Geoscience ›› 2024, Vol. 38 ›› Issue (01): 169-182.DOI: 10.19657/j.geoscience.1000-8527.2023.100
• Mineralogy, Petrology, Ore Deposits • Previous Articles Next Articles
CHEN Yaoxin1(), LIU Wenheng1,2(
), WANG Kaixing1,2, LIU Xiaodong2, SUN Liqiang1, YIN Donghua1
Received:
2023-06-25
Revised:
2023-12-20
Online:
2024-02-10
Published:
2024-03-20
CLC Number:
CHEN Yaoxin, LIU Wenheng, WANG Kaixing, LIU Xiaodong, SUN Liqiang, YIN Donghua. Petrogenesis and Tectonic Implications of the Zhongpai Fine-grained Granite in Qingshanbao, Gansu: Constraints from Geochemistry and Zircon U-Pb Chronology[J]. Geoscience, 2024, 38(01): 169-182.
样品 | 含量(10-6) | 232TH/ 238U | 同位素比值 | 同位素年龄(Ma) | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
232Th | 238U | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | |||
QSB21-2-1 | 192 | 547 | 0.35 | 0.05638 | 0.0035 | 0.50206 | 0.0302 | 0.06462 | 0.00114 | 466.6 | 132.7 | 413.1 | 20.4 | 403.6 | 6.9 | |
QSB21-2-2 | 469 | 1002 | 0.47 | 0.05283 | 0.00314 | 0.48336 | 0.02801 | 0.06637 | 0.00104 | 321.6 | 129.5 | 400.4 | 19.2 | 414.2 | 6.3 | |
QSB21-2-3 | 76 | 227 | 0.33 | 0.05326 | 0.00537 | 0.48769 | 0.04774 | 0.06641 | 0.00177 | 340.0 | 213.5 | 403.3 | 32.6 | 414.5 | 10.7 | |
QSB21-2-4 | 151 | 520 | 0.29 | 0.05545 | 0.00357 | 0.50919 | 0.03164 | 0.06659 | 0.00128 | 430.0 | 137.8 | 417.9 | 21.3 | 415.6 | 7.7 | |
QSB21-2-8 | 171 | 919 | 0.19 | 0.05474 | 0.00164 | 0.51073 | 0.01372 | 0.06761 | 0.00097 | 401.5 | 64.9 | 418.9 | 9.2 | 421.8 | 5.9 | |
QSB21-2-9 | 247 | 1169 | 0.21 | 0.05528 | 0.00197 | 0.50364 | 0.01647 | 0.06602 | 0.00101 | 423.4 | 77.2 | 414.2 | 11.1 | 412.1 | 6.1 | |
QSB21-2-12 | 449 | 2407 | 0.19 | 0.06011 | 0.00182 | 0.54539 | 0.01477 | 0.06582 | 0.00089 | 607.5 | 64.1 | 442.0 | 9.7 | 411.0 | 5.4 | |
QSB21-2-13 | 1232 | 3146 | 0.39 | 0.09385 | 0.00208 | 0.87823 | 0.01555 | 0.06791 | 0.00089 | 1505.0 | 41.3 | 640.0 | 8.4 | 423.6 | 5.4 | |
QSB21-2-14 | 658 | 1418 | 0.46 | 0.05491 | 0.00193 | 0.50772 | 0.01634 | 0.06712 | 0.00095 | 408.6 | 76.3 | 416.9 | 11.0 | 418.8 | 5.8 | |
QSB21-2-15 | 177 | 753 | 0.24 | 0.05748 | 0.00311 | 0.51905 | 0.02709 | 0.06558 | 0.00094 | 509.6 | 115.3 | 424.5 | 18.1 | 409.5 | 5.7 | |
QSB21-2-16 | 111 | 271 | 0.41 | 0.05649 | 0.00339 | 0.50795 | 0.02926 | 0.06539 | 0.00107 | 471.0 | 128.2 | 417.1 | 19.7 | 408.3 | 6.5 | |
QSB21-2-17 | 328 | 1254 | 0.26 | 0.05549 | 0.00157 | 0.50529 | 0.01223 | 0.06626 | 0.0009 | 431.6 | 61.4 | 415.3 | 8.3 | 413.6 | 5.5 | |
QSB21-2-19 | 381 | 1134 | 0.34 | 0.05448 | 0.00176 | 0.48773 | 0.01381 | 0.06522 | 0.00093 | 390.7 | 70.0 | 403.4 | 9.4 | 407.3 | 5.7 | |
QSB21-2-20 | 211 | 947 | 0.22 | 0.05783 | 0.00224 | 0.52039 | 0.01859 | 0.0656 | 0.00091 | 523.2 | 83.1 | 425.4 | 12.4 | 409.6 | 5.5 | |
QSB21-2-21 | 277 | 1030 | 0.27 | 0.05713 | 0.00292 | 0.52523 | 0.02562 | 0.06707 | 0.00092 | 496.0 | 109.3 | 428.6 | 17.1 | 418.5 | 5.5 |
Table 1 Zircon U-Pb isotopic analysis results for the Zhongpai fine-grained granites
样品 | 含量(10-6) | 232TH/ 238U | 同位素比值 | 同位素年龄(Ma) | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
