Geoscience ›› 2018, Vol. 32 ›› Issue (02): 305-315.DOI: 10.19657/j.geoscience.1000-8527.2018.02.09
• Petrology • Previous Articles Next Articles
DONG Pengsheng(), DONG Guochen(
), SUN Zhuanrong, LI Huawei, WANG Shushu, ZHAI Tianlei, WANG Weiqing, GENG Jianzhen
Received:
2017-05-16
Revised:
2017-12-20
Online:
2018-04-10
Published:
2018-05-07
CLC Number:
DONG Pengsheng, DONG Guochen, SUN Zhuanrong, LI Huawei, WANG Shushu, ZHAI Tianlei, WANG Weiqing, GENG Jianzhen. Chronology,Geochemistry Characteristics and Petrogenesis of Wufenglou Lamprophyres in Northern Hebei, China[J]. Geoscience, 2018, 32(02): 305-315.
样品号 | SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | Na2O+ K2O | Na2O/ K2O | Mg# |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
16WF88 | 51.47 | 1.34 | 13.75 | 8.87 | 5.64 | 0.14 | 7.81 | 8.24 | 3.71 | 2.90 | 0.62 | 1.25 | 100.10 | 6.61 | 1.28 | 71.17 |
16WF93 | 48.25 | 1.65 | 14.12 | 11.12 | 6.21 | 0.16 | 8.00 | 7.11 | 4.83 | 2.09 | 1.10 | 1.68 | 100.11 | 6.92 | 2.31 | 69.66 |
16CL94 | 49.35 | 1.62 | 14.00 | 10.88 | 5.89 | 0.14 | 6.97 | 6.32 | 3.93 | 3.47 | 1.16 | 2.26 | 100.10 | 7.40 | 1.13 | 67.84 |
16WF301 | 50.43 | 1.38 | 13.76 | 9.28 | 5.64 | 0.14 | 7.27 | 7.85 | 3.78 | 2.71 | 0.73 | 2.51 | 99.84 | 6.49 | 1.39 | 69.68 |
16WF303 | 51.03 | 1.31 | 14.00 | 8.98 | 4.97 | 0.13 | 6.94 | 7.35 | 3.92 | 2.70 | 0.67 | 2.86 | 99.89 | 6.62 | 1.45 | 71.34 |
样品号 | K/Al | K/(K +Na) | Rb | Sr | Nb | Ba | Ta | Pb | Th | U | V | Zr | Hf | Y | La | Ce |
16WF88 | 0.23 | 0.34 | 105.7 | 969 | 51.6 | 1 141 | 2.45 | 15.10 | 9.27 | 2.42 | 170 | 235 | 8.84 | 17.34 | 48.8 | 114 |
16WF93 | 0.16 | 0.22 | 49.07 | 915 | 64.8 | 1 558 | 3.65 | 8.49 | 5.52 | 1.35 | 170 | 256 | 8.24 | 19.06 | 79.3 | 163 |
16CL94 | 0.27 | 0.37 | 25.08 | 1 167 | 59.1 | 2 029 | 3.31 | 13.70 | 4.65 | 1.46 | 164 | 279 | 9.59 | 17.39 | 53.0 | 133 |
16WF301 | 0.21 | 0.32 | 84.78 | 1 230 | 38.2 | 1 400 | 1.04 | 9.64 | 4.82 | 2.55 | 205 | 224 | 9.13 | 15.34 | 75.6 | 158 |
16WF303 | 0.21 | 0.31 | 78.29 | 1 257 | 39.8 | 1 290 | 1.30 | 9.40 | 6.14 | 2.44 | 181 | 231 | 8.9 | 14.19 | 67.7 | 142 |
样品号 | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | ΣREE | LREE/ HREE | (La/ Yb)N | δEu |
16WF88 | 12.5 | 46.6 | 8.15 | 2.56 | 6.82 | 0.82 | 3.98 | 0.71 | 1.78 | 0.23 | 1.27 | 0.20 | 248.26 | 14.70 | 27.57 | 1.02 |
16WF93 | 19.0 | 68.5 | 10.90 | 3.28 | 8.84 | 0.98 | 4.52 | 0.78 | 1.98 | 0.25 | 1.32 | 0.20 | 362.76 | 18.22 | 43.07 | 0.99 |
16CL94 | 17.1 | 64.6 | 10.10 | 3.08 | 8.02 | 0.89 | 4.10 | 0.70 | 1.86 | 0.22 | 1.21 | 0.19 | 297.86 | 16.33 | 31.41 | 1.01 |
16WF301 | 17.4 | 63.3 | 9.55 | 3.09 | 8.61 | 0.92 | 3.96 | 0.67 | 1.81 | 0.23 | 1.26 | 0.21 | 344.46 | 18.49 | 43.04 | 1.02 |
16WF303 | 16.2 | 58.8 | 8.89 | 2.88 | 7.94 | 0.85 | 3.71 | 0.62 | 1.70 | 0.21 | 1.15 | 0.19 | 312.99 | 18.12 | 42.24 | 1.03 |
