Geoscience ›› 2021, Vol. 35 ›› Issue (03): 763-775.DOI: 10.19657/j.geoscience.1000-8527.2021.034
• Petrology • Previous Articles Next Articles
ZHANG Yu1,2(), TANG Mingying3, CUI Xiaofeng1, HE Yuliang2,4, DONG Weidong4
Received:
2020-04-16
Revised:
2020-12-01
Online:
2021-06-23
Published:
2021-06-24
CLC Number:
ZHANG Yu, TANG Mingying, CUI Xiaofeng, HE Yuliang, DONG Weidong. Northward Subduction of Subashi Ocean in Eastern Part of the West Kunlun Orogen: Evidence from Early-Middle Permian Volcanic Rocks[J]. Geoscience, 2021, 35(03): 763-775.
样品号 (岩性) | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | 207Pb/ 206Pb | 207Pb/ 235U | 206Pb/ 238U | ||||
3706-U-Pb01 (酸性晶屑 凝灰岩) | 1 | 211 | 382 | 0.55 | 0.047±0.002 | 0.292±0.015 | 0.045±0.000 6 | 47 | 260 | 284 | |
2 | 113 | 151 | 0.74 | 0.052±0.004 | 0.321±0.022 | 0.045±0.000 7 | 264 | 283 | 285 | ||
4 | 91 | 185 | 0.49 | 0.053±0.005 | 0.330±0.030 | 0.045±0.001 0 | 325 | 289 | 285 | ||
6 | 381 | 2 149 | 0.18 | 0.055±0.002 | 0.339±0.010 | 0.045±0.000 4 | 404 | 297 | 283 | ||
8 | 286 | 689 | 0.42 | 0.055±0.002 | 0.341±0.011 | 0.045±0.000 4 | 414 | 298 | 283 | ||
9 | 376 | 889 | 0.42 | 0.055±0.001 | 0.342±0.006 | 0.045±0.000 3 | 416 | 299 | 284 | ||
10 | 222 | 797 | 0.28 | 0.053±0.002 | 0.331±0.009 | 0.045±0.000 4 | 342 | 290 | 284 | ||
11 | 193 | 599 | 0.32 | 0.057±0.002 | 0.352±0.011 | 0.045±0.000 4 | 479 | 306 | 284 | ||
12 | 328 | 714 | 0.46 | 0.054±0.003 | 0.336±0.016 | 0.045±0.000 6 | 360 | 294 | 286 | ||
13 | 146 | 573 | 0.25 | 0.056±0.002 | 0.345±0.013 | 0.045±0.000 5 | 440 | 301 | 284 | ||
14 | 132 | 277 | 0.48 | 0.052±0.003 | 0.322±0.016 | 0.045±0.000 6 | 271 | 283 | 285 | ||
19 | 157 | 711 | 0.22 | 0.055±0.003 | 0.343±0.019 | 0.045±0.000 7 | 415 | 300 | 285 | ||
20 | 112 | 430 | 0.26 | 0.057±0.003 | 0.355±0.018 | 0.045±0.000 6 | 495 | 309 | 284 | ||
21 | 81 | 337 | 0.24 | 0.053±0.002 | 0.331±0.015 | 0.045±0.000 6 | 334 | 290 | 285 | ||
23 | 162 | 1 336 | 0.12 | 0.054±0.002 | 0.337±0.012 | 0.045±0.000 5 | 380 | 295 | 285 | ||
PM012-U-Pb22 (蚀变玄武岩) | 1 | 387 | 361 | 1.07 | 0.048±0.001 | 0.277±0.007 | 0.042±0.000 3 | 102 | 248 | 264 | |
