.00 | 0.172 5 | 0.00 | 0.025 4 | 0.00 | 52.0 | 13.0 | 162.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-2 | 4.73 | 93.88 | 190.15 | 0.49 | 0.046 9 | 0.00 | 0.174 3 | 0.00 | 0.025 8 | 0.00 | 44.0 | 14.0 | 163.0 | 2.0 | 164.2 | 1.0 | |
SKC-5-3 | 6.53 | 98.23 | 265.51 | 0.37 | 0.047 6 | 0.00 | 0.173 5 | 0.00 | 0.025 3 | 0.00 | 77.0 | 12.0 | 162.0 | 1.0 | 161.2 | 0.9 | |
SKC-5-4 | 3.71 | 84.78 | 150.46 | 0.56 | 0.047 0 | 0.00 | 0.172 4 | 0.00 | 0.025 5 | 0.00 | 50.0 | 14.0 | 162.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-6 | 5.03 | 106.68 | 205.31 | 0.52 | 0.046 9 | 0.00 | 0.170 5 | 0.00 | 0.025 2 | 0.00 | 46.0 | 12.0 | 160.0 | 1.0 | 160.5 | 1.0 | |
SKC-5-7 | 5.14 | 93.99 | 207.28 | 0.45 | 0.047 1 | 0.00 | 0.172 8 | 0.00 | 0.025 5 | 0.00 | 56.0 | 12.0 | 162.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-8 | 3.59 | 70.20 | 145.59 | 0.48 | 0.049 2 | 0.00 | 0.180 3 | 0.00 | 0.025 4 | 0.00 | 157.0 | 21.0 | 168.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-9 | 8.05 | 132.21 | 325.67 | 0.41 | 0.048 0 | 0.00 | 0.175 5 | 0.00 | 0.025 4 | 0.00 | 100.0 | 14.0 | 164.0 | 2.0 | 162.0 | 1.0 | |
SKC-5-10 | 4.84 | 127.53 | 200.27 | 0.64 | 0.049 5 | 0.00 | 0.181 2 | 0.00 | 0.025 4 | 0.00 | 171.0 | 16.0 | 169.0 | 2.0 | 162.0 | 2.0 | |
SKC-5-11 | 6.80 | 139.53 | 273.60 | 0.51 | 0.047 9 | 0.00 | 0.172 9 | 0.00 | 0.025 8 | 0.00 | 93.0 | 12.0 | 162.0 | 2.0 | 164.0 | 2.0 | |
SKC-5-12 | 5.56 | 117.00 | 224.15 | 0.52 | 0.047 1 | 0.00 | 0.169 3 | 0.00 | 0.025 7 | 0.00 | 56.0 | 15.0 | 159.0 | 2.0 | 163.0 | 1.0 | |
SKC-5-13 | 6.68 | 183.19 | 269.70 | 0.68 | 0.048 0 | 0.00 | 0.174 6 | 0.00 | 0.026 0 | 0.00 | 98.0 | 15.0 | 163.0 | 2.0 | 165.0 | 2.0 | |
SKC-5-14 | 7.30 | 198.29 | 295.68 | 0.67 | 0.049 3 | 0.00 | 0.176 0 | 0.00 | 0.025 5 | 0.00 | 161.0 | 12.0 | 165.0 | 2.0 | 163.0 | 1.0 | |
SKC-5-15 | 7.04 | 166.20 | 280.12 | 0.59 | 0.048 2 | 0.00 | 0.175 4 | 0.00 | 0.026 0 | 0.00 | 110.0 | 12.0 | 164.0 | 2.0 | 165.0 | 1.0 | |
SKC-5-16 | 6.36 | 140.55 | 253.76 | 0.55 | 0.047 7 | 0.00 | 0.173 0 | 0.00 | 0.026 0 | 0.00 | 82.0 | 12.0 | 162.0 | 2.0 | 165.0 | 1.0 | |
SKC-5-17 | 6.11 | 137.03 | 248.71 | 0.55 | 0.047 7 | 0.00 | 0.171 1 | 0.00 | 0.025 6 | 0.00 | 86.0 | 11.0 | 160.0 | 1.0 | 163.0 | 1.0 | |
SKC-5-18 | 8.64 | 168.49 | 347.55 | 0.48 | 0.047 4 | 0.00 | 0.169 9 | 0.00 | 0.025 6 | 0.00 | 69.0 | 11.0 | 159.0 | 1.0 | 163.0 | 1.0 | |
SKC-5-19 | 5.98 | 158.51 | 237.47 | 0.67 | 0.047 3 | 0.00 | 0.171 6 | 0.00 | 0.025 9 | 0.00 | 65.0 | 14.0 | 161.0 | 2.0 | 165.0 | 1.0 | |
SKC-4-1 | 8.26 | 362.00 | 346.85 | 1.04 | 0.047 7 | 0.00 | 0.173 5 | 0.00 | 0.024 9 | 0.00 | 84.0 | 10.0 | 162.0 | 1.0 | 158.5 | 1.0 | |
SKC-4-2 | 6.45 | 181.83 | 280.59 | 0.65 | 0.047 9 | 0.00 | 0.169 7 | 0.00 | 0.024 2 | 0.00 | 93.0 | 11.0 | 159.0 | 1.0 | 154.4 | 0.9 | |
SKC-4-3 | 6.05 | 137.12 | 258.10 | 0.53 | 0.046 7 | 0.00 | 0.169 6 | 0.00 | 0.024 8 | 0.00 | 36.0 | 10.0 | 159.0 | 1.0 | 158.0 | 1.0 | |
SKC-4-4 | 4.89 | 146.97 | 208.03 | 0.71 | 0.047 9 | 0.00 | 0.173 7 | 0.00 | 0.024 7 | 0.00 | 93.0 | 24.0 | 163.0 | 2.0 | 158.0 | 1.0 | |
SKC-4-5 | 6.66 | 111.07 | 283.48 | 0.39 | 0.047 0 | 0.00 | 0.170 2 | 0.00 | 0.024 7 | 0.00 | 51.0 | 12.0 | 160.0 | 2.0 | 158.0 | 1.0 | |
SKC-4-6 | 4.57 | 126.63 | 195.96 | 0.65 | 0.047 4 | 0.00 | 0.170 3 | 0.00 | 0.024 6 | 0.00 | 72.0 | 13.0 | 160.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-7 | 4.09 | 93.62 | 175.43 | 0.53 | 0.046 7 | 0.00 | 0.168 7 | 0.00 | 0.024 7 | 0.00 | 32.0 | 13.0 | 158.0 | 2.0 | 157.0 | 1.0 | |
SKC-4-8 | 7.54 | 137.37 | 327.21 | 0.42 | 0.047 7 | 0.00 | 0.169 7 | 0.00 | 0.024 4 | 0.00 | 84.0 | 9.0 | 159.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-9 | 3.48 | 85.91 | 150.59 | 0.57 | 0.047 3 | 0.00 | 0.169 6 | 0.00 | 0.024 6 | 0.00 | 62.0 | 14.0 | 159.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-10 | 6.25 | 121.29 | 271.77 | 0.45 | 0.047 7 | 0.00 | 0.169 2 | 0.00 | 0.024 7 | 0.00 | 86.0 | 13.0 | 159.0 | 1.0 | 157.5 | 1.0 | |
SKC-4-11 | 7.67 | 183.40 | 327.68 | 0.56 | 0.047 5 | 0.00 | 0.177 0 | 0.00 | 0.024 8 | 0.00 | 73.0 | 9.0 | 166.0 | 1.0 | 158.0 | 1.0 | |
SKC-4-12 | 5.05 | 80.55 | 213.60 | 0.38 | 0.047 0 | 0.00 | 0.175 0 | 0.00 | 0.024 7 | 0.00 | 51.0 | 11.0 | 164.0 | 1.0 | 157.4 | 1.0 | |
SKC-4-13 | 4.91 | 84.25 | 209.23 | 0.40 | 0.047 5 | 0.00 | 0.177 8 | 0.00 | 0.024 9 | 0.00 | 74.0 | 11.0 | 166.0 | 1.0 | 158.0 | 1.0 | |
测点编号 | 元素含量/10-6 | 同位素比值 | 年龄/Ma | ||||||||||||||
206Pb | 232Th | 238U | 232Th/238U | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/206Pb | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||
SKC-4-14 | 9.18 | 239.73 | 397.65 | 0.60 | 0.047 3 | 0.00 | 0.173 1 | 0.00 | 0.024 3 | 0.00 | 65.0 | 9.0 | 162.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-15 | 5.18 | 93.07 | 224.58 | 0.41 | 0.048 5 | 0.00 | 0.182 9 | 0.01 | 0.024 6 | 0.00 | 126.0 | 98.0 | 171.0 | 8.0 | 157.0 | 1.0 | |
SKC-4-16 | 3.66 | 91.03 | 158.86 | 0.57 | 0.047 4 | 0.00 | 0.171 7 | 0.00 | 0.024 1 | 0.00 | 70.0 | 12.0 | 161.0 | 1.0 | 153.4 | 0.9 | |
SKC-4-17 | 5.50 | 149.79 | 240.87 | 0.62 | 0.047 2 | 0.00 | 0.171 0 | 0.00 | 0.024 1 | 0.00 | 59.0 | 11.0 | 160.0 | 1.0 | 153.3 | 0.9 | |
SKC-4-20 | 4.94 | 127.20 | 207.89 | 0.61 | 0.047 6 | 0.00 | 0.178 5 | 0.00 | 0.024 9 | 0.00 | 81.0 | 11.0 | 167.0 | 2.0 | 159.0 | 1.0 | |
SKC-4-21 | 5.71 | 178.30 | 244.08 | 0.73 | 0.047 1 | 0.00 | 0.169 0 | 0.00 | 0.024 6 | 0.00 | 52.0 | 10.0 | 159.0 | 1.0 | 156.5 | 0.9 | |
SKC-4-22 | 3.64 | 104.32 | 156.36 | 0.67 | 0.046 7 | 0.00 | 0.159 7 | 0.00 | 0.024 6 | 0.00 | 35.0 | 15.0 | 150.0 | 2.0 | 157.0 | 1.0 | |
SKC-4-23 | 5.16 | 152.47 | 223.85 | 0.68 | 0.047 1 | 0.00 | 0.160 1 | 0.00 | 0.024 4 | 0.00 | 56.0 | 13.0 | 151.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-24 | 8.56 | 317.81 | 363.86 | 0.87 | 0.046 6 | 0.00 | 0.160 0 | 0.00 | 0.024 7 | 0.00 | 31.0 | 10.0 | 151.0 | 1.0 | 157.0 | 0.9 | |