Table 1 Composition of major elements (%) and trace elements (10-6) of Wufenglou lamprophyres
样品号 | SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | Na2O+ K2O | Na2O/ K2O | Mg# |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
16WF88 | 51.47 | 1.34 | 13.75 | 8.87 | 5.64 | 0.14 | 7.81 | 8.24 | 3.71 | 2.90 | 0.62 | 1.25 | 100.10 | 6.61 | 1.28 | 71.17 |
16WF93 | 48.25 | 1.65 | 14.12 | 11.12 | 6.21 | 0.16 | 8.00 | 7.11 | 4.83 | 2.09 | 1.10 | 1.68 | 100.11 | 6.92 | 2.31 | 69.66 |
16CL94 | 49.35 | 1.62 | 14.00 | 10.88 | 5.89 | 0.14 | 6.97 | 6.32 | 3.93 | 3.47 | 1.16 | 2.26 | 100.10 | 7.40 | 1.13 | 67.84 |
16WF301 | 50.43 | 1.38 | 13.76 | 9.28 | 5.64 | 0.14 | 7.27 | 7.85 | 3.78 | 2.71 | 0.73 | 2.51 | 99.84 | 6.49 | 1.39 | 69.68 |
16WF303 | 51.03 | 1.31 | 14.00 | 8.98 | 4.97 | 0.13 | 6.94 | 7.35 | 3.92 | 2.70 | 0.67 | 2.86 | 99.89 | 6.62 | 1.45 | 71.34 |
样品号 | K/Al | K/(K +Na) | Rb | Sr | Nb | Ba | Ta | Pb | Th | U | V | Zr | Hf | Y | La | Ce |
16WF88 | 0.23 | 0.34 | 105.7 | 969 | 51.6 | 1 141 | 2.45 | 15.10 | 9.27 | 2.42 | 170 | 235 | 8.84 | 17.34 | 48.8 | 114 |
16WF93 | 0.16 | 0.22 | 49.07 | 915 | 64.8 | 1 558 | 3.65 | 8.49 | 5.52 | 1.35 | 170 | 256 | 8.24 | 19.06 | 79.3 | 163 |
16CL94 | 0.27 | 0.37 | 25.08 | 1 167 | 59.1 | 2 029 | 3.31 | 13.70 | 4.65 | 1.46 | 164 | 279 | 9.59 | 17.39 | 53.0 | 133 |
16WF301 | 0.21 | 0.32 | 84.78 | 1 230 | 38.2 | 1 400 | 1.04 | 9.64 | 4.82 | 2.55 | 205 | 224 | 9.13 | 15.34 | 75.6 | 158 |
16WF303 | 0.21 | 0.31 | 78.29 | 1 257 | 39.8 | 1 290 | 1.30 | 9.40 | 6.14 | 2.44 | 181 | 231 | 8.9 | 14.19 | 67.7 | 142 |
样品号 | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | ΣREE | LREE/ HREE | (La/ Yb)N | δEu |
16WF88 | 12.5 | 46.6 | 8.15 | 2.56 | 6.82 | 0.82 | 3.98 | 0.71 | 1.78 | 0.23 | 1.27 | 0.20 | 248.26 | 14.70 | 27.57 | 1.02 |
16WF93 | 19.0 | 68.5 | 10.90 | 3.28 | 8.84 | 0.98 | 4.52 | 0.78 | 1.98 | 0.25 | 1.32 | 0.20 | 362.76 | 18.22 | 43.07 | 0.99 |
16CL94 | 17.1 | 64.6 | 10.10 | 3.08 | 8.02 | 0.89 | 4.10 | 0.70 | 1.86 | 0.22 | 1.21 | 0.19 | 297.86 | 16.33 | 31.41 | 1.01 |
16WF301 | 17.4 | 63.3 | 9.55 | 3.09 | 8.61 | 0.92 | 3.96 | 0.67 | 1.81 | 0.23 | 1.26 | 0.21 | 344.46 | 18.49 | 43.04 | 1.02 |
16WF303 | 16.2 | 58.8 | 8.89 | 2.88 | 7.94 | 0.85 | 3.71 | 0.62 | 1.70 | 0.21 | 1.15 | 0.19 | 312.99 | 18.12 | 42.24 | 1.03 |
测 点 | 含量/10-6 | Th/U | 206Pb/238U | 207Pb/235U | 207Pb/206Pb | 年龄/Ma | ||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb/238U | 207Pb/235U | 207Pb/206Pb | ||||||||||||||||||||
Pb | Th | U | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | ||||||||
1 | 4 | 150 | 170 | 0.88 | 0.021 6 | 0.000 3 | 0.155 4 | 0.013 9 | 0.052 1 | 0.004 5 | 138 | 2 | 147 | 13 | 289 | 199 | ||||||
2 | 8 | 306 | 387 | 0.79 | 0.020 6 | 0.000 3 | 0.144 2 | 0.004 7 | 0.050 9 | 0.001 6 | 131 | 2 | 137 | 4 | 234 | 73 | ||||||