3 | 90 | 139 | 0.65 | 0.055±0.003 | 0.310±0.019 | 0.041±0.000 5 | 395 | 274 | 261 | ||
4 | 96 | 142 | 0.68 | 0.054±0.004 | 0.304±0.020 | 0.041±0.000 5 | 351 | 270 | 260 | ||
6 | 56 | 95 | 0.59 | 0.055±0.003 | 0.316±0.018 | 0.041±0.000 5 | 426 | 279 | 262 | ||
7 | 66 | 116 | 0.57 | 0.046±0.006 | 0.264±0.036 | 0.041±0.001 2 | 17 | 238 | 261 | ||
8 | 95 | 136 | 0.69 | 0.051±0.002 | 0.293±0.013 | 0.042±0.000 4 | 248 | 261 | 263 | ||
10 | 77 | 134 | 0.57 | 0.047±0.003 | 0.271±0.017 | 0.042±0.000 5 | 47 | 243 | 264 | ||
12 | 65 | 120 | 0.54 | 0.050±0.004 | 0.288±0.024 | 0.042±0.000 8 | 196 | 257 | 264 | ||
16 | 33 | 64 | 0.51 | 0.049±0.005 | 0.282±0.027 | 0.042±0.000 8 | 149 | 252 | 263 | ||
18 | 92 | 132 | 0.69 | 0.052±0.004 | 0.298±0.020 | 0.041±0.000 6 | 296 | 265 | 262 |
Table 1 Results of zircon LA-ICP-MS U-Pb dating of volcanic rocks in the Kalaletashi Group
样品号 (岩性) | 点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | 207Pb/ 206Pb | 207Pb/ 235U | 206Pb/ 238U | ||||
3706-U-Pb01 (酸性晶屑 凝灰岩) | 1 | 211 | 382 | 0.55 | 0.047±0.002 | 0.292±0.015 | 0.045±0.000 6 | 47 | 260 | 284 | |
2 | 113 | 151 | 0.74 | 0.052±0.004 | 0.321±0.022 | 0.045±0.000 7 | 264 | 283 | 285 | ||
4 | 91 | 185 | 0.49 | 0.053±0.005 | 0.330±0.030 | 0.045±0.001 0 | 325 | 289 | 285 | ||
6 | 381 | 2 149 | 0.18 | 0.055±0.002 | 0.339±0.010 | 0.045±0.000 4 | 404 | 297 | 283 | ||
8 | 286 | 689 | 0.42 | 0.055±0.002 | 0.341±0.011 | 0.045±0.000 4 | 414 | 298 | 283 | ||
9 | 376 | 889 | 0.42 | 0.055±0.001 | 0.342±0.006 | 0.045±0.000 3 | 416 | 299 | 284 | ||
10 | 222 | 797 | 0.28 | 0.053±0.002 | 0.331±0.009 | 0.045±0.000 4 | 342 | 290 | 284 | ||
11 | 193 | 599 | 0.32 | 0.057±0.002 | 0.352±0.011 | 0.045±0.000 4 | 479 | 306 | 284 | ||
12 | 328 | 714 | 0.46 | 0.054±0.003 | 0.336±0.016 | 0.045±0.000 6 | 360 | 294 | 286 | ||
13 | 146 | 573 | 0.25 | 0.056±0.002 | 0.345±0.013 | 0.045±0.000 5 | 440 | 301 | 284 | ||
14 | 132 | 277 | 0.48 | 0.052±0.003 | 0.322±0.016 | 0.045±0.000 6 | 271 | 283 | 285 | ||
19 | 157 | 711 | 0.22 | 0.055±0.003 | 0.343±0.019 | 0.045±0.000 7 | 415 | 300 | 285 | ||
20 | 112 | 430 | 0.26 | 0.057±0.003 | 0.355±0.018 | 0.045±0.000 6 | 495 | 309 | 284 | ||