SKC-4-25 | 4.39 | 74.40 | 189.10 | 0.39 | 0.047 7 | 0.00 | 0.162 8 | 0.00 | 0.024 5 | 0.00 | 82.0 | 15.0 | 153.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-26 | 4.68 | 82.39 | 202.70 | 0.41 | 0.047 4 | 0.00 | 0.163 0 | 0.00 | 0.024 7 | 0.00 | 71.0 | 13.0 | 153.0 | 2.0 | 157.0 | 1.0 | |
SKC-4-27 | 4.31 | 82.38 | 187.82 | 0.44 | 0.047 2 | 0.00 | 0.159 9 | 0.00 | 0.024 4 | 0.00 | 62.0 | 12.0 | 151.0 | 1.0 | 155.0 | 1.0 | |
SKC-4-28 | 3.61 | 112.13 | 157.55 | 0.71 | 0.047 5 | 0.00 | 0.162 0 | 0.00 | 0.024 5 | 0.00 | 74.0 | 17.0 | 152.0 | 2.0 | 156.0 | 1.0 | |
SKC-4-29 | 7.76 | 211.75 | 344.34 | 0.61 | 0.047 1 | 0.00 | 0.157 7 | 0.00 | 0.024 0 | 0.00 | 56.0 | 13.0 | 149.0 | 1.0 | 153.0 | 1.0 | |
SKC-4-30 | 4.72 | 94.25 | 201.64 | 0.47 | 0.046 7 | 0.00 | 0.160 4 | 0.00 | 0.024 7 | 0.00 | 32.0 | 13.0 | 151.0 | 2.0 | 157.0 | 1.0 |
成分 | 老鸭巢花岗闪长岩 | 鸭公塘花岗闪长岩 | |||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SKC2-3 | SKC2-4 | SKC2-5 | SKC2-6 | SKC2-7 | SKC2-8 | SKC2-9 | SKC2-10 | SKC-B5 | SKC-B4 | 喻亨祥-1 | 喻亨祥-2 | 喻亨祥-3 | 喻亨祥-4 | 喻亨祥-5 | |||||||||||||||||||||||||||||||||||
SiO2 | 55.44 | 59.45 | 57.56 | 55.17 | 51.79 | 60.39 | 53.10 | 50.11 | 58.91 | 60.21 | 59.52 | 55.61 | 51.34 | 57.01 | 59.31 | ||||||||||||||||||||||||||||||||||
Al2O3 | 17.63 | 16.60 | 15.63 | 19.51 | 14.96 | 16.57 | 17.84 | 12.62 | 13.93 | 19.84 | 14.29 | 14.65 | 14.25 | 14.69 | 15.10 | ||||||||||||||||||||||||||||||||||
Fe2O3T | 3.56 | 6.36 | 4.81 | 3.72 | 4.58 | 5.45 | 4.89 | 5.88 | 7.89 | 3.55 | 1.66 | 3.27 | 3.57 | 2.66 | 3.68 | ||||||||||||||||||||||||||||||||||
MgO | 3.13 | 2.85 | 1.28 | 1.32 | 1.32 | 1.88 | 1.35 | 1.26 | 1.91 | 0.48 | 1.72 | 2.43 | 2.43 | 2.58 | 2.25 | ||||||||||||||||||||||||||||||||||
CaO | 6.40 | 4.03 | 6.55 | 4.60 | 8.76 | 3.42 | 9.16 | 15.58 | 6.34 | 5.88 | 5.54 | 6.83 | 10.59 | 5.37 | 3.88 | ||||||||||||||||||||||||||||||||||
Na2O | 1.08 | 2.57 | 2.72 | 0.51 | 1.50 | 2.18 | 0.19 | 0.20 | 0.12 | 0.07 | 2.09 | 2.12 | 3.49 | 4.24 | 3.26 | ||||||||||||||||||||||||||||||||||
K2O | 4.67 | 2.21 | 4.96 | 7.02 | 7.77 | 4.73 | 3.53 | 1.96 | 2.72 | 1.25 | 2.67 | 3.70 | 1.57 | 1.93 | 3.06 | ||||||||||||||||||||||||||||||||||
MnO | 0.09 | 0.08 | 0.13 | 0.07 | 0.14 | 0.07 | 0.12 | 0.18 | 0.25 | 0.07 | 0.09 | 0.14 | 0.23 | 0.11 | 0.08 | ||||||||||||||||||||||||||||||||||
TiO2 | 0.68 | 0.86 | 0.80 | 0.86 | 0.72 | 0.81 | 0.72 | 0.41 | 0.31 | 0.66 | 0.50 | 0.64 | 0.64 | 0.62 | 0.51 | ||||||||||||||||||||||||||||||||||
P2O5 | 0.34 | 0.41 | 0.37 | 0.35 | 0.34 | 0.37 | 0.29 | 0.14 | 0.13 | 0.33 | 0.28 | 0.22 | 0.19 | 0.20 | 0.30 | ||||||||||||||||||||||||||||||||||
烧失量 | 6.91 | 4.30 | 5.13 | 6.63 | 7.84 | 4.05 | 8.79 | 11.16 | 7.23 | 7.35 | 6.68 | 6.69 | 8.28 | 6.26 | 5.21 | ||||||||||||||||||||||||||||||||||
成分 | 老鸭巢花岗闪长岩 | 鸭公塘花岗闪长岩 | |||||||||||||||||||||||||||||||||||||||||||||||
SKC2-3 | SKC2-4 | SKC2-5 | SKC2-6 | SKC2-7 | SKC2-8 | SKC2-9 | SKC2-10 | SKC-B5 | SKC-B4 | 喻亨祥-1 | 喻亨祥-2 | 喻亨祥-3 | 喻亨祥-4 | 喻亨祥-5 | |||||||||||||||||||||||||||||||||||
Li | 32.6 | 23.5 | 15.7 | 9.97 | 11.9 | 22.5 | 37.1 | 31.2 | 133 | 92.8 | |||||||||||||||||||||||||||||||||||||||
Be | 2.39 | 2.26 | 1.29 | 2.32 | 1.97 | 2.07 | 2.22 | 1.33 | 2 | 1.66 | |||||||||||||||||||||||||||||||||||||||
Sc | 15.4 | 16.4 | 17.8 | 20.7 | 19.2 | 19.2 | 18.3 | 12.3 | 5.44 | 17.4 | |||||||||||||||||||||||||||||||||||||||
V | 117 | 134 | 145 | 162 | 162 | 135 | 137 | 85.2 | 56 | 126 | |||||||||||||||||||||||||||||||||||||||
Cr | 105 | 150 | 133 | 155 | 97.9 | 203 | 203 | 179 | 13.3 | 32.6 | |||||||||||||||||||||||||||||||||||||||
Co | 15.5 | 13 | 12 | 12.8 | 12 | 16.3 | 16.3 | 15.4 | 5.07 | 9.94 | |||||||||||||||||||||||||||||||||||||||
Ni | 8.74 | 11.8 | 15.3 | 19.7 | 11.8 | 12.8 | 11.5 | 16 | 7.15 | 7.98 | |||||||||||||||||||||||||||||||||||||||
Cu | 33.2 | 37.5 | 53.4 | 48.2 | 59.8 | 139 | 48.3 | 174 | 78.5 | 203 | |||||||||||||||||||||||||||||||||||||||
Zn | 61 | 96.8 | 688 | 857 | 278 | 603 | 1 604 | 3 326 | 288 | 87.1 | |||||||||||||||||||||||||||||||||||||||
Ga | 17.6 | 17.9 | 16.9 | 21.5 | 18.7 | 18.6 | 19.3 | 12.3 | 18.5 | 20.3 | |||||||||||||||||||||||||||||||||||||||
Rb | 173 | 97.8 | 185 | 240 | 258 | 173 | 209 | 66.2 | 106 | 47.1 | |||||||||||||||||||||||||||||||||||||||
Sr | 205 | 246 | 217 | 152 | 451 | 247 | 46.5 | 50.7 | 40.6 | 27.3 | |||||||||||||||||||||||||||||||||||||||
Y | 26.4 | 17 | 20 | 17.9 | 33.6 | 22.5 | 22.8 | 21.3 | 16 | 22.6 | |||||||||||||||||||||||||||||||||||||||
Nb | 13.4 | 14.7 | 14.3 | 15.7 | 14.1 | 15 | 13.8 | 10.3 | 11.2 | 14.6 | |||||||||||||||||||||||||||||||||||||||
Mo | 2.26 | 1.94 | 3.24 | 3.54 | 3.28 | 3.49 | 3.55 | 18.3 | 15.9 | 37 | |||||||||||||||||||||||||||||||||||||||
Cd | 0.237 | 0.086 | 1.91 | 2.68 | 0.55 | 0.651 | 6.84 | 13.8 | 0.554 | 0.225 | |||||||||||||||||||||||||||||||||||||||
In | 0.117 | 0.064 | 0.148 | 0.473 | 0.077 | 0.052 | 0.145 | 1.83 | 0.247 | 0.053 | |||||||||||||||||||||||||||||||||||||||
Sb | 4.88 | 2.68 | 7.7 | 6.07 | 25.5 | 18.6 | 5.9 | 30 | 18.7 | 3.66 | |||||||||||||||||||||||||||||||||||||||
Cs | 32.3 | 14.3 | 7.88 | 17.9 | 15.7 | 15.8 | 14.8 | 11.7 | 13.7 | 9.73 | |||||||||||||||||||||||||||||||||||||||
Ba | 546 | 241 | 542 | 591 | 1202 | 611 | 45.5 | 44.9 | 30.5 | 78.5 | |||||||||||||||||||||||||||||||||||||||
La | 41.5 | 34.9 | 41.1 | 36.9 | 46 | 44.4 | 66.9 | 35.6 | 35.2 | 40 | |||||||||||||||||||||||||||||||||||||||
Ce | 79.3 | 64.5 | 76.9 | 69.7 | 86.4 | 83.1 | 124 | 67.3 | 53.4 | 77.2 | |||||||||||||||||||||||||||||||||||||||
Pr | 9.51 | 7.23 | 8.86 | 8.09 | 10.3 | 9.76 | 14.6 | 7.72 | 5.78 | 9.1 | |||||||||||||||||||||||||||||||||||||||
Nd | 37.7 | 27.6 | 34 | 30 | 40.7 | 37 | 58 | 29.3 | 19.7 | 34.9 | |||||||||||||||||||||||||||||||||||||||
Sm | 7.2 | 5.15 | 6.39 | 5.35 | 7.91 | 6.74 | 9.95 | 5.4 | 3.51 | 6.57 | |||||||||||||||||||||||||||||||||||||||
Eu | 1.82 | 1.73 | 1.43 | 1.09 | 2.18 | 1.69 | 2.54 | 1.4 | 1.06 | 1.41 | |||||||||||||||||||||||||||||||||||||||
Gd | 6.19 | 4.23 | 5.08 | 4.63 | 6.92 | 5.43 | 7.42 | 4.74 | 3.23 | 5.75 | |||||||||||||||||||||||||||||||||||||||