3 | 6 | 160 | 281 | 0.57 | 0.020 6 | 0.000 4 | 0.154 7 | 0.005 8 | 0.054 6 | 0.002 3 | 131 | 2 | 146 | 6 | 394 | 93 | ||||||
4 | 7 | 220 | 305 | 0.72 | 0.021 8 | 0.000 5 | 0.156 2 | 0.005 4 | 0.051 9 | 0.002 0 | 139 | 3 | 147 | 5 | 279 | 88 | ||||||
5 | 6 | 167 | 260 | 0.64 | 0.021 2 | 0.000 4 | 0.155 1 | 0.006 0 | 0.053 0 | 0.002 3 | 135 | 3 | 146 | 6 | 330 | 97 | ||||||
6 | 5 | 126 | 227 | 0.56 | 0.020 5 | 0.000 5 | 0.158 6 | 0.004 8 | 0.056 2 | 0.002 0 | 131 | 3 | 149 | 5 | 460 | 80 | ||||||
7 | 5 | 138 | 207 | 0.67 | 0.021 7 | 0.000 4 | 0.157 1 | 0.005 6 | 0.052 5 | 0.002 1 | 138 | 2 | 148 | 5 | 309 | 90 | ||||||
8 | 4 | 163 | 188 | 0.87 | 0.020 8 | 0.000 3 | 0.154 8 | 0.005 7 | 0.053 9 | 0.001 9 | 133 | 2 | 146 | 5 | 366 | 77 | ||||||
9 | 5 | 172 | 246 | 0.70 | 0.021 1 | 0.000 4 | 0.164 3 | 0.006 9 | 0.056 5 | 0.002 4 | 135 | 3 | 155 | 6 | 471 | 92 | ||||||
10 | 5 | 147 | 237 | 0.62 | 0.021 0 | 0.000 4 | 0.152 4 | 0.005 4 | 0.052 7 | 0.002 3 | 134 | 3 | 144 | 5 | 317 | 101 | ||||||
11 | 4 | 188 | 195 | 0.96 | 0.020 7 | 0.000 3 | 0.148 9 | 0.005 4 | 0.052 1 | 0.001 9 | 132 | 2 | 141 | 5 | 289 | 83 | ||||||
12 | 7 | 328 | 301 | 1.09 | 0.021 7 | 0.000 3 | 0.158 5 | 0.005 3 | 0.052 9 | 0.001 8 | 139 | 2 | 149 | 5 | 325 | 78 | ||||||
13 | 7 | 338 | 315 | 1.07 | 0.021 3 | 0.000 3 | 0.147 8 | 0.004 6 | 0.050 2 | 0.001 6 | 136 | 2 | 140 | 4 | 206 | 75 | ||||||
14 | 4 | 171 | 201 | 0.85 | 0.021 5 | 0.000 3 | 0.158 6 | 0.008 8 | 0.053 6 | 0.003 8 | 137 | 2 | 149 | 8 | 353 | 160 | ||||||
15 | 5 | 164 | 212 | 0.77 | 0.021 3 | 0.000 3 | 0.147 6 | 0.005 8 | 0.050 1 | 0.001 9 | 136 | 2 | 140 | 6 | 201 | 89 | ||||||
16 | 21 | 106 | 847 | 1.25 | 0.021 4 | 0.000 3 | 0.153 8 | 0.012 2 | 0.052 2 | 0.004 1 | 136 | 2 | 145 | 12 | 296 | 178 | ||||||
17 | 7 | 297 | 295 | 1.01 | 0.021 5 | 0.000 6 | 0.155 7 | 0.013 3 | 0.052 6 | 0.003 4 | 137 | 4 | 147 | 13 | 312 | 147 | ||||||
18 | 6 | 288 | 289 | 1.00 | 0.021 1 | 0.000 3 | 0.161 5 | 0.005 0 | 0.055 6 | 0.001 9 | 134 | 2 | 152 | 5 | 437 | 75 |
Table 2 LA-ICP-MS zircon U-Pb isotopic data of Wufenglou lamprophyres
测 点 | 含量/10-6 | Th/U | 206Pb/238U | 207Pb/235U | 207Pb/206Pb | 年龄/Ma | ||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb/238U | 207Pb/235U | 207Pb/206Pb | ||||||||||||||||||||
Pb | Th | U | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | 比值 | 1σ | ||||||||
1 | 4 | 150 | 170 | 0.88 | 0.021 6 | 0.000 3 | 0.155 4 | 0.013 9 | 0.052 1 | 0.004 5 | 138 | 2 | 147 | 13 | 289 | 199 | ||||||
2 | 8 | 306 | 387 | 0.79 | 0.020 6 | 0.000 3 | 0.144 2 | 0.004 7 | 0.050 9 | 0.001 6 | 131 | 2 | 137 | 4 | 234 | 73 | ||||||
3 | 6 | 160 | 281 | 0.57 | 0.020 6 | 0.000 4 | 0.154 7 | 0.005 8 | 0.054 6 | 0.002 3 | 131 | 2 | 146 | 6 | 394 | 93 | ||||||
4 | 7 | 220 | 305 | 0.72 | 0.021 8 | 0.000 5 | 0.156 2 | 0.005 4 | 0.051 9 | 0.002 0 | 139 | 3 | 147 | 5 | 279 | 88 | ||||||