232Th | 238U | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | 207Pb/ 206Pb | 1σ | 207Pb/ 235U | 1σ | 206Pb/ 238U | 1σ | |||
QSB21-2-1 | 192 | 547 | 0.35 | 0.05638 | 0.0035 | 0.50206 | 0.0302 | 0.06462 | 0.00114 | 466.6 | 132.7 | 413.1 | 20.4 | 403.6 | 6.9 | |
QSB21-2-2 | 469 | 1002 | 0.47 | 0.05283 | 0.00314 | 0.48336 | 0.02801 | 0.06637 | 0.00104 | 321.6 | 129.5 | 400.4 | 19.2 | 414.2 | 6.3 | |
QSB21-2-3 | 76 | 227 | 0.33 | 0.05326 | 0.00537 | 0.48769 | 0.04774 | 0.06641 | 0.00177 | 340.0 | 213.5 | 403.3 | 32.6 | 414.5 | 10.7 | |
QSB21-2-4 | 151 | 520 | 0.29 | 0.05545 | 0.00357 | 0.50919 | 0.03164 | 0.06659 | 0.00128 | 430.0 | 137.8 | 417.9 | 21.3 | 415.6 | 7.7 | |
QSB21-2-8 | 171 | 919 | 0.19 | 0.05474 | 0.00164 | 0.51073 | 0.01372 | 0.06761 | 0.00097 | 401.5 | 64.9 | 418.9 | 9.2 | 421.8 | 5.9 | |
QSB21-2-9 | 247 | 1169 | 0.21 | 0.05528 | 0.00197 | 0.50364 | 0.01647 | 0.06602 | 0.00101 | 423.4 | 77.2 | 414.2 | 11.1 | 412.1 | 6.1 | |
QSB21-2-12 | 449 | 2407 | 0.19 | 0.06011 | 0.00182 | 0.54539 | 0.01477 | 0.06582 | 0.00089 | 607.5 | 64.1 | 442.0 | 9.7 | 411.0 | 5.4 | |
QSB21-2-13 | 1232 | 3146 | 0.39 | 0.09385 | 0.00208 | 0.87823 | 0.01555 | 0.06791 | 0.00089 | 1505.0 | 41.3 | 640.0 | 8.4 | 423.6 | 5.4 | |
QSB21-2-14 | 658 | 1418 | 0.46 | 0.05491 | 0.00193 | 0.50772 | 0.01634 | 0.06712 | 0.00095 | 408.6 | 76.3 | 416.9 | 11.0 | 418.8 | 5.8 | |
QSB21-2-15 | 177 | 753 | 0.24 | 0.05748 | 0.00311 | 0.51905 | 0.02709 | 0.06558 | 0.00094 | 509.6 | 115.3 | 424.5 | 18.1 | 409.5 | 5.7 | |
QSB21-2-16 | 111 | 271 | 0.41 | 0.05649 | 0.00339 | 0.50795 | 0.02926 | 0.06539 | 0.00107 | 471.0 | 128.2 | 417.1 | 19.7 | 408.3 | 6.5 | |
QSB21-2-17 | 328 | 1254 | 0.26 | 0.05549 | 0.00157 | 0.50529 | 0.01223 | 0.06626 | 0.0009 | 431.6 | 61.4 | 415.3 | 8.3 | 413.6 | 5.5 | |
QSB21-2-19 | 381 | 1134 | 0.34 | 0.05448 | 0.00176 | 0.48773 | 0.01381 | 0.06522 | 0.00093 | 390.7 | 70.0 | 403.4 | 9.4 | 407.3 | 5.7 | |
QSB21-2-20 | 211 | 947 | 0.22 | 0.05783 | 0.00224 | 0.52039 | 0.01859 | 0.0656 | 0.00091 | 523.2 | 83.1 | 425.4 | 12.4 | 409.6 | 5.5 | |
QSB21-2-21 | 277 | 1030 | 0.27 | 0.05713 | 0.00292 | 0.52523 | 0.02562 | 0.06707 | 0.00092 | 496.0 | 109.3 | 428.6 | 17.1 | 418.5 | 5.5 |
样品号 | SiO2 | TiO2 | Al2O3 | TFe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | LOI | Total | A/ CNK | A/ NK | AKI | Mg# | K2O+ Na2O | K2O/ Na2O |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
QSB21-2 | 76.48 | 0.11 | 12.15 | 0.75 | 0.03 | 0.15 | 0.37 | 3.36 | 5.41 | 0.01 | 0.77 | 98.82 | 1.01 | 1.07 | 0.94 | 34.89 | 8.77 | 1.61 |
QSB21-3 | 76.08 | 0.10 | 12.32 | 0.71 | 0.02 | 0.10 | 0.46 | 3.43 | 5.11 | 0.01 | 0.87 | 98.34 | 1.02 | 1.10 | 0.91 | 28.99 | 8.54 | 1.49 |
QSB21-4 | 76.26 | 0.14 | 12.41 | 0.86 | 0.03 | 0.19 | 0.55 | 3.43 | 4.94 | 0.02 | 0.93 | 98.83 | 1.03 | 1.13 | 0.89 | 39.45 | 8.37 | 1.44 |
QSB21-5 | 75.99 | 0.10 | 12.14 | 0.76 | 0.02 | 0.13 | 0.48 | 3.45 | 5.02 | 0.01 | 0.94 | 98.10 | 1.01 | 1.09 | 0.92 | 33.63 | 8.47 | 1.46 |
QSB21-6 | 76.74 | 0.11 | 12.20 | 0.80 | 0.03 | 0.15 | 0.61 | 3.53 | 4.74 | 0.01 | 0.97 | 98.92 | 1.01 | 1.11 | 0.90 | 33.09 | 8.27 | 1.34 |