Tb | 1.01 | 0.68 | 0.795 | 0.721 | 1.16 | 0.866 | 1.05 | 0.749 | 0.54 | 0.976 | |||||||||||||||||||||||||||||||||||||||
Dy | 5.47 | 3.85 | 4.13 | 3.73 | 6.41 | 4.91 | 5.33 | 4.36 | 3.24 | 4.89 | |||||||||||||||||||||||||||||||||||||||
Ho | 0.948 | 0.64 | 0.762 | 0.646 | 1.21 | 0.82 | 0.888 | 0.786 | 0.588 | 0.882 | |||||||||||||||||||||||||||||||||||||||
Er | 2.81 | 1.95 | 2.37 | 2.02 | 3.6 | 2.56 | 2.46 | 2.37 | 1.83 | 2.56 | |||||||||||||||||||||||||||||||||||||||
Tm | 0.483 | 0.302 | 0.364 | 0.299 | 0.588 | 0.395 | 0.372 | 0.383 | 0.295 | 0.422 | |||||||||||||||||||||||||||||||||||||||
Yb | 3.21 | 1.92 | 2.52 | 2.03 | 4.12 | 2.44 | 2.46 | 2.93 | 1.79 | 2.49 | |||||||||||||||||||||||||||||||||||||||
Lu | 0.475 | 0.272 | 0.375 | 0.311 | 0.607 | 0.408 | 0.373 | 0.423 | 0.294 | 0.385 | |||||||||||||||||||||||||||||||||||||||
成分 | 老鸭巢花岗闪长岩 | 鸭公塘花岗闪长岩 | |||||||||||||||||||||||||||||||||||||||||||||||
SKC2-3 | SKC2-4 | SKC2-5 | SKC2-6 | SKC2-7 | SKC2-8 | SKC2-9 | SKC2-10 | SKC-B5 | SKC-B4 | 喻亨祥-1 | 喻亨祥-2 | 喻亨祥-3 | 喻亨祥-4 | 喻亨祥-5 | |||||||||||||||||||||||||||||||||||
Ta | 1.21 | 1.17 | 1.18 | 1.21 | 1.27 | 1.25 | 1.06 | 1.28 | 1.22 | 1.15 | |||||||||||||||||||||||||||||||||||||||
W | 7.8 | 9.65 | 11.8 | 19.7 | 7.28 | 15.8 | 27.5 | 20.3 | 56.5 | 5.73 | |||||||||||||||||||||||||||||||||||||||
Re | 0.017 | 0.022 | 0.02 | 0.038 | 0.015 | 0.026 | 0.038 | 0.052 | 0.011 | 0.015 | |||||||||||||||||||||||||||||||||||||||
Tl | 1.36 | 0.738 | 0.889 | 1.45 | 0.876 | 0.764 | 1.62 | 0.686 | |||||||||||||||||||||||||||||||||||||||||
Pb | 23.8 | 12.4 | 29.4 | 145 | 47.6 | 21.9 | 246 | 710 | 37.4 | 34.2 | |||||||||||||||||||||||||||||||||||||||
Bi | 1.18 | 0.601 | 1 | 1.16 | 0.657 | 0.553 | 2.5 | 62.7 | |||||||||||||||||||||||||||||||||||||||||
Th | 12.6 | 16.8 | 18.2 | 15.6 | 20.2 | 16.5 | 12.2 | 18.4 | 26.3 | 15 | |||||||||||||||||||||||||||||||||||||||
U | 2.81 | 3.43 | 3.84 | 14.8 | 4.13 | 3.61 | 4.98 | 4.24 | 2.04 | 1.99 | |||||||||||||||||||||||||||||||||||||||
Zr | 120 | 94.9 | 98.3 | 93.2 | 126 | 96.7 | 92.1 | 117 | 104 | 80.8 | |||||||||||||||||||||||||||||||||||||||
Hf | 6.03 | 4.38 | 5.03 | 4.32 | 5.35 | 4.2 | 4.14 | 5.27 | 3.58 | 2.66 |
Table 2 Major and trace elements compositions of the Laoyachao and Yagongtang plutons
成分 | 老鸭巢花岗闪长岩 | 鸭公塘花岗闪长岩 | |||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SKC2-3 | SKC2-4 | SKC2-5 | SKC2-6 | SKC2-7 | SKC2-8 | SKC2-9 | SKC2-10 | SKC-B5 | SKC-B4 | 喻亨祥-1 | 喻亨祥-2 | 喻亨祥-3 | 喻亨祥-4 | 喻亨祥-5 | |||||||||||||||||||||||||||||||||||
SiO2 | 55.44 | 59.45 | 57.56 | 55.17 | 51.79 | 60.39 | 53.10 | 50.11 | 58.91 | 60.21 | 59.52 | 55.61 | 51.34 | 57.01 | 59.31 | ||||||||||||||||||||||||||||||||||
Al2O3 | 17.63 | 16.60 | 15.63 | 19.51 | 14.96 | 16.57 | 17.84 | 12.62 | 13.93 | 19.84 | 14.29 | 14.65 | 14.25 | 14.69 | 15.10 | ||||||||||||||||||||||||||||||||||
Fe2O3T | 3.56 | 6.36 | 4.81 | 3.72 | 4.58 | 5.45 | 4.89 | 5.88 | 7.89 | 3.55 | 1.66 | 3.27 | 3.57 | 2.66 | 3.68 | ||||||||||||||||||||||||||||||||||
MgO | 3.13 | 2.85 | 1.28 | 1.32 | 1.32 | 1.88 | 1.35 | 1.26 | 1.91 | 0.48 | 1.72 | 2.43 | 2.43 | 2.58 | 2.25 | ||||||||||||||||||||||||||||||||||
CaO | 6.40 | 4.03 | 6.55 | 4.60 | 8.76 | 3.42 | 9.16 | 15.58 | 6.34 | 5.88 | 5.54 | 6.83 | 10.59 | 5.37 | 3.88 | ||||||||||||||||||||||||||||||||||
Na2O | 1.08 | 2.57 | 2.72 | 0.51 | 1.50 | 2.18 | 0.19 | 0.20 | 0.12 | 0.07 | 2.09 | 2.12 | 3.49 | 4.24 | 3.26 | ||||||||||||||||||||||||||||||||||
K2O | 4.67 | 2.21 | 4.96 | 7.02 | 7.77 | 4.73 | 3.53 | 1.96 | 2.72 | 1.25 | 2.67 | 3.70 | 1.57 | 1.93 | 3.06 | ||||||||||||||||||||||||||||||||||
MnO | 0.09 | 0.08 | 0.13 | 0.07 | 0.14 | 0.07 | 0.12 | 0.18 | 0.25 | 0.07 | 0.09 | 0.14 | 0.23 | 0.11 | 0.08 | ||||||||||||||||||||||||||||||||||
TiO2 | 0.68 | 0.86 | 0.80 | 0.86 | 0.72 | 0.81 | 0.72 | 0.41 | 0.31 | 0.66 | 0.50 | 0.64 | 0.64 | 0.62 | 0.51 | ||||||||||||||||||||||||||||||||||
P2O5 | 0.34 | 0.41 | 0.37 | 0.35 | 0.34 | 0.37 | 0.29 | 0.14 | 0.13 | 0.33 | 0.28 | 0.22 | 0.19 | 0.20 | 0.30 | ||||||||||||||||||||||||||||||||||
烧失量 | 6.91 | 4.30 | 5.13 | 6.63 | 7.84 | 4.05 | 8.79 | 11.16 | 7.23 | 7.35 | 6.68 | 6.69 | 8.28 | 6.26 | 5.21 | ||||||||||||||||||||||||||||||||||
成分 | 老鸭巢花岗闪长岩 | 鸭公塘花岗闪长岩 | |||||||||||||||||||||||||||||||||||||||||||||||
SKC2-3 | SKC2-4 | SKC2-5 | SKC2-6 | SKC2-7 | SKC2-8 | SKC2-9 | SKC2-10 | SKC-B5 | SKC-B4 | 喻亨祥-1 | 喻亨祥-2 | 喻亨祥-3 | 喻亨祥-4 | 喻亨祥-5 | |||||||||||||||||||||||||||||||||||
Li | 32.6 | 23.5 | 15.7 | 9.97 | 11.9 | 22.5 | 37.1 | 31.2 | 133 | 92.8 | |||||||||||||||||||||||||||||||||||||||
Be | 2.39 | 2.26 | 1.29 | 2.32 | 1.97 | 2.07 | 2.22 | 1.33 | 2 | 1.66 | |||||||||||||||||||||||||||||||||||||||
Sc | 15.4 | 16.4 | 17.8 | 20.7 | 19.2 | 19.2 | 18.3 | 12.3 | 5.44 | 17.4 | |||||||||||||||||||||||||||||||||||||||
V | 117 | 134 | 145 | 162 | 162 | 135 | 137 | 85.2 | 56 | 126 | |||||||||||||||||||||||||||||||||||||||
Cr | 105 | 150 | 133 | 155 | 97.9 | 203 | 203 | 179 | 13.3 | 32.6 | |||||||||||||||||||||||||||||||||||||||
Co | 15.5 | 13 | 12 | 12.8 | 12 | 16.3 | 16.3 | 15.4 | 5.07 | 9.94 | |||||||||||||||||||||||||||||||||||||||
Ni | 8.74 | 11.8 | 15.3 | 19.7 | 11.8 | 12.8 | 11.5 | 16 | 7.15 | 7.98 | |||||||||||||||||||||||||||||||||||||||
Cu | 33.2 | 37.5 | 53.4 | 48.2 | 59.8 | 139 | 48.3 | 174 | 78.5 | 203 | |||||||||||||||||||||||||||||||||||||||
Zn | 61 | 96.8 | 688 | 857 | 278 | 603 | 1 604 | 3 326 | 288 | 87.1 | |||||||||||||||||||||||||||||||||||||||
Ga | 17.6 | 17.9 | 16.9 | 21.5 | 18.7 | 18.6 | 19.3 | 12.3 | 18.5 | 20.3 | |||||||||||||||||||||||||||||||||||||||
Rb | 173 | 97.8 | 185 | 240 | 258 | 173 | 209 | 66.2 | 106 | 47.1 | |||||||||||||||||||||||||||||||||||||||
Sr | 205 | 246 | 217 | 152 | 451 | 247 | 46.5 | 50.7 | 40.6 | 27.3 | |||||||||||||||||||||||||||||||||||||||
Y | 26.4 | 17 | 20 | 17.9 | 33.6 | 22.5 | 22.8 | 21.3 | 16 | 22.6 | |||||||||||||||||||||||||||||||||||||||
Nb | 13.4 | 14.7 | 14.3 | 15.7 | 14.1 | 15 | 13.8 | 10.3 | 11.2 | 14.6 | |||||||||||||||||||||||||||||||||||||||