5 | 6 | 167 | 260 | 0.64 | 0.021 2 | 0.000 4 | 0.155 1 | 0.006 0 | 0.053 0 | 0.002 3 | 135 | 3 | 146 | 6 | 330 | 97 | ||||||
6 | 5 | 126 | 227 | 0.56 | 0.020 5 | 0.000 5 | 0.158 6 | 0.004 8 | 0.056 2 | 0.002 0 | 131 | 3 | 149 | 5 | 460 | 80 | ||||||
7 | 5 | 138 | 207 | 0.67 | 0.021 7 | 0.000 4 | 0.157 1 | 0.005 6 | 0.052 5 | 0.002 1 | 138 | 2 | 148 | 5 | 309 | 90 | ||||||
8 | 4 | 163 | 188 | 0.87 | 0.020 8 | 0.000 3 | 0.154 8 | 0.005 7 | 0.053 9 | 0.001 9 | 133 | 2 | 146 | 5 | 366 | 77 | ||||||
9 | 5 | 172 | 246 | 0.70 | 0.021 1 | 0.000 4 | 0.164 3 | 0.006 9 | 0.056 5 | 0.002 4 | 135 | 3 | 155 | 6 | 471 | 92 | ||||||
10 | 5 | 147 | 237 | 0.62 | 0.021 0 | 0.000 4 | 0.152 4 | 0.005 4 | 0.052 7 | 0.002 3 | 134 | 3 | 144 | 5 | 317 | 101 | ||||||
11 | 4 | 188 | 195 | 0.96 | 0.020 7 | 0.000 3 | 0.148 9 | 0.005 4 | 0.052 1 | 0.001 9 | 132 | 2 | 141 | 5 | 289 | 83 | ||||||
12 | 7 | 328 | 301 | 1.09 | 0.021 7 | 0.000 3 | 0.158 5 | 0.005 3 | 0.052 9 | 0.001 8 | 139 | 2 | 149 | 5 | 325 | 78 | ||||||
13 | 7 | 338 | 315 | 1.07 | 0.021 3 | 0.000 3 | 0.147 8 | 0.004 6 | 0.050 2 | 0.001 6 | 136 | 2 | 140 | 4 | 206 | 75 | ||||||
14 | 4 | 171 | 201 | 0.85 | 0.021 5 | 0.000 3 | 0.158 6 | 0.008 8 | 0.053 6 | 0.003 8 | 137 | 2 | 149 | 8 | 353 | 160 | ||||||
15 | 5 | 164 | 212 | 0.77 | 0.021 3 | 0.000 3 | 0.147 6 | 0.005 8 | 0.050 1 | 0.001 9 | 136 | 2 | 140 | 6 | 201 | 89 | ||||||
16 | 21 | 106 | 847 | 1.25 | 0.021 4 | 0.000 3 | 0.153 8 | 0.012 2 | 0.052 2 | 0.004 1 | 136 | 2 | 145 | 12 | 296 | 178 | ||||||
17 | 7 | 297 | 295 | 1.01 | 0.021 5 | 0.000 6 | 0.155 7 | 0.013 3 | 0.052 6 | 0.003 4 | 137 | 4 | 147 | 13 | 312 | 147 | ||||||
18 | 6 | 288 | 289 | 1.00 | 0.021 1 | 0.000 3 | 0.161 5 | 0.005 0 | 0.055 6 | 0.001 9 | 134 | 2 | 152 | 5 | 437 | 75 |
测点 | 年龄/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | σ | εHf(t) | tDM1 | tDM2 | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|
1 | 138.0 | 0.020 241 | 0.000 787 | 0.282 286 | 0.000 027 | -14.2 | 1 356 | 2 096 | -0.98 |
2 | 131.3 | 0.015 294 | 0.000 643 | 0.282 218 | 0.000 027 | -16.8 | 1 445 | 2 251 | -0.98 |
3 | 131.3 | 0.013 540 | 0.000 532 | 0.282 260 | 0.000 029 | -15.3 | 1 383 | 2 156 | -0.98 |
4 | 139.3 | 0.020 063 | 0.000 781 | 0.282 189 | 0.000 029 | -17.6 | 1 490 | 2 311 | -0.98 |
5 | 135.3 | 0.017 704 | 0.000 712 | 0.282 234 | 0.000 030 | -16.1 | 1 425 | 2 213 | -0.98 |
6 | 130.6 | 0.029 956 | 0.001 163 | 0.282 162 | 0.000 033 | -18.8 | 1 542 | 2 377 | -0.96 |
7 | 138.3 | 0.013 245 | 0.000 537 | 0.282 186 | 0.000 029 | -17.7 | 1 484 | 2 316 | -0.98 |
8 | 132.9 | 0.012 139 | 0.000 500 | 0.282 232 | 0.000 028 | -16.2 | 1 419 | 2 216 | -0.98 |
9 | 134.6 | 0.011 332 | 0.000 452 | 0.282 229 | 0.000 027 | -16.3 | 1 422 | 2 223 | -0.99 |
10 | 133.8 | 0.013 045 | 0.000 525 | 0.282 279 | 0.000 030 | -14.5 | 1 356 | 2 112 | -0.98 |