21 | 81 | 337 | 0.24 | 0.053±0.002 | 0.331±0.015 | 0.045±0.000 6 | 334 | 290 | 285 | ||
23 | 162 | 1 336 | 0.12 | 0.054±0.002 | 0.337±0.012 | 0.045±0.000 5 | 380 | 295 | 285 | ||
PM012-U-Pb22 (蚀变玄武岩) | 1 | 387 | 361 | 1.07 | 0.048±0.001 | 0.277±0.007 | 0.042±0.000 3 | 102 | 248 | 264 | |
3 | 90 | 139 | 0.65 | 0.055±0.003 | 0.310±0.019 | 0.041±0.000 5 | 395 | 274 | 261 | ||
4 | 96 | 142 | 0.68 | 0.054±0.004 | 0.304±0.020 | 0.041±0.000 5 | 351 | 270 | 260 | ||
6 | 56 | 95 | 0.59 | 0.055±0.003 | 0.316±0.018 | 0.041±0.000 5 | 426 | 279 | 262 | ||
7 | 66 | 116 | 0.57 | 0.046±0.006 | 0.264±0.036 | 0.041±0.001 2 | 17 | 238 | 261 | ||
8 | 95 | 136 | 0.69 | 0.051±0.002 | 0.293±0.013 | 0.042±0.000 4 | 248 | 261 | 263 | ||
10 | 77 | 134 | 0.57 | 0.047±0.003 | 0.271±0.017 | 0.042±0.000 5 | 47 | 243 | 264 | ||
12 | 65 | 120 | 0.54 | 0.050±0.004 | 0.288±0.024 | 0.042±0.000 8 | 196 | 257 | 264 | ||
16 | 33 | 64 | 0.51 | 0.049±0.005 | 0.282±0.027 | 0.042±0.000 8 | 149 | 252 | 263 | ||
18 | 92 | 132 | 0.69 | 0.052±0.004 | 0.298±0.020 | 0.041±0.000 6 | 296 | 265 | 262 |
样品号 | SiO2 | Al2O3 | TFe2O3 | FeO | MgO | CaO | Na2O | K2O | MnO | TiO2 | P2O5 | 烧失量 | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
3706-WXG01 | 66.77 | 13.90 | 2.10 | 1.42 | 1.28 | 4.38 | 3.94 | 1.90 | 0.08 | 0.30 | 0.02 | 5.24 | ||||||||||
3707-WXG01 | 45.64 | 16.16 | 10.68 | 6.78 | 7.33 | 8.69 | 3.34 | 0.56 | 0.24 | 1.40 | 0.09 | 5.78 | ||||||||||
PM012-WXG22 | 51.45 | 15.14 | 12.96 | 6.21 | 3.54 | 3.60 | 6.13 | 0.24 | 0.14 | 2.93 | 0.47 | 3.34 | ||||||||||
#D137/1 | 67.21 | 12.20 | 0.45 | 3.83 | 1.46 | 5.58 | 3.04 | 2.29 | 0.08 | 0.32 | 0.22 | 3.27 | ||||||||||
#D138/3 | 62.75 | 14.73 | 1.00 | 5.69 | 3.44 | 3.94 | 3.05 | 1.96 | 0.26 | 0.64 | 0.20 | 1.95 | ||||||||||
#D140/1 | 39.19 | 16.20 | 8.32 | 1.76 | 2.79 | 15.80 | 2.68 | 11.30 | 0.16 | 1.26 | 0.24 | 11.30 | ||||||||||
#D139/1 | 46.55 | 13.53 | 5.76 | 6.23 | 7.07 | 11.10 | 3.02 | 3.84 | 0.18 | 1.54 | 0.28 | 3.84 | ||||||||||
#D138/1 | 48.87 | 14.92 | 2.74 | 7.51 | 7.54 | 10.10 | 2.71 | 2.72 | 0.28 | 1.30 | 0.22 | 2.72 | ||||||||||