Mo | 2.26 | 1.94 | 3.24 | 3.54 | 3.28 | 3.49 | 3.55 | 18.3 | 15.9 | 37 | |||||||||||||||||||||||||||||||||||||||
Cd | 0.237 | 0.086 | 1.91 | 2.68 | 0.55 | 0.651 | 6.84 | 13.8 | 0.554 | 0.225 | |||||||||||||||||||||||||||||||||||||||
In | 0.117 | 0.064 | 0.148 | 0.473 | 0.077 | 0.052 | 0.145 | 1.83 | 0.247 | 0.053 | |||||||||||||||||||||||||||||||||||||||
Sb | 4.88 | 2.68 | 7.7 | 6.07 | 25.5 | 18.6 | 5.9 | 30 | 18.7 | 3.66 | |||||||||||||||||||||||||||||||||||||||
Cs | 32.3 | 14.3 | 7.88 | 17.9 | 15.7 | 15.8 | 14.8 | 11.7 | 13.7 | 9.73 | |||||||||||||||||||||||||||||||||||||||
Ba | 546 | 241 | 542 | 591 | 1202 | 611 | 45.5 | 44.9 | 30.5 | 78.5 | |||||||||||||||||||||||||||||||||||||||
La | 41.5 | 34.9 | 41.1 | 36.9 | 46 | 44.4 | 66.9 | 35.6 | 35.2 | 40 | |||||||||||||||||||||||||||||||||||||||
Ce | 79.3 | 64.5 | 76.9 | 69.7 | 86.4 | 83.1 | 124 | 67.3 | 53.4 | 77.2 | |||||||||||||||||||||||||||||||||||||||
Pr | 9.51 | 7.23 | 8.86 | 8.09 | 10.3 | 9.76 | 14.6 | 7.72 | 5.78 | 9.1 | |||||||||||||||||||||||||||||||||||||||
Nd | 37.7 | 27.6 | 34 | 30 | 40.7 | 37 | 58 | 29.3 | 19.7 | 34.9 | |||||||||||||||||||||||||||||||||||||||
Sm | 7.2 | 5.15 | 6.39 | 5.35 | 7.91 | 6.74 | 9.95 | 5.4 | 3.51 | 6.57 | |||||||||||||||||||||||||||||||||||||||
Eu | 1.82 | 1.73 | 1.43 | 1.09 | 2.18 | 1.69 | 2.54 | 1.4 | 1.06 | 1.41 | |||||||||||||||||||||||||||||||||||||||
Gd | 6.19 | 4.23 | 5.08 | 4.63 | 6.92 | 5.43 | 7.42 | 4.74 | 3.23 | 5.75 | |||||||||||||||||||||||||||||||||||||||
Tb | 1.01 | 0.68 | 0.795 | 0.721 | 1.16 | 0.866 | 1.05 | 0.749 | 0.54 | 0.976 | |||||||||||||||||||||||||||||||||||||||
Dy | 5.47 | 3.85 | 4.13 | 3.73 | 6.41 | 4.91 | 5.33 | 4.36 | 3.24 | 4.89 | |||||||||||||||||||||||||||||||||||||||
Ho | 0.948 | 0.64 | 0.762 | 0.646 | 1.21 | 0.82 | 0.888 | 0.786 | 0.588 | 0.882 | |||||||||||||||||||||||||||||||||||||||
Er | 2.81 | 1.95 | 2.37 | 2.02 | 3.6 | 2.56 | 2.46 | 2.37 | 1.83 | 2.56 | |||||||||||||||||||||||||||||||||||||||
Tm | 0.483 | 0.302 | 0.364 | 0.299 | 0.588 | 0.395 | 0.372 | 0.383 | 0.295 | 0.422 | |||||||||||||||||||||||||||||||||||||||
Yb | 3.21 | 1.92 | 2.52 | 2.03 | 4.12 | 2.44 | 2.46 | 2.93 | 1.79 | 2.49 | |||||||||||||||||||||||||||||||||||||||
Lu | 0.475 | 0.272 | 0.375 | 0.311 | 0.607 | 0.408 | 0.373 | 0.423 | 0.294 | 0.385 | |||||||||||||||||||||||||||||||||||||||
成分 | 老鸭巢花岗闪长岩 | 鸭公塘花岗闪长岩 | |||||||||||||||||||||||||||||||||||||||||||||||
SKC2-3 | SKC2-4 | SKC2-5 | SKC2-6 | SKC2-7 | SKC2-8 | SKC2-9 | SKC2-10 | SKC-B5 | SKC-B4 | 喻亨祥-1 | 喻亨祥-2 | 喻亨祥-3 | 喻亨祥-4 | 喻亨祥-5 | |||||||||||||||||||||||||||||||||||
Ta | 1.21 | 1.17 | 1.18 | 1.21 | 1.27 | 1.25 | 1.06 | 1.28 | 1.22 | 1.15 | |||||||||||||||||||||||||||||||||||||||
W | 7.8 | 9.65 | 11.8 | 19.7 | 7.28 | 15.8 | 27.5 | 20.3 | 56.5 | 5.73 | |||||||||||||||||||||||||||||||||||||||
Re | 0.017 | 0.022 | 0.02 | 0.038 | 0.015 | 0.026 | 0.038 | 0.052 | 0.011 | 0.015 | |||||||||||||||||||||||||||||||||||||||
Tl | 1.36 | 0.738 | 0.889 | 1.45 | 0.876 | 0.764 | 1.62 | 0.686 | |||||||||||||||||||||||||||||||||||||||||
Pb | 23.8 | 12.4 | 29.4 | 145 | 47.6 | 21.9 | 246 | 710 | 37.4 | 34.2 | |||||||||||||||||||||||||||||||||||||||
Bi | 1.18 | 0.601 | 1 | 1.16 | 0.657 | 0.553 | 2.5 | 62.7 | |||||||||||||||||||||||||||||||||||||||||
Th | 12.6 | 16.8 | 18.2 | 15.6 | 20.2 | 16.5 | 12.2 | 18.4 | 26.3 | 15 | |||||||||||||||||||||||||||||||||||||||
U | 2.81 | 3.43 | 3.84 | 14.8 | 4.13 | 3.61 | 4.98 | 4.24 | 2.04 | 1.99 | |||||||||||||||||||||||||||||||||||||||
Zr | 120 | 94.9 | 98.3 | 93.2 | 126 | 96.7 | 92.1 | 117 | 104 | 80.8 | |||||||||||||||||||||||||||||||||||||||
Hf | 6.03 | 4.38 | 5.03 | 4.32 | 5.35 | 4.2 | 4.14 | 5.27 | 3.58 | 2.66 |
Sample | t/Ma | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | εHf(0) | εHf(t) | TDM1/Ma | TDM2/Ma | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|---|---|
SKC-5-1 | 162.0 | 0.060 150 | 0.000 308 | 0.001 486 | 0.000 010 | 0.282 433 | 0.000 014 | -12.00 | -8.61 | 1 173 | 1 756 | -0.96 |
SKC-5-2 | 164.2 | 0.076 536 | 0.002 270 | 0.001 707 | 0.000 044 | 0.282 388 | 0.000 014 | -13.57 | -10.15 | 1 243 | 1 855 | -0.95 |
SKC-5-3 | 161.2 | 0.068 491 | 0.000 573 | 0.001 696 | 0.000 013 | 0.282 429 | 0.000 016 | -12.12 | -8.77 | 1 184 | 1 765 | -0.95 |
SKC-5-4 | 162.0 | 0.070 266 | 0.000 567 | 0.001 754 | 0.000 013 | 0.282 415 | 0.000 016 | -12.61 | -9.25 | 1 206 | 1 796 | -0.95 |
SKC-5-6 | 160.5 | 0.073 243 | 0.000 156 | 0.001 864 | 0.000 009 | 0.282 430 | 0.000 015 | -12.10 | -8.78 | 1 189 | 1 765 | -0.94 |
SKC-5-7 | 162.0 | 0.056 802 | 0.000 432 | 0.001 510 | 0.000 010 | 0.282 400 | 0.000 016 | -13.16 | -9.77 | 1 220 | 1 829 | -0.95 |
SKC-5-8 | 162.0 | 0.041 586 | 0.000 271 | 0.001 088 | 0.000 003 | 0.282 409 | 0.000 014 | -12.85 | -9.41 | 1 194 | 1 807 | -0.97 |
SKC-5-9 | 162.0 | 0.057 031 | 0.001 164 | 0.001 608 | 0.000 029 | 0.282 395 | 0.000 015 | -13.33 | -9.95 | 1 230 | 1 840 | -0.95 |
SKC-5-10 | 162.0 | 0.060 815 | 0.001 016 | 0.001 638 | 0.000 026 | 0.282 396 | 0.000 016 | -13.29 | -9.91 | 1 229 | 1 838 | -0.95 |
SKC-5-11 | 164.0 | 0.046 765 | 0.001 636 | 0.001 438 | 0.000 071 | 0.282 397 | 0.000 022 | -13.26 | -9.82 | 1 222 | 1 834 | -0.96 |
SKC-5-12 | 163.0 | 0.044 994 | 0.000 482 | 0.001 224 | 0.000 019 | 0.282 426 | 0.000 015 | -12.22 | -8.78 | 1 173 | 1 767 | -0.96 |
SKC-5-13 | 165.0 | 0.042 951 | 0.000 596 | 0.001 176 | 0.000 024 | 0.282 433 | 0.000 019 | -11.99 | -8.50 | 1 162 | 1 751 | -0.96 |
SKC-5-14 | 163.0 | 0.058 611 | 0.000 706 | 0.001 594 | 0.000 018 | 0.282 407 | 0.000 017 | -12.91 | -9.51 | 1 212 | 1 813 | -0.95 |
SKC-5-15 | 165.0 | 0.054 375 | 0.000 489 | 0.001 462 | 0.000 007 | 0.282 391 | 0.000 014 | -13.47 | -10.01 | 1 230 | 1 846 | -0.96 |
SKC-5-16 | 165.0 | 0.060 732 | 0.000 571 | 0.001 651 | 0.000 013 | 0.282 410 | 0.000 015 | -12.79 | -9.35 | 1 209 | 1 804 | -0.95 |
SKC-5-17 | 163.0 | 0.056 307 | 0.001 360 | 0.001 516 | 0.000 029 | 0.282 359 | 0.000 017 | -14.61 | -11.20 | 1 278 | 1 920 | -0.95 |