11 | 132.3 | 0.017 427 | 0.000 693 | 0.282 252 | 0.000 028 | -15.5 | 1399 | 2173 | -0.98 |
12 | 138.6 | 0.021 485 | 0.000 856 | 0.282 201 | 0.000 028 | -17.2 | 1 476 | 2 285 | -0.97 |
13 | 136.1 | 0.014 080 | 0.000 586 | 0.282 206 | 0.000 032 | -17.1 | 1 459 | 2 274 | -0.98 |
14 | 137.0 | 0.020 528 | 0.000 830 | 0.282 207 | 0.000 032 | -17.0 | 1 466 | 2 271 | -0.97 |
15 | 136.2 | 0.016 448 | 0.000 694 | 0.282 164 | 0.000 028 | -18.6 | 1 521 | 2 368 | -0.98 |
16 | 136.2 | 0.015 820 | 0.000 665 | 0.282 313 | 0.000 026 | -13.3 | 1 314 | 2 035 | -0.98 |
17 | 136.9 | 0.015 545 | 0.000 636 | 0.282 142 | 0.000 027 | -19.3 | 1 549 | 2 416 | -0.98 |
18 | 134.3 | 0.020 981 | 0.000 851 | 0.282 285 | 0.000 035 | -14.4 | 1 360 | 2 100 | -0.97 |
Table 3 Zircon Hf isotopic compositions of Wufenglou lamprophyres
测点 | 年龄/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf | σ | εHf(t) | tDM1 | tDM2 | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|
1 | 138.0 | 0.020 241 | 0.000 787 | 0.282 286 | 0.000 027 | -14.2 | 1 356 | 2 096 | -0.98 |
2 | 131.3 | 0.015 294 | 0.000 643 | 0.282 218 | 0.000 027 | -16.8 | 1 445 | 2 251 | -0.98 |
3 | 131.3 | 0.013 540 | 0.000 532 | 0.282 260 | 0.000 029 | -15.3 | 1 383 | 2 156 | -0.98 |
4 | 139.3 | 0.020 063 | 0.000 781 | 0.282 189 | 0.000 029 | -17.6 | 1 490 | 2 311 | -0.98 |
5 | 135.3 | 0.017 704 | 0.000 712 | 0.282 234 | 0.000 030 | -16.1 | 1 425 | 2 213 | -0.98 |
6 | 130.6 | 0.029 956 | 0.001 163 | 0.282 162 | 0.000 033 | -18.8 | 1 542 | 2 377 | -0.96 |
7 | 138.3 | 0.013 245 | 0.000 537 | 0.282 186 | 0.000 029 | -17.7 | 1 484 | 2 316 | -0.98 |
8 | 132.9 | 0.012 139 | 0.000 500 | 0.282 232 | 0.000 028 | -16.2 | 1 419 | 2 216 | -0.98 |
9 | 134.6 | 0.011 332 | 0.000 452 | 0.282 229 | 0.000 027 | -16.3 | 1 422 | 2 223 | -0.99 |
10 | 133.8 | 0.013 045 | 0.000 525 | 0.282 279 | 0.000 030 | -14.5 | 1 356 | 2 112 | -0.98 |
11 | 132.3 | 0.017 427 | 0.000 693 | 0.282 252 | 0.000 028 | -15.5 | 1399 | 2173 | -0.98 |
12 | 138.6 | 0.021 485 | 0.000 856 | 0.282 201 | 0.000 028 | -17.2 | 1 476 | 2 285 | -0.97 |
13 | 136.1 | 0.014 080 | 0.000 586 | 0.282 206 | 0.000 032 | -17.1 | 1 459 | 2 274 | -0.98 |
14 | 137.0 | 0.020 528 | 0.000 830 | 0.282 207 | 0.000 032 | -17.0 | 1 466 | 2 271 | -0.97 |
15 | 136.2 | 0.016 448 | 0.000 694 | 0.282 164 | 0.000 028 | -18.6 | 1 521 | 2 368 | -0.98 |
16 | 136.2 | 0.015 820 | 0.000 665 | 0.282 313 | 0.000 026 | -13.3 | 1 314 | 2 035 | -0.98 |
17 | 136.9 | 0.015 545 | 0.000 636 | 0.282 142 | 0.000 027 | -19.3 | 1 549 | 2 416 | -0.98 |
18 | 134.3 | 0.020 981 | 0.000 851 | 0.282 285 | 0.000 035 | -14.4 | 1 360 | 2 100 | -0.97 |
[1] | ROCK N M S, BOWES D R, WRIGHT A E. Lamprophyres[M]. Glasgow: Blackie, 1991:1-285. |
[2] | 路凤香, 舒小辛, 赵崇贺. 有关煌斑岩分类的建议[J]. 地质科技情报, 1991, 10(S1):55-62. |
[3] |
ROCK N M S, GROVES, D I. Do lamprophyres carry gold as well as diamonds?[J]. Nature, 1988, 332:253-255.