QSB21-7 | 77.12 | 0.09 | 12.44 | 0.74 | 0.03 | 0.11 | 0.42 | 3.36 | 5.30 | 0.01 | 0.86 | 99.62 | 1.03 | 1.10 | 0.91 | 30.00 | 8.66 | 1.58 |
QSB21-8 | 75.84 | 0.18 | 12.56 | 1.36 | 0.03 | 0.28 | 0.60 | 3.35 | 5.09 | 0.02 | 0.89 | 99.31 | 1.04 | 1.14 | 0.88 | 36.93 | 8.44 | 1.52 |
QSB21-9 | 76.62 | 0.10 | 12.42 | 0.85 | 0.03 | 0.10 | 0.43 | 3.32 | 5.43 | 0.01 | 0.67 | 99.31 | 1.02 | 1.09 | 0.91 | 24.10 | 8.75 | 1.63 |
样品号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | (La/ Yb)N | δEu | ΣREE | LREE/ HREE |
QSB21-2 | 23.1 | 54.7 | 5.46 | 19.5 | 4.31 | 0.34 | 3.76 | 0.65 | 4.23 | 0.86 | 2.71 | 0.45 | 3.27 | 0.50 | 5.07 | 0.25 | 123.84 | 6.54 |
QSB21-3 | 25.5 | 56.9 | 6.30 | 22.6 | 4.98 | 0.38 | 4.23 | 0.70 | 4.48 | 0.90 | 2.73 | 0.44 | 3.01 | 0.45 | 6.08 | 0.25 | 133.60 | 6.89 |
QSB21-4 | 32.3 | 66.6 | 7.25 | 25.1 | 5.08 | 0.49 | 4.17 | 0.68 | 4.24 | 0.86 | 2.61 | 0.41 | 2.71 | 0.41 | 8.55 | 0.32 | 152.91 | 8.50 |
QSB21-5 | 23.8 | 51.5 | 5.68 | 20.7 | 4.64 | 0.37 | 4.01 | 0.66 | 4.27 | 0.87 | 2.66 | 0.44 | 2.94 | 0.45 | 5.81 | 0.26 | 122.99 | 6.55 |
QSB21-6 | 26.3 | 56.5 | 6.25 | 22.2 | 5.09 | 0.41 | 4.55 | 0.75 | 4.73 | 0.97 | 2.97 | 0.46 | 3.10 | 0.46 | 6.09 | 0.26 | 134.74 | 6.49 |
QSB21-7 | 24.7 | 55.3 | 6.16 | 22.1 | 5.26 | 0.30 | 4.58 | 0.78 | 5.20 | 1.07 | 3.44 | 0.58 | 4.18 | 0.67 | 4.24 | 0.18 | 134.32 | 5.55 |
QSB21-8 | 28.2 | 57.3 | 6.77 | 24.5 | 5.54 | 0.48 | 4.75 | 0.79 | 4.95 | 0.99 | 2.95 | 0.49 | 3.38 | 0.53 | 5.98 | 0.28 | 141.62 | 6.52 |
QSB21-9 | 25.7 | 59.0 | 6.78 | 24.9 | 6.58 | 0.26 | 6.41 | 1.11 | 7.63 | 1.55 | 4.81 | 0.78 | 5.24 | 0.79 | 3.52 | 0.12 | 151.54 | 4.35 |
样品号 | Li | Be | Sc | V | Cr | Cs | Co | Ni | Cu | Ga | Sr | Rb | Ba | Th | U | Ta | Nb | P |
QSB21-2 | 3.50 | 2.42 | 2.80 | 9.00 | 2.00 | 3.07 | 1.00 | 1.40 | 1.50 | 13.60 | 61.40 | 208.00 | 226.00 | 37.40 | 5.72 | 2.55 | 23.20 | 60.00 |
QSB21-3 | 4.30 | 2.94 | 2.60 | 6.00 | 1.00 | 3.10 | 0.60 | 0.40 | 0.80 | 15.85 | 47.30 | 218.00 | 169.50 | 42.10 | 5.43 | 1.74 | 17.40 | 50.00 |
QSB21-4 | 7.60 | 4.06 | 2.80 | 8.00 | 3.00 | 3.39 | 1.30 | 1.90 | 8.50 | 15.10 | 57.40 | 222.00 | 228.00 | 27.40 | 5.42 | 1.85 | 18.10 | 80.00 |
QSB21-5 | 4.90 | 2.98 | 2.70 | 6.00 | 1.00 | 3.67 | 0.70 | 0.70 | 1.40 | 15.90 | 47.40 | 215.00 | 151.50 | 36.50 | 4.94 | 1.81 | 17.10 | 50.00 |
QSB21-6 | 8.00 | 3.70 | 3.50 | 6.00 | 2.00 | 4.54 | 0.70 | 0.90 | 1.40 | 15.25 | 51.40 | 229.00 | 168.00 | 34.10 | 6.71 | 1.90 | 20.70 | 60.00 |
QSB21-7 | 8.00 | 4.84 | 3.60 | 5.00 | 2.00 | 5.09 | 0.70 | 0.60 | 2.20 | 16.90 | 36.70 | 219.00 | 135.50 | 48.40 | 9.63 | 3.36 | 26.70 | 40.00 |
QSB21-8 | 18.30 | 4.44 | 4.80 | 14.00 | 8.00 | 7.08 | 1.70 | 2.70 | 1.40 | 16.60 | 57.50 | 238.00 | 197.00 | 39.30 | 7.52 | 2.55 | 25.60 | 120.00 |
QSB21-9 | 8.30 | 3.62 | 3.30 | 5.00 | 1.00 | 2.48 | 0.80 | 0.80 | 8.30 | 16.90 | 33.80 | 220.00 | 103.50 | 53.70 | 11.80 | 2.71 | 30.20 | 50.00 |
样品号 | Zr | Hf | Y | Ti | Zn | Mo | Bi | Sn | Pb | K | Nb/U | Rb/Sr | Ti/Zr | Nb/Ta | K/ Rb | TZr (℃) | Zr+Nb+ Ce+Y | 10000 Ga/Al |
QSB21-2 | 105.00 | 4.30 | 24.4 | 680 | 11.00 | 0.25 | 0.07 | 1.70 | 32.0 | 43800 | 4.06 | 3.40 | 6.48 | 9.10 | 210.58 | 792.00 | 207.30 | 2.11 |