样品号 | 总量 | σ | Mg# | AR | A/CNK | DI | SI | Na2O/K2O | Sc | V | Cr | Co | ||||||||||
3706-WXG01 | 101.33 | 1.43 | 0.41 | 2.52 | 0.84 | 73.59 | 12.08 | 2.07 | 0.35 | 28.20 | 23.20 | 2.52 | ||||||||||
3707-WXG01 | 106.69 | 5.75 | 0.44 | 1.37 | 0.74 | 30.21 | 25.98 | 5.94 | 29.40 | 518.00 | 432.00 | 40.50 | ||||||||||
PM012-WXG22 | 106.15 | 4.79 | 0.26 | 4.79 | 0.90 | 52.09 | 12.39 | 25.94 | 21.70 | 346.00 | 4.67 | 32.50 | ||||||||||
#D137/1 | 99.90 | 1.17 | 0.38 | 1.85 | 0.71 | * | 13.19 | 1.33 | 6.37 | * | 161.10 | 5.10 | ||||||||||
#D138/3 | 99.60 | 1.27 | 0.48 | 1.73 | 1.08 | * | 22.72 | 1.56 | 15.74 | * | 119.50 | 22.74 | ||||||||||
#D140/1 | 100.00 | 4.20 | 0.35 | 1.33 | 0.47 | * | 10.39 | 0.24 | 27.82 | * | 266.60 | 36.50 | ||||||||||
#D139/1 | 99.90 | 4.11 | 0.53 | 1.37 | 0.55 | * | 27.27 | 0.79 | 39.36 | * | 213.30 | 46.07 | ||||||||||
#D138/1 | 99.80 | 2.20 | 0.57 | 1.34 | 0.66 | * | 32.47 | 1.00 | 29.38 | * | 303.60 | 27.48 | ||||||||||
样品号 | Ni | Ba | Hf | Ta | W | Tl | Rb | Sr | Zr | Nb | Th | U | ||||||||||
3706-WXG01 | 10.40 | 436.00 | 4.20 | 0.54 | 0.71 | 0.51 | 63.50 | 210.00 | 87.70 | 5.98 | 7.81 | 2.25 | ||||||||||
3707-WXG01 | 72.10 | 211.00 | 3.39 | 0.15 | 0.45 | 0.11 | 10.70 | 140.00 | 132.00 | 1.58 | 0.37 | 0.17 | ||||||||||
PM012-WXG22 | 6.20 | 118.00 | 12.00 | 1.01 | 0.54 | 0.18 | 4.84 | 55.20 | 517.00 | 10.30 | 3.95 | 1.30 | ||||||||||
#D137/1 | 29.12 | 115.50 | 2.96 | 0.18 | * | * | 103.90 | 202.10 | 84.42 | 15.60 | 9.35 | * | ||||||||||
#D138/3 | 66.38 | 127.90 | 3.30 | 1.01 | * | * | 72.31 | 155.80 | 99.05 | 17.44 | 11.20 | * | ||||||||||
#D140/1 | 118.60 | 37.02 | 2.43 | 0.10 | * | * | 54.76 | 135.70 | 86.92 | 15.21 | 0.95 | * | ||||||||||
#D139/1 | 95.74 | 41.26 | 1.66 | 0.39 | * | * | 24.53 | 257.30 | 42.85 | 15.99 | 2.01 | * | ||||||||||
#D138/1 | 81.55 | 52.99 | 0.86 | 0.31 | * | * | 45.38 | 378.00 | 20.49 | 8.69 | 1.55 | * | ||||||||||
样品号 | Cs | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | ||||||||||
3706-WXG01 | 2.53 | 20.30 | 36.30 | 4.25 | 15.00 | 2.74 | 0.71 | 2.51 | 0.38 | 2.10 | 0.42 | 1.37 | ||||||||||
3707-WXG01 | 0.47 | 3.61 | 9.89 | 1.68 | 8.98 | 3.19 | 1.20 | 3.41 | 0.70 | 5.13 | 1.08 | 3.17 | ||||||||||