DOI |
[4] |
HUANG Z L, LI C Q, YANG H L, et al. The geochemistry of lamprophyres in the Laowangzhai gold deposits, Yunnan Pro-vince, China: implications for its characteristics of source region[J]. Geochemical Journal, 2002, 36(2):91-112.
DOI URL |
[5] |
BERNARD G J, FOURCADE S, DUPUY C. Isotopic study (Sr, Nd, O and C) of lamprophyres and associated dykes from Tamazert (Morroco): Crustal contamination processes and source characteristics[J]. Earth and Planetary Science Letters, 1991, 103(1/4):190-199.
DOI URL |
[6] |
PRELEVIC D, FOLEY S F, CVETKOVIC V, et al. Origin of minette by mixing of lamproite and dacite magmas in Veliki Majdan, Serbia[J]. Journal of Petrology, 2004, 45(4):759-792.
DOI URL |
[7] | 贾丽琼, 莫宣学, 董国臣, 等. 滇西马厂箐煌斑岩成因: 地球化学、年代学及Sr-Nd-Pb-Hf同位素约束[J]. 岩石学报, 2013, 29(4):1247-1260. |
[8] | 贾大成, 胡瑞忠, 卢焱, 等. 湘东北钠质煌斑岩地幔源区特征及成岩构造环境[J]. 中国科学:D辑, 2003, 33(4):344-352. |
[9] | 张海东, 刘建朝, 王金雅, 等. 太行山北段王安镇杂岩体岩石学、年代学、地球化学特征及地质意义[J]. 岩石学报, 2016, 32(3):727-745. |
[10] | 徐义刚, 李洪颜, 庞崇进, 等. 论华北克拉通破坏的时限[J]. 科学通报, 2009, 54(14):1974-1989. |
[11] | 张运强, 陈海燕, 刘应龙, 等. 冀北寿王坟铜矿石英二长岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J]. 黄金科学技术, 2014, 22(3):23-29. |
[12] | 董朋生. 燕山地区寿王坟杂岩体年代学、地球化学及其成矿意义[D]. 北京: 中国地质大学(北京), 2017:1-30. |
[13] | 耿建珍, 李怀坤, 张健, 等. 锆石Hf同位素组成的LA-MC-ICP-MS测定[J]. 地质通报, 2011, 30(10):1508-1513. |
[14] |
ROCK N M S. The nature and origin of lamprophyres: An overview[J]. Geological Society of London Special Publications, 1987, 30(1):191-226.
DOI URL |
[15] |
SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society of London Special Publications, 1989, 42(1):313-345.
DOI URL |
[16] | 姜耀辉, 蒋少涌, 赵葵东, 等. 辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约[J]. 科学通报, 2005, 50(19):2161-2168. |
[17] | 程彦博, 毛景文, 陈懋弘, 等. 云南个旧锡矿田碱性岩和煌斑岩LA-lCP-MS锆石U-Pb测年及其地质意义[J]. 中国地质, 2008, 35(6):1138-1149. |
[18] | HOSKIN P O W. The composition of zircon and igneous and meta-morphic petrogenesis[J]. Reviews in Mineralogy and Geochemi-stry, 2003, 53(1):27-62. |
[19] | 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. |
[20] | 邵济安, 张履桥. 华北北部中生代岩墙群[J]. 岩石学报, 2002, 18(3):312-318. |
[21] | 邵济安, 李献华, 张履桥, 等. 南口—古崖居中生代双峰式岩墙群形成机制的地球化学制约[J]. 地球化学, 2001, 30(6):517-524. |
[22] | 张勇, 陈斌, 邵济安, 等. 华北太行晚中生代煌斑岩地球化学特征及成因探讨[J]. 岩石矿物学杂志, 2003, 22(1):29-33. |
[23] | 刘国平, 艾永富, 冼伟胜. 辽宁桃源—小佟家堡子金矿带煌斑岩的地球化学特征及地质意义[J]. 岩石矿物学杂志, 1997, 16(4):324-330. |
[24] | 张德全, 孙桂英. 中国东部花岗岩[M]. 武汉: 中国地质大学出版社, 1988:1-298. |
[25] |
PEI F P, XU W L, YANG D B, et al. Petrogenesis of late Mesozoic granitoids in southern Jilin province, northeastern China: Geochronological, geochemical, and Sr-Nd-Pb isotopic evidence[J]. Lithos, 2011, 125(1/2):27-39.
DOI URL |
[26] | 唐亮, 刘燊, 冯彩霞, 等. 河北省北部杨树沟基性岩墙年代学和地球化学研究[J]. 矿物岩石地球化学通报, 2014, 33(1):82-90. |
[27] | YANG C, XU W, YANG D, et al. Petrogenesis of Mesozoic High-Mg diorites in Western Shandong: Evidence from chronology and petro-geochemistry[J]. Journal of China University of Geosciences, 2005, 16(4):81-92. |
[28] | 文霞. 燕山造山带后石湖山碱性环状杂岩体的成因及其构造意义[D]. 武汉: 中国地质大学(武汉), 2013:1-134. |
[29] |
HOFMANN A W. Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust[J]. Earth and Planetary Science Letters, 1988, 90(3):297-314.