QSB21-3 | 85.00 | 3.70 | 26.0 | 640 | 13.00 | 0.14 | 0.04 | 1.70 | 34.6 | 42800 | 3.20 | 4.60 | 7.53 | 10.00 | 196.33 | 774.00 | 185.30 | 2.43 |
QSB21-4 | 80.00 | 3.30 | 25.3 | 880 | 14.00 | 0.34 | 0.07 | 1.60 | 33.1 | 41300 | 3.34 | 3.90 | 11.00 | 9.78 | 186.04 | 769.00 | 190.00 | 2.30 |
QSB21-5 | 91.00 | 3.80 | 25.2 | 680 | 12.00 | 0.13 | 0.05 | 1.90 | 33.6 | 42400 | 3.46 | 4.50 | 7.47 | 9.45 | 197.21 | 779.00 | 184.80 | 2.47 |
QSB21-6 | 77.00 | 3.20 | 26.8 | 700 | 15.00 | 0.23 | 0.09 | 2.30 | 34.7 | 39000 | 3.08 | 4.50 | 9.09 | 10.89 | 170.31 | 764.00 | 181.00 | 2.36 |
QSB21-7 | 127.00 | 5.50 | 31.1 | 620 | 11.00 | 0.22 | 0.11 | 2.10 | 37.1 | 45100 | 2.77 | 6.00 | 4.88 | 7.95 | 205.94 | 811.00 | 240.10 | 2.57 |
QSB21-8 | 122.00 | 4.90 | 27.9 | 1160 | 23.00 | 0.76 | 0.14 | 4.40 | 35.8 | 41600 | 3.40 | 4.10 | 9.51 | 10.04 | 174.79 | 805.00 | 232.80 | 2.50 |
QSB21-9 | 147.00 | 6.00 | 43.0 | 660 | 11.00 | 0.25 | 0.05 | 1.50 | 35.0 | 45500 | 2.56 | 6.50 | 4.49 | 11.14 | 206.82 | 823.00 | 279.20 | 2.57 |
Table 2 Major (%) and trace (10-6) element data for the Zhongpai fine-grained granites
样品号 | SiO2 | TiO2 | Al2O3 | TFe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | LOI | Total | A/ CNK | A/ NK | AKI | Mg# | K2O+ Na2O | K2O/ Na2O |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
QSB21-2 | 76.48 | 0.11 | 12.15 | 0.75 | 0.03 | 0.15 | 0.37 | 3.36 | 5.41 | 0.01 | 0.77 | 98.82 | 1.01 | 1.07 | 0.94 | 34.89 | 8.77 | 1.61 |
QSB21-3 | 76.08 | 0.10 | 12.32 | 0.71 | 0.02 | 0.10 | 0.46 | 3.43 | 5.11 | 0.01 | 0.87 | 98.34 | 1.02 | 1.10 | 0.91 | 28.99 | 8.54 | 1.49 |
QSB21-4 | 76.26 | 0.14 | 12.41 | 0.86 | 0.03 | 0.19 | 0.55 | 3.43 | 4.94 | 0.02 | 0.93 | 98.83 | 1.03 | 1.13 | 0.89 | 39.45 | 8.37 | 1.44 |
QSB21-5 | 75.99 | 0.10 | 12.14 | 0.76 | 0.02 | 0.13 | 0.48 | 3.45 | 5.02 | 0.01 | 0.94 | 98.10 | 1.01 | 1.09 | 0.92 | 33.63 | 8.47 | 1.46 |
QSB21-6 | 76.74 | 0.11 | 12.20 | 0.80 | 0.03 | 0.15 | 0.61 | 3.53 | 4.74 | 0.01 | 0.97 | 98.92 | 1.01 | 1.11 | 0.90 | 33.09 | 8.27 | 1.34 |
QSB21-7 | 77.12 | 0.09 | 12.44 | 0.74 | 0.03 | 0.11 | 0.42 | 3.36 | 5.30 | 0.01 | 0.86 | 99.62 | 1.03 | 1.10 | 0.91 | 30.00 | 8.66 | 1.58 |
QSB21-8 | 75.84 | 0.18 | 12.56 | 1.36 | 0.03 | 0.28 | 0.60 | 3.35 | 5.09 | 0.02 | 0.89 | 99.31 | 1.04 | 1.14 | 0.88 | 36.93 | 8.44 | 1.52 |
QSB21-9 | 76.62 | 0.10 | 12.42 | 0.85 | 0.03 | 0.10 | 0.43 | 3.32 | 5.43 | 0.01 | 0.67 | 99.31 | 1.02 | 1.09 | 0.91 | 24.10 | 8.75 | 1.63 |
样品号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | (La/ Yb)N | δEu | ΣREE | LREE/ HREE |
QSB21-2 | 23.1 | 54.7 | 5.46 | 19.5 | 4.31 | 0.34 | 3.76 | 0.65 | 4.23 | 0.86 | 2.71 | 0.45 | 3.27 | 0.50 | 5.07 | 0.25 | 123.84 | 6.54 |
QSB21-3 | 25.5 | 56.9 | 6.30 | 22.6 | 4.98 | 0.38 | 4.23 | 0.70 | 4.48 | 0.90 | 2.73 | 0.44 | 3.01 | 0.45 | 6.08 | 0.25 | 133.60 | 6.89 |
QSB21-4 | 32.3 | 66.6 | 7.25 | 25.1 | 5.08 | 0.49 | 4.17 | 0.68 | 4.24 | 0.86 | 2.61 | 0.41 | 2.71 | 0.41 | 8.55 | 0.32 | 152.91 | 8.50 |
QSB21-5 | 23.8 | 51.5 | 5.68 | 20.7 | 4.64 | 0.37 | 4.01 | 0.66 | 4.27 | 0.87 | 2.66 | 0.44 | 2.94 | 0.45 | 5.81 | 0.26 | 122.99 | 6.55 |