SKC-5-18 | 163.0 | 0.060 284 | 0.000 698 | 0.001 682 | 0.000 028 | 0.282 425 | 0.000 021 | -12.26 | -8.87 | 1 189 | 1 773 | -0.95 |
SKC-5-19 | 165.0 | 0.057 023 | 0.001 358 | 0.001 623 | 0.000 061 | 0.282 442 | 0.000 017 | -11.68 | -8.24 | 1 164 | 1 734 | -0.95 |
Sample | t/Ma | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | εHf(0) | εHf(t) | TDM1/Ma | TDM2/Ma | fLu/Hf |
SKC-4-1 | 158.5 | 0.048 149 | 0.000 824 | 0.001 222 | 0.000 022 | 0.282 425 | 0.000 017 | -12.28 | -8.94 | 1 175 | 1 774 | -0.96 |
SKC-4-2 | 154.4 | 0.043 035 | 0.000 219 | 0.001 082 | 0.000 004 | 0.282 431 | 0.000 016 | -12.06 | -8.79 | 1 162 | 1 761 | -0.97 |
SKC-4-3 | 158.0 | 0.054 419 | 0.000 975 | 0.001 437 | 0.000 011 | 0.282 397 | 0.000 015 | -13.26 | -9.95 | 1 221 | 1 837 | -0.96 |
SKC-4-4 | 158.0 | 0.052 119 | 0.000 697 | 0.001 336 | 0.000 013 | 0.282 398 | 0.000 015 | -13.22 | -9.89 | 1 216 | 1 834 | -0.96 |
SKC-4-5 | 158.0 | 0.068 126 | 0.000 879 | 0.001 627 | 0.000 018 | 0.282 408 | 0.000 015 | -12.89 | -9.59 | 1 213 | 1 815 | -0.95 |
SKC-4-6 | 156.0 | 0.056 267 | 0.000 225 | 0.001 406 | 0.000 007 | 0.282 417 | 0.000 016 | -12.56 | -9.29 | 1 192 | 1 794 | -0.96 |
SKC-4-7 | 157.0 | 0.064 913 | 0.001 252 | 0.001 608 | 0.000 032 | 0.282 421 | 0.000 016 | -12.42 | -9.14 | 1 193 | 1 786 | -0.95 |
SKC-4-8 | 155.0 | 0.087 113 | 0.001 206 | 0.002 440 | 0.000 056 | 0.282 505 | 0.000 118 | -9.43 | -6.27 | 1 097 | 1 602 | -0.93 |
SKC-4-9 | 156.0 | 0.059 965 | 0.000 464 | 0.001 493 | 0.000 016 | 0.282 442 | 0.000 017 | -11.67 | -8.40 | 1 159 | 1 738 | -0.96 |
SKC-4-10 | 157.5 | 0.051 321 | 0.000 882 | 0.001 323 | 0.000 039 | 0.282 410 | 0.000 018 | -12.81 | -9.49 | 1 200 | 1 808 | -0.96 |
SKC-4-11 | 158.0 | 0.024 387 | 0.001 077 | 0.000 569 | 0.000 028 | 0.282 294 | 0.000 014 | -16.92 | -13.51 | 1 337 | 2 063 | -0.98 |
SKC-4-12 | 157.4 | 0.041 567 | 0.000 644 | 0.001 153 | 0.000 030 | 0.282 406 | 0.000 037 | -12.95 | -9.62 | 1 200 | 1 816 | -0.97 |
SKC-4-13 | 158.0 | 0.060 840 | 0.001 203 | 0.001 482 | 0.000 021 | 0.282 395 | 0.000 018 | -13.34 | -10.03 | 1 226 | 1 842 | -0.96 |
SKC-4-14 | 155.0 | 0.060 400 | 0.000 708 | 0.001 527 | 0.000 013 | 0.282 421 | 0.000 015 | -12.41 | -9.16 | 1 190 | 1 785 | -0.95 |
SKC-4-15 | 157.0 | 0.076 601 | 0.000 580 | 0.001 875 | 0.000 016 | 0.282 397 | 0.000 017 | -13.25 | -10.00 | 1 235 | 1 839 | -0.94 |
SKC-4-16 | 153.4 | 0.049 778 | 0.000 670 | 0.001 379 | 0.000 033 | 0.282 406 | 0.000 020 | -12.94 | -9.71 | 1 206 | 1 819 | -0.96 |
SKC-4-17 | 153.3 | 0.056 876 | 0.000 438 | 0.001 469 | 0.000 010 | 0.282 433 | 0.000 019 | -11.98 | -8.77 | 1 171 | 1 759 | -0.96 |
SKC-4-20 | 159.0 | 0.032 239 | 0.000 303 | 0.000 887 | 0.000 011 | 0.282 441 | 0.000 014 | -11.69 | -8.29 | 1 142 | 1 734 | -0.97 |
SKC-4-21 | 156.5 | 0.043 889 | 0.000 452 | 0.001 147 | 0.000 007 | 0.282 444 | 0.000 018 | -11.60 | -8.28 | 1 146 | 1 731 | -0.97 |
SKC-4-22 | 157.0 | 0.031 698 | 0.000 278 | 0.000 865 | 0.000 006 | 0.282 417 | 0.000 014 | -12.55 | -9.19 | 1 175 | 1 789 | -0.97 |
SKC-4-23 | 155.0 | 0.057 053 | 0.000 323 | 0.001 563 | 0.000 019 | 0.282 457 | 0.000 014 | -11.13 | -7.89 | 1 140 | 1 705 | -0.95 |
SKC-4-24 | 157.0 | 0.068 774 | 0.000 715 | 0.001 802 | 0.000 014 | 0.282 355 | 0.000 016 | -14.74 | -11.48 | 1 293 | 1 933 | -0.95 |
SKC-4-25 | 156.0 | 0.045 155 | 0.000 487 | 0.001 273 | 0.000 011 | 0.282 434 | 0.000 017 | -11.96 | -8.67 | 1 164 | 1 755 | -0.96 |
SKC-4-26 | 157.0 | 0.043 342 | 0.000 368 | 0.001 239 | 0.000 010 | 0.282 420 | 0.000 017 | -12.44 | -9.12 | 1 182 | 1 785 | -0.96 |
SKC-4-27 | 155.0 | 0.065 170 | 0.001 949 | 0.002 261 | 0.000 059 | 0.282 366 | 0.000 024 | -14.36 | -11.19 | 1 294 | 1 913 | -0.93 |
SKC-4-28 | 156.0 | 0.043 650 | 0.000 230 | 0.001 196 | 0.000 011 | 0.282 503 | 0.000 027 | -9.53 | -6.23 | 1 065 | 1 601 | -0.96 |
SKC-4-29 | 153.0 | 0.055 429 | 0.000 533 | 0.001 452 | 0.000 015 | 0.282 416 | 0.000 015 | -12.60 | -9.39 | 1 195 | 1 798 | -0.96 |
SKC-4-30 | 157.0 | 0.049 419 | 0.000 471 | 0.001 432 | 0.000 018 | 0.282 347 | 0.000 016 | -15.01 | -11.72 | 1 291 | 1 948 | -0.96 |
Table 3 Zircon Lu-Hf isotopic compositions for the Laoyachao and Yagongtang plutons
Sample | t/Ma | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | εHf(0) | εHf(t) | TDM1/Ma | TDM2/Ma | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|---|---|
SKC-5-1 | 162.0 | 0.060 150 | 0.000 308 | 0.001 486 | 0.000 010 | 0.282 433 | 0.000 014 | -12.00 | -8.61 | 1 173 | 1 756 | -0.96 |
SKC-5-2 | 164.2 | 0.076 536 | 0.002 270 | 0.001 707 | 0.000 044 | 0.282 388 | 0.000 014 | -13.57 | -10.15 | 1 243 | 1 855 | -0.95 |
SKC-5-3 | 161.2 | 0.068 491 | 0.000 573 | 0.001 696 | 0.000 013 | 0.282 429 | 0.000 016 | -12.12 | -8.77 | 1 184 | 1 765 | -0.95 |
SKC-5-4 | 162.0 | 0.070 266 | 0.000 567 | 0.001 754 | 0.000 013 | 0.282 415 | 0.000 016 | -12.61 | -9.25 | 1 206 | 1 796 | -0.95 |
SKC-5-6 | 160.5 | 0.073 243 | 0.000 156 | 0.001 864 | 0.000 009 | 0.282 430 | 0.000 015 | -12.10 | -8.78 | 1 189 | 1 765 | -0.94 |
SKC-5-7 | 162.0 | 0.056 802 | 0.000 432 | 0.001 510 | 0.000 010 | 0.282 400 | 0.000 016 | -13.16 | -9.77 | 1 220 | 1 829 | -0.95 |
SKC-5-8 | 162.0 | 0.041 586 | 0.000 271 | 0.001 088 | 0.000 003 | 0.282 409 | 0.000 014 | -12.85 | -9.41 | 1 194 | 1 807 | -0.97 |
SKC-5-9 | 162.0 | 0.057 031 | 0.001 164 | 0.001 608 | 0.000 029 | 0.282 395 | 0.000 015 | -13.33 | -9.95 | 1 230 | 1 840 | -0.95 |
SKC-5-10 | 162.0 | 0.060 815 | 0.001 016 | 0.001 638 | 0.000 026 | 0.282 396 | 0.000 016 | -13.29 | -9.91 | 1 229 | 1 838 | -0.95 |
SKC-5-11 | 164.0 | 0.046 765 | 0.001 636 | 0.001 438 | 0.000 071 | 0.282 397 | 0.000 022 | -13.26 | -9.82 | 1 222 | 1 834 | -0.96 |
SKC-5-12 | 163.0 | 0.044 994 | 0.000 482 | 0.001 224 | 0.000 019 | 0.282 426 | 0.000 015 | -12.22 | -8.78 | 1 173 | 1 767 | -0.96 |
SKC-5-13 | 165.0 | 0.042 951 | 0.000 596 | 0.001 176 | 0.000 024 | 0.282 433 | 0.000 019 | -11.99 | -8.50 | 1 162 | 1 751 | -0.96 |