DOI URL |
[30] |
MA L, JIANG S Y, HOFMANN A W et al. Lithospheric and asthenospheric sources of lamprophyres in the Jiaodong Peninsula: A consequence of rapid lithospheric thinning beneath the North China Craton?[J]. Geochimica et Cosmochimica Acta, 2014, 124(1):250-271.
DOI URL |
[31] | RUDNICK R L, GAO S. Composition of the continental crust[J]. Treatise on Geochemistry, 2014, 4:1-51. |
[32] |
MUNKER C. Nb/Ta fractionation in a Cambrian arc/back arc system, New Zealand: Source constraints and application of refined ICP-MS techniques[J]. Chemical Geology, 1998, 144(1/2):23-45.
DOI URL |
[33] | 邵济安, 李献华, 张履桥, 等. 南口—古崖居中生代双峰式岩墙群形成机制的地球化学制约[J]. 地球化学, 2001, 30(6):517-524. |
[34] |
DEVINE J D. Petrogenesis of the basalt-andesite-dacite association of Grenada, Lesser Antilles island arc, revisited[J]. Journal of Volcanology and Geothermal Research, 1995, 69(1):1-33.
DOI URL |
[35] |
ZHU Y F, ZHANG L F, GU L B, et al. The zircon SHRIMP chronology and trace element geochemistry of the Carboniferous volcanic rocks in western Tianshan Mountains[J]. Chinese Science Bulletin, 2005, 50(19):2201-2212.
DOI URL |
[36] |
KEPEZHINSKAS P, DEFANT M J, DRUMMOND M S. Progre-ssive enrichment of island arc mantle by melt-peridotite interaction inferred from Kamchatka xenoliths[J]. Geochimica et Cosmochimica Acta, 1996, 60(7):1217-1229.
DOI URL |
[37] |
FURMAN T, GRAHAM D. Erosion of lithospheric mantle beneath the East African Rift system: Geochemical evidence from the Kivu volcanic province[J]. Lithos, 1999, 48(1/4):237-262.
DOI URL |
[38] |
LATOURRETTE T, HERVIG R L, HOLLOWAY J R. Trace element partitioning between amphibole, phlogopite, and basanite melt[J]. Earth and Planetary Science Letters, 1995, 135(1/4):13-30.
DOI URL |
[39] | DUGGEN S, HOERNLE K, VAN D B P, et al. Post-collisional transition from subduction-to intraplate-type magmatism in the Westernmost Mediterranean: Evidence for continental-edge delamination of subcontinental lithosphere[J]. Journal of Petro-logy, 2005, 46(6):1155-1201. |
[40] |
MCKENZIE D, O’NIONS R K. Partial melt distributions from invertion of rare earth element concentrations[J]. Journal of Petrology, 1991, 32(5):1021-1091.
DOI URL |
[41] |
IRVING A J, FREY F A. Trace element abundances in megacrysts and their host rocks: Constraints on partition coefficients and megacryst genesis[J]. Geochimica et Cosmochimica Acta, 1984, 48(6):1201-1221.
DOI URL |
[42] | 翟明国, 孟庆任, 刘建明, 等. 华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨[J]. 地学前缘, 2004, 11(3):285-297. |
[43] |
MARUYAMA S, ISOZAKI Y, KIMURA G, et al. Paleogeographic maps of the Japanese islands: Plate tectonic synthesis from 750 Ma to the present[J]. Island Arc, 1997, 6(1):121-142.
DOI URL |
[44] | 陈广俊, 孙丰月, 李玉春, 等. 胶东郭家岭花岗闪长岩U-Pb年代学、地球化学特征及地质意义[J]. 世界地质, 2014, 33(1):39-47. |
[45] | 邵济安, 张履桥, 牟保磊. 大兴安岭中生代伸展造山过程中的岩浆作用[J]. 地学前缘, 1999, 6(4):339-346. |
[46] |
WU F Y, LIN J Q, WILDE S A, et al. Nature and significance of the Early Cretaceous giant igneous event in eastern China[J]. Earth and Planetary Science Letters, 2005, 233(1/2):103-119.