QSB21-6 | 26.3 | 56.5 | 6.25 | 22.2 | 5.09 | 0.41 | 4.55 | 0.75 | 4.73 | 0.97 | 2.97 | 0.46 | 3.10 | 0.46 | 6.09 | 0.26 | 134.74 | 6.49 |
QSB21-7 | 24.7 | 55.3 | 6.16 | 22.1 | 5.26 | 0.30 | 4.58 | 0.78 | 5.20 | 1.07 | 3.44 | 0.58 | 4.18 | 0.67 | 4.24 | 0.18 | 134.32 | 5.55 |
QSB21-8 | 28.2 | 57.3 | 6.77 | 24.5 | 5.54 | 0.48 | 4.75 | 0.79 | 4.95 | 0.99 | 2.95 | 0.49 | 3.38 | 0.53 | 5.98 | 0.28 | 141.62 | 6.52 |
QSB21-9 | 25.7 | 59.0 | 6.78 | 24.9 | 6.58 | 0.26 | 6.41 | 1.11 | 7.63 | 1.55 | 4.81 | 0.78 | 5.24 | 0.79 | 3.52 | 0.12 | 151.54 | 4.35 |
样品号 | Li | Be | Sc | V | Cr | Cs | Co | Ni | Cu | Ga | Sr | Rb | Ba | Th | U | Ta | Nb | P |
QSB21-2 | 3.50 | 2.42 | 2.80 | 9.00 | 2.00 | 3.07 | 1.00 | 1.40 | 1.50 | 13.60 | 61.40 | 208.00 | 226.00 | 37.40 | 5.72 | 2.55 | 23.20 | 60.00 |
QSB21-3 | 4.30 | 2.94 | 2.60 | 6.00 | 1.00 | 3.10 | 0.60 | 0.40 | 0.80 | 15.85 | 47.30 | 218.00 | 169.50 | 42.10 | 5.43 | 1.74 | 17.40 | 50.00 |
QSB21-4 | 7.60 | 4.06 | 2.80 | 8.00 | 3.00 | 3.39 | 1.30 | 1.90 | 8.50 | 15.10 | 57.40 | 222.00 | 228.00 | 27.40 | 5.42 | 1.85 | 18.10 | 80.00 |
QSB21-5 | 4.90 | 2.98 | 2.70 | 6.00 | 1.00 | 3.67 | 0.70 | 0.70 | 1.40 | 15.90 | 47.40 | 215.00 | 151.50 | 36.50 | 4.94 | 1.81 | 17.10 | 50.00 |
QSB21-6 | 8.00 | 3.70 | 3.50 | 6.00 | 2.00 | 4.54 | 0.70 | 0.90 | 1.40 | 15.25 | 51.40 | 229.00 | 168.00 | 34.10 | 6.71 | 1.90 | 20.70 | 60.00 |
QSB21-7 | 8.00 | 4.84 | 3.60 | 5.00 | 2.00 | 5.09 | 0.70 | 0.60 | 2.20 | 16.90 | 36.70 | 219.00 | 135.50 | 48.40 | 9.63 | 3.36 | 26.70 | 40.00 |
QSB21-8 | 18.30 | 4.44 | 4.80 | 14.00 | 8.00 | 7.08 | 1.70 | 2.70 | 1.40 | 16.60 | 57.50 | 238.00 | 197.00 | 39.30 | 7.52 | 2.55 | 25.60 | 120.00 |
QSB21-9 | 8.30 | 3.62 | 3.30 | 5.00 | 1.00 | 2.48 | 0.80 | 0.80 | 8.30 | 16.90 | 33.80 | 220.00 | 103.50 | 53.70 | 11.80 | 2.71 | 30.20 | 50.00 |
样品号 | Zr | Hf | Y | Ti | Zn | Mo | Bi | Sn | Pb | K | Nb/U | Rb/Sr | Ti/Zr | Nb/Ta | K/ Rb | TZr (℃) | Zr+Nb+ Ce+Y | 10000 Ga/Al |
QSB21-2 | 105.00 | 4.30 | 24.4 | 680 | 11.00 | 0.25 | 0.07 | 1.70 | 32.0 | 43800 | 4.06 | 3.40 | 6.48 | 9.10 | 210.58 | 792.00 | 207.30 | 2.11 |
QSB21-3 | 85.00 | 3.70 | 26.0 | 640 | 13.00 | 0.14 | 0.04 | 1.70 | 34.6 | 42800 | 3.20 | 4.60 | 7.53 | 10.00 | 196.33 | 774.00 | 185.30 | 2.43 |
QSB21-4 | 80.00 | 3.30 | 25.3 | 880 | 14.00 | 0.34 | 0.07 | 1.60 | 33.1 | 41300 | 3.34 | 3.90 | 11.00 | 9.78 | 186.04 | 769.00 | 190.00 | 2.30 |
QSB21-5 | 91.00 | 3.80 | 25.2 | 680 | 12.00 | 0.13 | 0.05 | 1.90 | 33.6 | 42400 | 3.46 | 4.50 | 7.47 | 9.45 | 197.21 | 779.00 | 184.80 | 2.47 |
QSB21-6 | 77.00 | 3.20 | 26.8 | 700 | 15.00 | 0.23 | 0.09 | 2.30 | 34.7 | 39000 | 3.08 | 4.50 | 9.09 | 10.89 | 170.31 | 764.00 | 181.00 | 2.36 |
QSB21-7 | 127.00 | 5.50 | 31.1 | 620 | 11.00 | 0.22 | 0.11 | 2.10 | 37.1 | 45100 | 2.77 | 6.00 | 4.88 | 7.95 | 205.94 | 811.00 | 240.10 | 2.57 |
QSB21-8 | 122.00 | 4.90 | 27.9 | 1160 | 23.00 | 0.76 | 0.14 | 4.40 | 35.8 | 41600 | 3.40 | 4.10 | 9.51 | 10.04 | 174.79 | 805.00 | 232.80 | 2.50 |
QSB21-9 | 147.00 | 6.00 | 43.0 | 660 | 11.00 | 0.25 | 0.05 | 1.50 | 35.0 | 45500 | 2.56 | 6.50 | 4.49 | 11.14 | 206.82 | 823.00 | 279.20 | 2.57 |