SKC-5-14 | 163.0 | 0.058 611 | 0.000 706 | 0.001 594 | 0.000 018 | 0.282 407 | 0.000 017 | -12.91 | -9.51 | 1 212 | 1 813 | -0.95 |
SKC-5-15 | 165.0 | 0.054 375 | 0.000 489 | 0.001 462 | 0.000 007 | 0.282 391 | 0.000 014 | -13.47 | -10.01 | 1 230 | 1 846 | -0.96 |
SKC-5-16 | 165.0 | 0.060 732 | 0.000 571 | 0.001 651 | 0.000 013 | 0.282 410 | 0.000 015 | -12.79 | -9.35 | 1 209 | 1 804 | -0.95 |
SKC-5-17 | 163.0 | 0.056 307 | 0.001 360 | 0.001 516 | 0.000 029 | 0.282 359 | 0.000 017 | -14.61 | -11.20 | 1 278 | 1 920 | -0.95 |
SKC-5-18 | 163.0 | 0.060 284 | 0.000 698 | 0.001 682 | 0.000 028 | 0.282 425 | 0.000 021 | -12.26 | -8.87 | 1 189 | 1 773 | -0.95 |
SKC-5-19 | 165.0 | 0.057 023 | 0.001 358 | 0.001 623 | 0.000 061 | 0.282 442 | 0.000 017 | -11.68 | -8.24 | 1 164 | 1 734 | -0.95 |
Sample | t/Ma | 176Yb/177Hf | 2σ | 176Lu/177Hf | 2σ | 176Hf/177Hf | 2σ | εHf(0) | εHf(t) | TDM1/Ma | TDM2/Ma | fLu/Hf |
SKC-4-1 | 158.5 | 0.048 149 | 0.000 824 | 0.001 222 | 0.000 022 | 0.282 425 | 0.000 017 | -12.28 | -8.94 | 1 175 | 1 774 | -0.96 |
SKC-4-2 | 154.4 | 0.043 035 | 0.000 219 | 0.001 082 | 0.000 004 | 0.282 431 | 0.000 016 | -12.06 | -8.79 | 1 162 | 1 761 | -0.97 |
SKC-4-3 | 158.0 | 0.054 419 | 0.000 975 | 0.001 437 | 0.000 011 | 0.282 397 | 0.000 015 | -13.26 | -9.95 | 1 221 | 1 837 | -0.96 |
SKC-4-4 | 158.0 | 0.052 119 | 0.000 697 | 0.001 336 | 0.000 013 | 0.282 398 | 0.000 015 | -13.22 | -9.89 | 1 216 | 1 834 | -0.96 |
SKC-4-5 | 158.0 | 0.068 126 | 0.000 879 | 0.001 627 | 0.000 018 | 0.282 408 | 0.000 015 | -12.89 | -9.59 | 1 213 | 1 815 | -0.95 |
SKC-4-6 | 156.0 | 0.056 267 | 0.000 225 | 0.001 406 | 0.000 007 | 0.282 417 | 0.000 016 | -12.56 | -9.29 | 1 192 | 1 794 | -0.96 |
SKC-4-7 | 157.0 | 0.064 913 | 0.001 252 | 0.001 608 | 0.000 032 | 0.282 421 | 0.000 016 | -12.42 | -9.14 | 1 193 | 1 786 | -0.95 |
SKC-4-8 | 155.0 | 0.087 113 | 0.001 206 | 0.002 440 | 0.000 056 | 0.282 505 | 0.000 118 | -9.43 | -6.27 | 1 097 | 1 602 | -0.93 |
SKC-4-9 | 156.0 | 0.059 965 | 0.000 464 | 0.001 493 | 0.000 016 | 0.282 442 | 0.000 017 | -11.67 | -8.40 | 1 159 | 1 738 | -0.96 |
SKC-4-10 | 157.5 | 0.051 321 | 0.000 882 | 0.001 323 | 0.000 039 | 0.282 410 | 0.000 018 | -12.81 | -9.49 | 1 200 | 1 808 | -0.96 |
SKC-4-11 | 158.0 | 0.024 387 | 0.001 077 | 0.000 569 | 0.000 028 | 0.282 294 | 0.000 014 | -16.92 | -13.51 | 1 337 | 2 063 | -0.98 |
SKC-4-12 | 157.4 | 0.041 567 | 0.000 644 | 0.001 153 | 0.000 030 | 0.282 406 | 0.000 037 | -12.95 | -9.62 | 1 200 | 1 816 | -0.97 |
SKC-4-13 | 158.0 | 0.060 840 | 0.001 203 | 0.001 482 | 0.000 021 | 0.282 395 | 0.000 018 | -13.34 | -10.03 | 1 226 | 1 842 | -0.96 |
SKC-4-14 | 155.0 | 0.060 400 | 0.000 708 | 0.001 527 | 0.000 013 | 0.282 421 | 0.000 015 | -12.41 | -9.16 | 1 190 | 1 785 | -0.95 |
SKC-4-15 | 157.0 | 0.076 601 | 0.000 580 | 0.001 875 | 0.000 016 | 0.282 397 | 0.000 017 | -13.25 | -10.00 | 1 235 | 1 839 | -0.94 |
SKC-4-16 | 153.4 | 0.049 778 | 0.000 670 | 0.001 379 | 0.000 033 | 0.282 406 | 0.000 020 | -12.94 | -9.71 | 1 206 | 1 819 | -0.96 |
SKC-4-17 | 153.3 | 0.056 876 | 0.000 438 | 0.001 469 | 0.000 010 | 0.282 433 | 0.000 019 | -11.98 | -8.77 | 1 171 | 1 759 | -0.96 |
SKC-4-20 | 159.0 | 0.032 239 | 0.000 303 | 0.000 887 | 0.000 011 | 0.282 441 | 0.000 014 | -11.69 | -8.29 | 1 142 | 1 734 | -0.97 |
SKC-4-21 | 156.5 | 0.043 889 | 0.000 452 | 0.001 147 | 0.000 007 | 0.282 444 | 0.000 018 | -11.60 | -8.28 | 1 146 | 1 731 | -0.97 |
SKC-4-22 | 157.0 | 0.031 698 | 0.000 278 | 0.000 865 | 0.000 006 | 0.282 417 | 0.000 014 | -12.55 | -9.19 | 1 175 | 1 789 | -0.97 |
SKC-4-23 | 155.0 | 0.057 053 | 0.000 323 | 0.001 563 | 0.000 019 | 0.282 457 | 0.000 014 | -11.13 | -7.89 | 1 140 | 1 705 | -0.95 |
SKC-4-24 | 157.0 | 0.068 774 | 0.000 715 | 0.001 802 | 0.000 014 | 0.282 355 | 0.000 016 | -14.74 | -11.48 | 1 293 | 1 933 | -0.95 |
SKC-4-25 | 156.0 | 0.045 155 | 0.000 487 | 0.001 273 | 0.000 011 | 0.282 434 | 0.000 017 | -11.96 | -8.67 | 1 164 | 1 755 | -0.96 |
SKC-4-26 | 157.0 | 0.043 342 | 0.000 368 | 0.001 239 | 0.000 010 | 0.282 420 | 0.000 017 | -12.44 | -9.12 | 1 182 | 1 785 | -0.96 |
SKC-4-27 | 155.0 | 0.065 170 | 0.001 949 | 0.002 261 | 0.000 059 | 0.282 366 | 0.000 024 | -14.36 | -11.19 | 1 294 | 1 913 | -0.93 |
SKC-4-28 | 156.0 | 0.043 650 | 0.000 230 | 0.001 196 | 0.000 011 | 0.282 503 | 0.000 027 | -9.53 | -6.23 | 1 065 | 1 601 | -0.96 |
SKC-4-29 | 153.0 | 0.055 429 | 0.000 533 | 0.001 452 | 0.000 015 | 0.282 416 | 0.000 015 | -12.60 | -9.39 | 1 195 | 1 798 | -0.96 |
SKC-4-30 | 157.0 | 0.049 419 | 0.000 471 | 0.001 432 | 0.000 018 | 0.282 347 | 0.000 016 | -15.01 | -11.72 | 1 291 | 1 948 | -0.96 |
岩/矿区 | 岩性 | 测年方法 | t/Ma | 数据来源 | |
---|---|---|---|---|---|
岩体 | 老鸦巢 | 花岗闪长岩 | 锆石U-Pb测年 | 162.9±0.7 | 本文 |
鸭公塘 | 花岗闪长岩 | 锆石U-Pb测年 | 156.3±0.6 | 本文 | |
仙人岩 | 二长岩 | 锆石U-Pb测年 | 156.09±0.46 | 甄世民等[ | |
骑田岭 | 黑云母二长花岗岩 | 单颗粒锆石U-Pb测年 | 161±2 | 朱金初等[ | |
全岩Rb-Sr等时线测年 | 159±1.2 | ||||
锆石U-Pb测年 | 160±2 | 付建明等[ | |||
芙蓉超单元 | 黑云母二长花岗岩 | 锆石U-Pb测年 | 155±6 | 李华芹等[ | |
全岩Rb-Sr等时线测年 | 146±10 | ||||
锆石U-Pb测年 | 155.5±1.3 | 赵葵东等[ | |||
锆石U-Pb测年 | 157.1±1.2 | ||||
千里山 | 花岗岩 | 钾长石Ar-Ar | 162.55±3.25 | 刘义茂等[ | |
钾长石Ar-Ar | 151~153 | Li等[ | |||
西山 | 花岗岩 | 全岩Rb-Sr等时线测年 | 156±6 | 付建明等[ | |
碎斑熔岩 | 全岩Rb-Sr等时线测年 | 159±2 | |||
流纹岩 | 全岩Rb-Sr等时线测年 | 154±11 | |||
牛庙 | 闪长岩 | 锆石U-Pb测年 | 163±4 | 朱金初等[ | |
同安 | 石英二长岩 | 锆石U-Pb测年 | 160±4 | ||
姑婆山里松 | 花岗岩 | 锆石U-Pb测年 | 162±1 | ||
隘子 | 黑云母花岗岩 | 锆石U-Pb测年 | 160.1±6.1 | 徐夕生等[ | |
全南 | 正长岩 | 锆石U-Pb测年 | 161±4 | 陈志刚等[ | |
宝山 | 花岗斑岩 | 锆石U-Pb测年 | 161±1 | 路远发等[ | |
黄沙坪 | 花岗斑岩 | 锆石U-Pb测年 | 161.6±2 | 姚军明等[ | |
九疑山金鸡岭 | 二云母二长花岗岩 | 锆石U-Pb测年 | 156±2 | 付建明等[ | |
荷花坪 | 花岗斑岩 | 锆石U-Pb测年 | 154.7±0.5 | 章荣清等[ | |
矿床 | 黄沙坪 | 铅锌铜矿床 | 辉钼矿Re-Os | 154.8±1.9 | Yao等[ |
153.8±4.8 | 马丽艳等[ | ||||
159.4±3.3 | 雷泽恒等[ | ||||
157.5±2.4 | |||||
157.6±2.3 | |||||
水口山 | 铅锌金矿床 | 辉钼矿Re-Os | 157.8±1.4 | Yang等[ | |
宝山 | 铅锌铜矿床 | 辉钼矿Re-Os | 160±2 | 路远发等[ | |
铜山岭 | 铅锌铜矿床 | 辉钼矿Re-Os | 155±3 | 卢友月等[ | |
159.0±5.6 | Zhao等[ | ||||
162.2±1.6 |
Table 4 Statistical table of diagenetic and metallogenic ages of lead-zinc deposits in the Nanling area