DOI URL |
[47] | 陈斌, 田伟, 翟明国, 等. 太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义[J]. 岩石学报, 2005, 21(1):13-24. |
[48] | FUKAO Y, OBAYASGI M, INOUE H. Subducting slabs stagnant in the mantle transition zone[J]. Journal of Geophysical Research: Solid Earth, 1992, 97(B4):4809-4822. |
[1] | ZHU Tuo, HE Dengyang, HUANG Yaqi, QIU Kunfeng. Apatite U-Pb Geochronology of the Trachy Dacite in Mashan Area, Jiaolai Basin, North China Craton, and Its Geological Significance [J]. Geoscience, 2024, 38(01): 117-127. |
[2] | HE Yunlong, ZHANG Guobin, YANG Yanchen, FENG Yue, KONG Jingui, CHEN Xingkai. Genesis and Tectonics of the Sipingshan Gold Deposit in Nadanhada Terrane, Sikhote-Alin Orogen: Constraints from Zircon U-Pb Chronology, Petrological and Fluid Geochemistry [J]. Geoscience, 2024, 38(01): 128-153. |
[3] | ZHOU Yan, FAN Feipeng, KANG Congxuan, ZHAO Xilin, XIAO Fan, XU Mincheng, SHEN Mangting, ZHU Yiping. Geochronological and Geochemical Characteristics of the Tianchitang Granodiorite in Southwestern Fujian Province: Indications for the Regional Metallogeny [J]. Geoscience, 2023, 37(06): 1467-1481. |
[4] | ZHANG Liang, CHEN Qi, GAO Tian, LI Wen, QIAN Jinlong, LIU Lijun, WANG Changming. Delicate Timescale of the Machangqing Porphyry Copper-Molybdenum Deposit in Sanjiang Tethyan Domain, SW China: Constraints from the Diffusion Chronology of Ti and Al in Quartz [J]. Geoscience, 2023, 37(06): 1509-1523. |
[5] | LUO Haiyi, LUO Xianrong, LIU Panfeng, MA Mingliang, LU Xiansheng, JIANG Xiaoming, BAO Guangui, JIANG Yuxiong. Soil Geochemical Characteristics in the Naqu Area,Chongzuo City, Guangxi,and Their Mineral Prospecting Applications [J]. Geoscience, 2023, 37(06): 1553-1566. |
[6] | LI Zhipeng, YU Qiling, ZAN Lin, YU Wenduan, ZHANG Zhihuan. Geochemical Characteristics and Hydrocarbon Generation Potential of Different Lithologic Source Rocks in the Second Member of Funing Formation in Qintong Sag, Subei Basin [J]. Geoscience, 2023, 37(05): 1345-1357. |
[7] | HAN Fei, SONG Yuanbao, ZHANG Wei, LI Daoling, HUANG Yonggao, LI Yingxu, JIA Xiaochuan, YANG Xuejun, YANG Qingsong, SONG Xubo, LU Liu. Petrogenesis and Tectonic Significance of the Late Triassic Nanmulin Intermediate-felsic Magmatic Rocks in the Gangdese Batholith, Southern Tibet [J]. Geoscience, 2023, 37(03): 547-561. |
[8] | WANG Xiangwei, ZHANG Baotao, YANG Haoqiang, HAN Jinguo. Geochronology, Geochemistry and Geological Significance of Tuanbaoshan Metamorphic Rocks in Haiyan, Qinghai Province [J]. Geoscience, 2023, 37(03): 586-598. |
[9] | ZHANG Wei, AN Maoguo, WANG Zhipeng, YANG Qi, CHEN Huaixin, MA Xiaofeng, ZHI Chenglong, XING Qitao, PEI Changshi, WANG Na, LIU Ming. Geochemical Characteristics of Stream Sediments and Prospecting in the Middle Reach of the Nalinggele River, Qinghai Province [J]. Geoscience, 2023, 37(03): 690-707. |
[10] | LIANG Dong, HUA Bei, ZHAO Dehuai, WU Hao, WAN Shengnan, TAN Chaoxin, ZHAO Xiaojian, YANG Zhipeng. Geochemical Characteristics of River Sediment and Ore Prediction in the Malashan Area of the Karakoram Region [J]. Geoscience, 2023, 37(03): 708-721. |
[11] | LOU Yuanlin, CHENG Ming, TANG Yao, ZHANG Chaoming, LAN Jingzhou, YUAN Yongsheng, YANG Tao. Geochemical Characteristics,Tectonic Setting, and Mineralization of Magmatic Rocks in Gudui Area, Southern Tibet [J]. Geoscience, 2023, 37(02): 353-374. |
[12] | LIU Jinbao, ZHU Luoting, LI Longxue, HOU Qingye. Geochemistry and Tectonic Significance of the Weijing Pluton in Airgin Sum Area, Inner Mongolia [J]. Geoscience, 2023, 37(02): 419-432. |
[13] | ZHANG Hongyu, YANG Liming, SU Li, SONG Shuguang, WANG Dachuan. LA-ICP-MS Monazite U(Th)-Pb Dating and Geological Applications [J]. Geoscience, 2023, 37(02): 443-462. |
[14] | CHEN Shiming, YANG Zhenxi, LEI Ziqiang, KANG Weiliang, ZHANG Jing, ZHAO Qinghu. Geochemical Characteristics and Prospecting on Stream Sediment Survey in Qianhongquan Area of Beishan in Gansu Province, China [J]. Geoscience, 2022, 36(06): 1513-1524. |
[15] | LIU Tong, LIU Chuanpeng, KANG Pengyu, ZHAO Xiufang, DENG Jun, WANG Kaikai. Geochemical Characteristics and Source Analysis of Heavy Metals in Soils of Eastern Yinan, Shandong Province [J]. Geoscience, 2022, 36(04): 1173-1182. |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||