Fig.6 Spider diagrams of chondrite-normalized REE (a) and primitive mantle-normalized trace elements (b) of the Zhongpai fine-grained granites (after McDonough and Sun [16])
Fig.8 Sr-Ba (a) and La-(LA/Yb)N (b) diagrams showing the fractional crystallization trends of the Zhongpai fine-grained granites Partition coefficients of Sr and Ba used in Fig.(a) are from Blundy and Shimizu[38] for plagioclase,and from Ewart and Griffin[39] for other minerals.The fractionation trends for accessory minerals shown in Fig.(b) are from Wu et al. [28], and the data on the lines represent the fractionation degree.Plan10.plagioclase with An = 10; Plan50.plagioclase with An = 50; Kf.K-feldspar; Bi.biotite; Amp.amphibole, Zr.zircon, Sph.sphene, Ap.apatite;Mon.monazite; Allan.allanite
Fig.9 Tectonic environment discrimination diagrams of Early Paleozoic intrusive rocks in Longshoushan Subduction (data of granites from refs.[2-3,44⇓⇓-47], and post-collision granites from refs[4,6⇓-8,19⇓-21,31,41-42])
位置 | 岩性 | 年龄(Ma) | 参考文献 |
---|---|---|---|
龙首山芨岭 | 肉红色中粗粒花岗岩 | 426.4±2.0 | 陈云杰等[ |
龙首山牛角沟 | 石英二长花岗岩 | 447.0±5.2 | 陈云杰等[ |
青山堡 | 灰绿色闪长玢岩 | 422.3±3.6 | 陈云杰等[ |
龙首山西井 | 橄榄辉石和辉长岩 | 421±9.0 | 段俊等[ |
青山堡 | 花岗闪长岩 | 451.5±3.2 | 何佳军等[ |
龙首山红石泉 | 正长岩 | 416±0.17 | 冷天赐等[ |
青山堡 | 中粗粒钾长花岗岩 | 441.6±4.2 | 刘文恒等[ |
青山堡 | 细晶花岗岩 | 430.1±5.6 | 刘文恒等[ |
龙首山青山堡 | 细粒闪长岩 | 438.6±4.7 | 牛宇奔[ |
大佛寺 | 花岗岩 | 426.1±2.8 | 孙宝璐等[ |
龙首山芨岭 | 花岗岩 | 428.6±8.1 | 汤琳[ |
龙首山芨岭 | 黑云母二长花岗岩 | 425.2±3.0 | 汤琳[ |
龙首山芨岭 | 二长花岗斑岩 | 416.6±9.2 | 汤琳[ |
龙首山芨岭 | 斑状黑云母二长花岗岩 | 412.8±9 | 汤琳[ |
龙首山大佛寺 | 碱性长石花岗岩 | 426±2.0 | 王增振等[ |
河西堡孟家大湾 | 花岗岩 | 444±2.0 | 魏俏巧等[ |
龙首山芨岭 | A型似斑状花岗岩 | 458.3±2.3 | 张甲民等[ |
龙首山莲花山 | 花岗闪长岩 | 441±4 | 张丽琪[ |
龙首山孟家大湾 | 花岗闪长岩 | 441±3 | 张丽琪[ |
龙首山芨岭 | 角闪辉长岩 | 441±2 | 张丽琪[ |
龙首山西井 | 二长岩 | 438±4 | 张丽琪[ |
杨前大山 | 花岗闪长岩 | 427±4 | 张丽琪[ |
龙首山孟家大湾 | 石英闪长岩 | 424±2 | 张丽琪[ |
龙首山圣容寺 | 钾长花岗岩 | 422±2 | 张丽琪[ |
新开沟 | 似斑状花岗岩 | 419±4 | 张丽琪[ |
新开沟 | 细粒花岗岩 | 414±3 | 张丽琪[ |
龙首山芨岭 | 正长岩 | 427.2±3.6 | 张志强等[ |
龙首山牛角沟 | 中粗粒花岗岩 | 445.2±7.8 | 赵如意等[ |
龙首山芨岭 | 纳长岩 | 442.9±5.7 | 赵如意等[ |
Table 3 Statistical data of zircon U-Pb ages of the Early Paleozoic intrusive rocks in Longshoushan
位置 | 岩性 | 年龄(Ma) | 参考文献 |
---|---|---|---|
龙首山芨岭 | 肉红色中粗粒花岗岩 | 426.4±2.0 | 陈云杰等[ |
龙首山牛角沟 | 石英二长花岗岩 | 447.0±5.2 | 陈云杰等[ |
青山堡 | 灰绿色闪长玢岩 | 422.3±3.6 | 陈云杰等[ |
龙首山西井 | 橄榄辉石和辉长岩 | 421±9.0 | 段俊等[ |
青山堡 | 花岗闪长岩 | 451.5±3.2 | 何佳军等[ |
龙首山红石泉 | 正长岩 | 416±0.17 | 冷天赐等[ |
青山堡 | 中粗粒钾长花岗岩 | 441.6±4.2 | 刘文恒等[ |
青山堡 | 细晶花岗岩 | 430.1±5.6 | 刘文恒等[ |
龙首山青山堡 | 细粒闪长岩 | 438.6±4.7 | 牛宇奔[ |
大佛寺 | 花岗岩 | 426.1±2.8 | 孙宝璐等[ |
龙首山芨岭 | 花岗岩 | 428.6±8.1 | 汤琳[ |
龙首山芨岭 | 黑云母二长花岗岩 | 425.2±3.0 | 汤琳[ |
龙首山芨岭 | 二长花岗斑岩 | 416.6±9.2 | 汤琳[ |
龙首山芨岭 | 斑状黑云母二长花岗岩 | 412.8±9 | 汤琳[ |
龙首山大佛寺 | 碱性长石花岗岩 | 426±2.0 | 王增振等[ |
河西堡孟家大湾 | 花岗岩 | 444±2.0 | 魏俏巧等[ |
龙首山芨岭 | A型似斑状花岗岩 | 458.3±2.3 | 张甲民等[ |
龙首山莲花山 | 花岗闪长岩 | 441±4 | 张丽琪[ |
龙首山孟家大湾 | 花岗闪长岩 | 441±3 | 张丽琪[ |
龙首山芨岭 | 角闪辉长岩 | 441±2 | 张丽琪[ |
龙首山西井 | 二长岩 | 438±4 | 张丽琪[ |
杨前大山 | 花岗闪长岩 | 427±4 | 张丽琪[ |
龙首山孟家大湾 | 石英闪长岩 | 424±2 | 张丽琪[ |
龙首山圣容寺 | 钾长花岗岩 | 422±2 | 张丽琪[ |
新开沟 | 似斑状花岗岩 | 419±4 | 张丽琪[ |
新开沟 | 细粒花岗岩 | 414±3 | 张丽琪[ |
龙首山芨岭 | 正长岩 | 427.2±3.6 | 张志强等[ |
龙首山牛角沟 | 中粗粒花岗岩 | 445.2±7.8 | 赵如意等[ |