岩/矿区 | 岩性 | 测年方法 | t/Ma | 数据来源 | |
---|---|---|---|---|---|
岩体 | 老鸦巢 | 花岗闪长岩 | 锆石U-Pb测年 | 162.9±0.7 | 本文 |
鸭公塘 | 花岗闪长岩 | 锆石U-Pb测年 | 156.3±0.6 | 本文 | |
仙人岩 | 二长岩 | 锆石U-Pb测年 | 156.09±0.46 | 甄世民等[ | |
骑田岭 | 黑云母二长花岗岩 | 单颗粒锆石U-Pb测年 | 161±2 | 朱金初等[ | |
全岩Rb-Sr等时线测年 | 159±1.2 | ||||
锆石U-Pb测年 | 160±2 | 付建明等[ | |||
芙蓉超单元 | 黑云母二长花岗岩 | 锆石U-Pb测年 | 155±6 | 李华芹等[ | |
全岩Rb-Sr等时线测年 | 146±10 | ||||
锆石U-Pb测年 | 155.5±1.3 | 赵葵东等[ | |||
锆石U-Pb测年 | 157.1±1.2 | ||||
千里山 | 花岗岩 | 钾长石Ar-Ar | 162.55±3.25 | 刘义茂等[ | |
钾长石Ar-Ar | 151~153 | Li等[ | |||
西山 | 花岗岩 | 全岩Rb-Sr等时线测年 | 156±6 | 付建明等[ | |
碎斑熔岩 | 全岩Rb-Sr等时线测年 | 159±2 | |||
流纹岩 | 全岩Rb-Sr等时线测年 | 154±11 | |||
牛庙 | 闪长岩 | 锆石U-Pb测年 | 163±4 | 朱金初等[ | |
同安 | 石英二长岩 | 锆石U-Pb测年 | 160±4 | ||
姑婆山里松 | 花岗岩 | 锆石U-Pb测年 | 162±1 | ||
隘子 | 黑云母花岗岩 | 锆石U-Pb测年 | 160.1±6.1 | 徐夕生等[ | |
全南 | 正长岩 | 锆石U-Pb测年 | 161±4 | 陈志刚等[ | |
宝山 | 花岗斑岩 | 锆石U-Pb测年 | 161±1 | 路远发等[ | |
黄沙坪 | 花岗斑岩 | 锆石U-Pb测年 | 161.6±2 | 姚军明等[ | |
九疑山金鸡岭 | 二云母二长花岗岩 | 锆石U-Pb测年 | 156±2 | 付建明等[ | |
荷花坪 | 花岗斑岩 | 锆石U-Pb测年 | 154.7±0.5 | 章荣清等[ | |
矿床 | 黄沙坪 | 铅锌铜矿床 | 辉钼矿Re-Os | 154.8±1.9 | Yao等[ |
153.8±4.8 | 马丽艳等[ | ||||
159.4±3.3 | 雷泽恒等[ | ||||
157.5±2.4 | |||||
157.6±2.3 | |||||
水口山 | 铅锌金矿床 | 辉钼矿Re-Os | 157.8±1.4 | Yang等[ | |
宝山 | 铅锌铜矿床 | 辉钼矿Re-Os | 160±2 | 路远发等[ | |
铜山岭 | 铅锌铜矿床 | 辉钼矿Re-Os | 155±3 | 卢友月等[ | |
159.0±5.6 | Zhao等[ | ||||
162.2±1.6 |
[1] | 李仕能. 水口山矿田成因机制新探: 介绍水口山浅成低温热液金矿成矿模式[J]. 矿产与地质, 1988, 2(2): 16-19. |
[2] | 刘伟. 水口山Pb-Zn-Au矿田含矿流体的性质、来源及其环流历程[J]. 大地构造与成矿学, 1994, 18(3): 209-218. |
[3] | 刘顺生, 谭凯旋. 湖南水口山矿田开放体系构造成矿动力学[J]. 大地构造与成矿学, 1996, 20(1): 1-9. |
[4] | 张庆华. 湖南水口山铅锌矿田地质特征及找矿思路[J]. 有色金属矿产与勘查, 1999, 8(3): 141-146. |
[5] | 李永胜, 巩小栋, 祝新友, 等. 湖南水口山铅锌金银矿田典型矿床成因分析[J]. 矿床地质, 2014, 33(增刊1): 219-220. |
[6] | 周新鹏, 李倩, 王登红, 等. 南岭东段典型矿区岩浆岩物性特征研究[J]. 地学前缘, 2017, 24(5): 131-137. |
[7] | 周永章, 郑义, 曾长育, 等. 关于钦-杭成矿带的若干认识[J]. 地学前缘, 2015, 22(2): 1-6. |
[8] | 喻亨祥, 刘家远. 水口山矿田花岗质潜火山杂岩的成因特征[J]. 大地构造与成矿学, 1997, 21(1): 32-40. |
[9] | 王岳军, 范蔚茗, 郭锋, 等. 湘东南中生代花岗闪长岩锆石U-Pb法定年及其成因指示[J]. 中国科学:D辑, 2001, 31(9): 745-751. |
[10] | 马丽艳, 路远发, 梅玉萍, 等. 湖南水口山矿区花岗闪长岩中的锆石SHRIMP U-Pb定年及其地质意义[J]. 岩石学报, 2006, 22(10): 2475-2482. |
[11] | 左昌虎, 路睿, 赵增霞, 等. 湖南常宁水口山Pb-Zn矿区花岗闪长岩元素地球化学, LA-ICP-MS锆石U-Pb年龄和Hf同位素特征[J]. 地质论评, 2014, 60(4): 811-823. |
[12] | 甄世民, 祝新友, 李永胜, 等. 湖南仙人岩与金矿床有关的二长岩锆石U-Pb年龄、Hf同位素及地质意义[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1740-1756. |
[13] | 毛景文, 陈懋弘, 袁顺达, 等. 华南地区钦杭成矿带地质特征和矿床时空分布规律[J]. 地质学报, 2011, 85(5): 636-658. |
[14] | 杨传益. 康家湾铅锌矿床的发现及成因[J]. 地质与勘探, 1985, 21(5): 1-7. |
[15] | 郑伟, 毛景文, 欧阳志侠, 等. 阳春盆地陂头面铜多金属矿床成岩成矿年代学、锆石微量元素及地质意义[J]. 岩石学报, 2018, 34(9): 2671-2686. |
[16] | 薛建玲, 宛克勇. 湖南水口山铅锌矿发现厚层铜硫矿体和铁铜矿体[J]. 中国地质调查成果快讯, 2015(7): 11-12. |
[17] |
LIU Y S, GAO S, KELEMEN P B, et al. Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton[J]. Geochimica et Cosmochimica Acta, 2008, 72(9): 2349-2376.
DOI URL |
[18] | 侯可军, 李延河, 田有荣. LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J]. 矿床地质, 2009, 28(4): 481-492. |
[19] | 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. |
[20] |
CHU N C, TAYLOR R N, CHAVAGNAC V R, 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.
DOI URL |
[21] | 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(18): A158. |
[22] |
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 |
[23] |
WU Y B, ZHENG Y F. Genesis of zircon and its constraints on interpretation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49(15): 1554-1569.
DOI URL |
[24] |
MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4): 215-224.
DOI URL |
[25] |
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 |
[26] |
MANIAR P D, PICCOLI P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989, 101(5): 635-643.
DOI URL |
[27] |
SUN S 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 |
[28] |
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(1/2): 243-258.
DOI URL |
[29] |
GRIFFIN W L, PEARSON N J, BELOUSOVA E, et al. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1): 133-147.
DOI URL |
[30] |
SÖDERLUND U, PATCHETT P J, VERVOORT J D, et al. The 176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions[J]. Earth and Planetary Science Letters, 2004, 219(3/4): 311-324.
DOI URL |
[31] |
VERVOORT J D, JONATHAN PATCHETT P. Behavior of hafnium and neodymium isotopes in the crust: constraints from Precambrian crustally derived granites[J]. Geochimica et Cosmochimica Acta, 1996, 60(19): 3717-3733.
DOI URL |
[32] |
HUANG J C, PENG J T, YANG J H, et al. Precise zircon U-Pb and molybdenite Re-Os dating of the Shuikoushan granodiorite-related Pb-Zn mineralization, southern Hunan, South China[J]. Ore Geology Reviews, 2015, 71: 305-317.
DOI URL |
[33] |
YANG J H, PENG J T, ZHENG Y F, et al. Petrogenesis of the Mesozoic Shuikoushan peraluminous I-type granodioritic intrusion in Hunan Province, South China: middle-lower crustal reworking in an extensional tectonic setting[J]. Journal of Asian Earth Sciences, 2016, 123: 224-242.
DOI URL |
[34] | 郭剑豪, 邹海洋. 鸭公塘铁铜矿床相关花岗闪长岩锆石U-Pb年龄、地球化学特征及地质意义[J]. 南方金属, 2019(4): 20-25. |
[35] | 陈志刚, 李献华, 李武显, 等. 赣南全南正长岩的SHRIMP锆石U-Pb年龄及其对华南燕山早期构造背景的制约[J]. 地球化学, 2003, 32(3): 223-229. |
[36] | 付建明, 马昌前, 谢才富, 等. 湖南骑田岭岩体东缘菜岭岩体的锆石SHRIMP定年及其意义[J]. 中国地质, 2004, 31(1): 96-100. |
[37] | 付建明, 马昌前, 谢才富, 等. 湘南西山铝质A型花岗质火山-侵入杂岩的地球化学及其形成环境[J]. 地球科学与环境学报, 2004, 26(4): 15-23. |
[38] | 朱金初, 黄革非, 张佩华, 等. 湘南骑田岭岩体菜岭超单元花岗岩侵位年龄和物质来源研究[J]. 地质论评, 2003, 49(3): 245-252. |
[39] | 李华芹, 路远发, 王登红, 等. 湖南骑田岭芙蓉矿田成岩成矿时代的厘定及其地质意义[J]. 地质论评, 2006, 52(1): 113-121. |
[40] | 赵葵东, 蒋少涌, 姜耀辉, 等. 湘南骑田岭岩体芙蓉超单元的锆石SHRIMP U-Pb年龄及其地质意义[J]. 岩石学报, 2006, 22(10): 2611-2616. |
[41] | 刘义茂, 戴橦谟, 卢焕章, 等. 千里山花岗岩成岩成矿的40Ar-39Ar和Sm-Nd同位素年龄[J]. 中国科学: D辑, 1997, 27(5): 425-430. |
[42] |
LI X H, CHUNG S L, ZHOU H W, et al. Jurassic intraplate magmatism in southern Hunan-eastern Guangxi: 40Ar/39Ar dating, geochemistry, Sr-Nd isotopes and implications for the tectonic evolution of SE China[J]. Geological Society of London, Special Publications, 2004, 226(1): 193-215.