龙首山芨岭 | 纳长岩 | 442.9±5.7 | 赵如意等[ |
[1] | 周立发. 阿拉善地块南缘早古生代大地构造特征和演化[J]. 西北大学学报(自然科学版), 1992, 22(1): 107-115. |
[2] | 何佳军, 邵东, 王刚, 等. 甘肃龙首山青山堡花岗闪长岩锆石U-Pb年龄、地球化学特征及地质意义[J]. 矿产与地质, 2022, 36(3): 596-606. |
[3] | 陈云杰, 赵如意, 王刚, 等. 甘肃龙首山牛角沟地区中粗粒石英二长花岗岩年代学与元素地球化学特征及其地质意义[J]. 东华理工大学学报(自然科学版), 2020, 43(1): 21-29. |
[4] | 刘文恒, 潘家永, 刘晓东, 等. 甘肃龙首山青山堡花岗岩成因及其构造意义: 元素地球化学、锆石U-Pb年龄和Sr-Nd同位素约束[J]. 矿物岩石, 2019, 39(4): 26-40. |
[5] | 牛宇奔. 甘肃龙首山青山堡岩体地质地球化学特征与成岩因研究[D]. 抚州: 东华理工大学, 2019. |
[6] | 王增振, 陈宣华, 邵兆刚, 等. 甘肃龙首山—合黎山晚志留世—早泥盆世花岗岩类的成因及其对阿拉善地块西南缘早古生代构造演化的约束[J]. 地质学报, 2020, 94(8): 2243-2261. |
[7] | 冷天赐, 刘文恒, 余驰达, 等. 甘肃龙首山红石泉正长岩地球化学特征及成因探讨[J]. 矿物岩石, 2021, 41(3): 72-83. |
[8] | 张丽琪. 北祁连—阿拉善地块南缘古生代碰撞后岩浆作用及深部过程[D]. 武汉: 中国地质大学, 2019. |
[9] | 邱检生, 胡建, 王孝磊, 等. 广东河源白石冈岩体: 一个高分异的I型花岗岩[J]. 地质学报, 2005, 79(4): 503-514. |
[10] | 苏扣林. 广东良口黄田埔高分异Ⅰ型花岗岩地球化学特征及大地构造意义[J]. 地质学刊, 2018, 42(2): 197-205. |
[11] | 黄孔文, 郭敏, 林杰春, 等. 粤北白沙地区晚侏罗世高分异Ⅰ型细粒花岗岩年代学、地球化学特征及其地质意义[J]. 矿床地质, 2020, 39(5): 926-944. |
[12] | 李响, 王令占, 涂兵, 等. 广东连山地区禾洞高分异花岗岩的锆石U-Pb年代学及岩石成因[J]. 地球科学, 2023, 48(10):3577-3596. |
[13] |
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 |
[14] |
MANIAR P D, PICCOLI P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989, 101(5): 635-643.
DOI URL |
[15] |
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 |
[16] |
MCDONOUGH W F, SUN S S. The composition of the earth[J]. Chemical Geology, 1995, 120(3/4): 223-253.
DOI URL |
[17] |
WATSON E B, HARRISON T M. Zircon saturation revisited: Temperature and composition effects in a variety of crustal magma types[J]. Earth and Planetary Science Letters, 1983, 64(2): 295-304.
DOI URL |
[18] | PITCHER W S. The Nature and Origin of Granite[M]. 2nd Edi.London: Chapman & Hall, 1997. |
[19] | 张志强, 王凯兴, 王刚, 等. 甘肃龙首山芨岭地区古生代正长岩成因及构造意义[J]. 地质论评, 2018, 64(4): 1017-1029. |
[20] | 汤琳. 甘肃龙首山芨岭地区花岗岩特征及锆石LA-ICP-MS U-Pb定年[D]. 抚州: 东华理工大学, 2015. |
[21] | 陈云杰, 王刚, 王伟, 等. 龙首山芨岭地区中粗粒花岗岩地质特征及其地质意义[J]. 铀矿地质, 2022, 38(6): 1111-1121. |
[22] | 刘昌实, 陈小明, 陈培荣, 等. A型岩套的分类、判别标志和成因[J]. 高校地质学报, 2003, 9(4): 573-591. |
[23] |
WHALEN J B, CURRIE K L, CHAPPELL B W. A-type gra-nites: Geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95(4): 407-419.
DOI URL |
[24] | 吴福元, 刘小驰, 纪伟强, 等. 高分异花岗岩的识别与研究[J]. 中国科学(地球科学), 2017, 47(7): 745-765. |
[25] | 吴福元, 李献华, 杨进辉, 等. 花岗岩成因研究的若干问题[J]. 岩石学报, 2007, 23(6): 1217-1238. |
[26] |
PICHAVANT M, MONTEL J M, RICHARD L R. Apatite solubility in peraluminous liquids: Experimental data and an extension of the Harrison-Watson model[J]. Geochimica et Cosmochimica Acta, 1992, 56(10): 3855-3861.
DOI URL |
[27] |
CHAPPELL B W. Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites[J]. Lithos, 1999, 46(3): 535-551.
DOI URL |
[28] |
WU F Y, JAHN B M, WILDE S A, et al. Highly fractionated I-type granites in NE China (I): Geochronology and petrogenesis[J]. Lithos, 2003, 66(3/4): 241-273.
DOI URL |
[29] |
WANG X S, BI X W, LENG C B, et al. Geochronology and geochemistry of Late Cretaceous igneous intrusions and Mo-Cu-(W) mineralization in the southern Yidun Arc, SW China: Implications for metallogenesis and geodynamic setting[J]. Ore Geology Reviews, 2014, 61: 73-95.
DOI URL |
[30] | 邱检生, 肖娥, 胡建, 等. 福建北东沿海高分异Ⅰ型花岗岩的成因: 锆石U-Pb年代学、地球化学和Nd-Hf同位素制约[J]. 岩石学报, 2008, 24(11): 2468-2484. |
[31] | 段俊, 钱壮志, 焦建刚, 等. 甘肃龙首山岩带西井镁铁质岩体成因及其构造意义[J]. 吉林大学学报(地球科学版), 2015, 45(3): 832-846. |
[32] |
DEFANT M J, DRUMMOND M S. Derivation of some modern arc magmas by melting of young subductedlithosphere[J]. Nature, 1990, 347(6294): 662-665.
DOI |
[33] | 许逢明, 孙巍, 吴大天, 等. 大兴安岭北段免渡河地区晚石炭世二长花岗岩成因:锆石U-Pb年代学、Hf同位素和地球化学证据[J]. 地球科学, 2022, 47(8): 2839-2855. |
[34] |
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 |
[35] | WILSON M. Igneous Petrogenesis[M]. London: Unwin Hyman, 1989. |
[36] | TAYLOR S R, MCLENNAN S M. The Continental Crust:Its Composition and Evolution:An Examination of the Geochemical Record Preserved in Sedimentary rocks[M]. Boston: Blackwell Scientific Publication, 1985:209-230. |
[37] | BAS M J L. Using geochemical data: evaluation, presentation, interpretation[J]. Mineralogical Magazine, 1994, 58:523-523. |
[38] |
BLUNDY J D, SHIMIZU N. Trace element evidence for plagioclase recycling in calc-alkaline magmas[J]. Earth and Planetary Science Letters, 1991, 102(2): 178-197.
DOI URL |
[39] |
EWART A, GRIFFIN W L. Application of proton-microprobe data to trace-element partitioning in volcanic rocks[J]. Chemical Geology, 1994, 117(1/2/3/4): 251-284.
DOI URL |
[40] | 张旗, 潘国强, 李承东, 等. 花岗岩构造环境问题:关于花岗岩研究的思考之三[J]. 岩石学报, 2007, 23(11): 2683-2698. |
[41] | 孙宝璐, 钱青, 张建新. 甘肃大佛寺、金佛寺花岗岩体的锆石U-Pb年龄、Hf-O同位素和全岩地球化学特征及地质意义[J]. 岩石学报, 2017, 33(10): 3091-3108. |
[42] | 陈云杰, 王刚, 赵如意, 等. 甘肃龙首山成矿带东段闪长玢岩锆石U-Pb年龄及其地质意义[J]. 铀矿地质, 2021, 37(1): 38-50, 111. |
[43] |
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 |
[44] | 张甲民, 赵如意, 王刚, 等. 甘肃龙首山芨岭铀矿区A型似斑状花岗岩地质特征及其地质意义[J]. 矿物岩石地球化学通报, 2017, 36(5): 813-823. |
[45] | 赵如意, 王博, 陈毓川, 等. 甘肃省龙首山牛角沟铀矿点钾钠混合交代作用研究[J]. 地质学报, 2018, 92(12): 2469-2484. |
[46] | 魏俏巧, 郝立波, 陆继龙, 等. 甘肃河西堡花岗岩LA-MC-ICP-MS锆石U-Pb年龄及其地质意义[J]. 矿物岩石地球化学通报, 2013, 32(6): 729-735. |
[47] | 赵如意, 姜常义, 陈旭, 等. 甘肃省龙首山成矿带中段钠长岩脉地质特征及其与铀矿化关系研究[J]. 地质与勘探, 2015, 51(6): 1069-1078. |
[48] | 相振群, 陆松年, 李怀坤, 等. 北祁连西段熬油沟辉长岩的锆石SHRIMP U-Pb年龄及地质意义[J]. 地质通报, 2007, 26(12): 1686-1691. |
[49] | 曾建元, 杨怀仁, 杨宏仪, 等. 北祁连东草河蛇绿岩: 一个早古生代的洋壳残片[J]. 科学通报, 2007, 52(7): 825-835. |
[50] | 孟繁聪, 张建新, 郭春满, 等. 大岔大坂MOR型和SSZ型蛇绿岩对北祁连洋演化的制约[J]. 岩石矿物学杂志, 2010, 29(5): 453-466. |
[51] | 武鹏, 李向民, 徐学义, 等. 北祁连山扎麻什地区东沟蛇绿岩LA-ICP-MS锆石U-Pb测年及其地球化学特征[J]. 地质通报, 2012, 31(6): 896-906. |
[52] | 夏小洪, 孙楠, 宋述光, 等. 北祁连西段熬油沟二只哈拉达坂蛇绿岩的形成环境和时代[J]. 北京大学学报(自然科学版), 2012, 48(5): 757-769. |
[53] | 宋述光, 张立飞, NIU Y, 等. 北祁连山榴辉岩锆石SHRIMP定年及其构造意义[J]. 科学通报, 2004, 49(6): 592-595. |
[54] |
ZHANG J X, MENG F C, WAN Y S. A cold Early Palaeozoic subduction zone in the North Qilian Mountains, NW China: Petrological and U-Pb geochronological constraints[J]. Journal of Metamorphic Geology, 2007, 25(3): 285-304.
DOI URL |
[55] |
ZHANG L, CHEN R X, ZHENG Y F, et al. Geochemical constraints on the protoliths of eclogites and blueschists from North Qilian, northern Tibet[J]. Chemical Geology, 2016, 421: 26-43.
DOI URL |
[56] | 喻星星, 张建新. 北祁连香子沟榴辉岩相变沉积岩的锆石U-Pb年代学、Hf同位素特征及其地质意义[J]. 岩石学报, 2016, 32(5): 1437-1451. |
[57] |
SONG S G, NIU Y L, SU L, et al. Tectonics of the North Qilian orogen, NW China[J]. Gondwana Research, 2013, 23(4): 1378-1401.
DOI URL |
[58] |
XU Y J, DU Y S, CAWOOD P A, et al. Provenance record of a foreland basin: Detrital zircon U-Pb ages from Devonian strata in the North Qilian Orogenic Belt, China[J]. Tectonophysics, 2010, 495(3/4): 337-347.
DOI URL |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||