DOI URL |
[43] | 朱金初, 谢才富, 张佩华, 等. 桂东北牛庙闪长岩和同安石英二长岩:岩石学、锆石SHRIMP U-Pb年代学和地球化学[J]. 岩石学报, 2005, 21(3): 665-676. |
[44] | 徐夕生, 邓平, O’REILLY S Y, 等. 华南贵东杂岩体单颗粒锆石激光探针ICPMS U-Pb定年及其成岩意义[J]. 科学通报, 2003, 48(12): 1328-1334. |
[45] | 路远发, 马丽艳, 屈文俊, 等. 湖南宝山铜-钼多金属矿床成岩成矿的U-Pb和Re-Os同位素定年研究[J]. 岩石学报, 2006, 22(10): 2483-2492. |
[46] | 姚军明, 华仁民, 林锦富. 湘东南黄沙坪花岗岩LA-ICPMS锆石U-Pb定年及岩石地球化学特征[J]. 岩石学报, 2005, 21(3): 688-696. |
[47] | 付建明, 马昌前, 谢才富, 等. 湖南九嶷山复式花岗岩体SHRIMP锆石定年及其地质意义[J]. 大地构造与成矿学, 2004, 28(4): 370-378. |
[48] | 章荣清, 陆建军, 朱金初, 等. 湘南荷花坪花岗斑岩锆石LA-MC-ICP-MS U-Pb年龄、Hf同位素制约及地质意义[J]. 高校地质学报, 2010, 16(4): 436-447. |
[49] |
KEMP A I S, HAWKESWORTH C J, FOSTER G L, et al. Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon[J]. Science, 2007, 315: 980-983.
DOI URL |
[50] | XIA Y, XU X S, ZOU H B, et al. Early Paleozoic crust-mantle interaction and lithosphere delamination in South China Block: evidence from geochronology, geochemistry, and Sr-Nd-Hf isotopes of granites[J]. Lithos, 2014, 184/185/186/187: 416-435. |
[51] |
GRAY C M. An isotopic mixing model for the origin of granitic rocks in southeastern Australia[J]. Earth and Planetary Science Letters, 1984, 70(1): 47-60.
DOI URL |
[52] | COLLINS W J. S- and I-type granitoids of the eastern La-chlan fold belt: products of three-component mixing[J]. Transactions of the Royal Society of Edinburgh, Earth Sciences, 1996, 88: 171-179. |
[53] |
WEYER S, MÜNKER C, MEZGER K. Nb/Ta, Zr/Hf and REE in the depleted mantle: implications for the differentiation history of the crust-mantle system[J]. Earth and Planetary Science Letters, 2003, 205(3/4): 309-324.
DOI URL |
[54] | 赵振华, 熊小林, 王强, 等. 铌与钽的某些地球化学问题[J]. 地球化学, 2008, 37(4): 304-320. |
[55] |
BARTH M G, MCDONOUGH W F, RUDNICK R L. Tracking the budget of Nb and Ta in the continental crust[J]. Chemical Geology, 2000, 165(3/4): 197-213.
DOI URL |
[56] |
BEARD J S, LOFGREN G E. Dehydration melting and water-saturated melting of basaltic and andesitic greenstones and amphibolites at 1, 3, and 6.9 kbar[J]. Journal of Petrology, 1991, 32(2): 365-401.
DOI URL |
[57] | RAPP R P. Amphibole-out phase boundary in partially melted metabasalt, its control over liquid fraction and composition, and source permeability[J]. Journal of Geophysical Research: Solid Earth, 1995, 100(B8): 15601-15610. |
[58] | JOHANNES W, HOLTZ F. Petrogenesis and experimental petrology of granitic rocks[M]. Berlin, Heidelberg: Springer, 1996. |
[59] |
SISSON T W, RATAJESKI K, HANKINS W B, et al. Voluminous granitic magmas from common basaltic sources[J]. Contributions to Mineralogy and Petrology, 2005, 148(6): 635-661.
DOI URL |
[60] | DOUCE A E P, MCCARTHY T C. Melting of crustal rocks during continental collision and subduction[M]// HACKER B R, LIOU J G. When continents collide: geodynamics and geochemistry of ultrahigh-pressure rocks. Dordrecht: Springer Netherlands, 1998: 27-55. |
[61] |
PATIÑO DOUCE A E. What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas?[J]. Geological Society of London, Special Publications, 1999, 168(1): 55-75.
DOI URL |
[62] |
STERN C R, KILIAN R. Role of the subducted slab, mantle wedge and continental crust in the generation of Adakites from the Andean Austral volcanic zone[J]. Contributions to Mineralogy and Petrology, 1996, 123(3): 263-281.
DOI URL |
[63] |
ALTHERR R, SIEBEL W. I-type plutonism in a continental back-arc setting: Miocene granitoids and monzonites from the central Aegean Sea, Greece[J]. Contributions to Mineralogy and Petrology, 2002, 143(4): 397-415.
DOI URL |
[64] | 周新民. 对华南花岗岩研究的若干思考[J]. 高校地质学报, 2003, 9(4): 556-565. |
[65] | 李兴远, 周永章, 安燕飞, 等. 钦-杭成矿带南段丰村铅锌矿区下园垌矿段围岩微量元素的地球化学特征及其意义[J]. 地学前缘, 2015, 22(2): 131-143. |
[66] | 徐德明, 蔺志永, 骆学全, 等. 钦-杭成矿带主要金属矿床成矿系列[J]. 地学前缘, 2015, 22(2): 7-24. |
[67] | 王少轶, 赵正, 方贵聪, 等. 赣南樟(东坑)—九(龙脑)钨多金属矿床矿物学、年代学特征及其地质意义[J]. 地学前缘, 2017, 24(5): 120-130. |
[68] | 许德如, 邓腾, 董国军, 等. 湘东北连云山二云母二长花岗岩的年代学和地球化学特征:对岩浆成因和成矿地球动力学背景的启示[J]. 地学前缘, 2017, 24(2): 104-122. |
[69] | 余盼, 郑义, 王岳军, 等. 湖南新宁星子岩锑矿流体包裹体特征及矿床成因[J]. 地学前缘, 2018, 25(5): 266-276. |
[70] |
ZHOU X M, LI W X. Origin of Late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas[J]. Tectonophysics, 2000, 326(3/4): 269-287.
DOI URL |
[71] | LI Z X, LI X H, CHUNG S L, et al. Magmatic switch-on and switch-off along the South China continental margin since the Permian: transition from an Andean-type to a Western Pacific-type plate boundary[J]. Tectonophysics, 2012, 532/533/534/535: 271-290. |
[72] | 王强, 赵振华, 简平, 等. 德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学[J]. 岩石学报, 2004, 20(2): 315-324. |
[73] | 董树文, 吴锡浩, 吴珍汉, 等. 论东亚大陆的构造翘变: 燕山运动的全球意义[J]. 地质论评, 2000, 46(1): 8-13. |
[74] | 周新民. 南岭地区晚中生代花岗岩成因与岩石圈动力学演化[M]. 北京: 科学出版社, 2007. |
[75] | 李晓峰, WATANABE Y, 华仁民, 等. 华南地区中生代Cu-(Mo)-W-Sn矿床成矿作用与洋岭/转换断层俯冲[J]. 地质学报, 2008, 82(5): 625-640. |
[76] | 华仁民, 陈培荣, 张文兰, 等. 论华南地区中生代3次大规模成矿作用[J]. 矿床地质, 2005, 24(2): 99-107. |
[77] | 毛景文, 谢桂青, 郭春丽, 等. 华南地区中生代主要金属矿床时空分布规律和成矿环境[J]. 高校地质学报, 2008, 14(4): 510-526. |
[78] | YAO J M, HUA R M, QU W J, et al. Re-Os isotope dating of molybdenites in the Huangshaping Pb-Zn-W-Mo polymetallic deposit, Hunan Province, South China and its geological significance[J]. Science in China Series D: Earth Sciences, 2007, 50(4): 519-526. |
[79] | 马丽艳, 路远发, 屈文俊, 等. 湖南黄沙坪铅锌多金属矿床的Re-Os同位素等时线年龄及其地质意义[J]. 矿床地质, 2007, 26(4): 425-431. |
[80] | 雷泽恒, 陈富文, 陈郑辉, 等. 黄沙坪铅锌多金属矿成岩成矿年龄测定及地质意义[J]. 地球学报, 2010, 31(4): 532-540. |
[81] |
YANG J H, KANG L F, PENG J T, et al. In-situ elemental and isotopic compositions of apatite and zircon from the Shuikoushan and Xihuashan granitic plutons: implication for Jurassic granitoid-related Cu-Pb-Zn and W mineralization in the Nanling Range, South China[J]. Ore Geology Reviews, 2018, 93: 382-403.
DOI URL |
[82] | 卢友月, 付建明, 程顺波, 等. 湘南铜山岭铜多金属矿田成岩成矿作用年代学研究[J]. 大地构造与成矿学, 2015, 39(6): 1061-1071. |
[83] |
ZHAO P L, YUAN S D, MAO J W, et al. Geochronological and petrogeochemical constraints on the skarn deposits in Tongshanling ore district, southern Hunan Province: implications for Jurassic Cu and W metallogenic events in South China[J]. Ore Geology Reviews, 2016, 78: 120-137.
DOI URL |
[84] | 叶天竺, 吕志成, 庞振山, 等. 勘查区找矿预测理论与方法(总论)[M]. 北京: 地质出版社, 2014. |
[85] |
CATHLES L M, ERENDI A H J, BARRIE T. How long can a hydrothermal system be sustained by a single intrusive event?[J]. Economic Geology, 1997, 92(7/8): 766-771.
DOI URL |
[86] | 杜保峰, 魏俊浩, 王启, 等. 中国东部钼矿成矿背景与成岩-成矿时差讨论[J]. 矿床地质, 2010, 29(6): 935-955. |
[87] |
MAO J W, ZHANG Z C, ZHANG Z H, et al. Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo)deposit in the northern Qilian Mountains and its geological significance[J]. Geochimica et Cosmochimica Acta, 1999, 63(11/12): 1815-1818.
DOI URL |
[88] |
STEIN H J, MARKEY R J, MORGAN J W, et al. The remarkable Re-Os chronometer in molybdenite: how and why it works[J]. Terra Nova, 2001, 13(6): 479-486.
DOI URL |
[89] |
JENNER F E. Cumulate causes for the low contents of sulfide-loving elements in the continental crust[J]. Nature Geoscience, 2017, 10(7): 524-529.
DOI URL |
[90] |
CHERNIAK D J. Diffusion in carbonates, fluorite, sulfide minerals, and diamond[J]. Reviews in Mineralogy and Geochemistry, 2010, 72(1): 871-897.
DOI URL |
[91] |
HOU Z Q, ZHOU Y, WANG R, et al. Recycling of metal-fertilized lower continental crust: origin of non-arc Au-rich porphyry deposits at cratonic edges[J]. Geology, 2017, 45(6): 563-566.
DOI URL |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||