PM012-WXG22 | 0.47 | 19.70 | 49.50 | 7.55 | 35.20 | 10.20 | 2.76 | 9.62 | 2.00 | 12.40 | 2.54 | 7.47 | ||||||||||
#D137/1 | * | 40.98 | 79.18 | 8.29 | 29.45 | 6.05 | 1.23 | 6.16 | 0.82 | 4.45 | 0.85 | 2.84 | ||||||||||
#D138/3 | * | 43.99 | 92.75 | 10.80 | 46.00 | 8.10 | 1.67 | 8.27 | 1.26 | 7.28 | 1.39 | 4.07 | ||||||||||
#D140/1 | * | 5.96 | 11.64 | 2.65 | 11.70 | 2.88 | 0.98 | 3.40 | 0.68 | 4.59 | 0.97 | 2.91 | ||||||||||
#D139/1 | * | 9.71 | 24.07 | 2.52 | 18.50 | 5.41 | 1.74 | 6.52 | 1.30 | 8.71 | 1.75 | 4.98 | ||||||||||
#D138/1 | * | 8.31 | 18.43 | 4.59 | 21.28 | 4.04 | 1.20 | 4.76 | 0.90 | 6.02 | 1.28 | 3.63 | ||||||||||
样品号 | Tm | Yb | Lu | Y | REE | LREE | HREE | LREE/ HREE | δEu | (La/Sm)N | (La/Yb)N | (Gd/Yb)N | ||||||||||
3706-WXG01 | 0.19 | 1.38 | 0.20 | 12.60 | 87.85 | 79.30 | 8.55 | 9.27 | 0.81 | 4.66 | 9.92 | 1.47 | ||||||||||
3707-WXG01 | 0.46 | 3.07 | 0.44 | 29.70 | 46.01 | 28.55 | 17.46 | 1.64 | 1.11 | 0.71 | 0.79 | 0.90 | ||||||||||
PM012-WXG22 | 1.02 | 7.03 | 1.00 | 69.20 | 167.99 | 124.91 | 43.08 | 2.90 | 0.84 | 1.21 | 1.89 | 1.10 | ||||||||||
#D137/1 | 0.36 | 2.58 | 0.37 | 21.80 | 183.61 | 165.18 | 18.43 | 8.96 | 0.61 | 4.26 | 10.71 | 1.93 | ||||||||||
#D138/3 | 0.58 | 3.71 | 0.53 | 25.60 | 230.40 | 203.31 | 27.09 | 7.50 | 0.62 | 3.42 | 7.99 | 1.80 | ||||||||||
#D140/1 | 0.41 | 2.75 | 0.41 | 20.90 | 51.93 | 35.81 | 16.12 | 2.22 | 0.96 | 1.30 | 1.46 | 1.00 | ||||||||||
#D139/1 | 0.72 | 4.42 | 0.59 | 30.20 | 90.94 | 61.95 | 28.99 | 2.14 | 0.89 | 1.13 | 1.48 | 1.19 | ||||||||||
#D138/1 | 0.52 | 3.19 | 0.41 | 35.90 | 78.56 | 57.85 | 20.71 | 2.79 | 0.84 | 1.29 | 1.76 | 1.20 |
Table 2 Major (%), trace(10-6) and rare earth (10-6) element compositions of volcanic rocks in the Kalaletashi Group
样品号 | SiO2 | Al2O3 | TFe2O3 | FeO | MgO | CaO | Na2O | K2O | MnO | TiO2 | P2O5 | 烧失量 | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
3706-WXG01 | 66.77 | 13.90 | 2.10 | 1.42 | 1.28 | 4.38 | 3.94 | 1.90 | 0.08 | 0.30 | 0.02 | 5.24 | ||||||||||
3707-WXG01 | 45.64 | 16.16 | 10.68 | 6.78 | 7.33 | 8.69 | 3.34 | 0.56 | 0.24 | 1.40 | 0.09 | 5.78 | ||||||||||
PM012-WXG22 | 51.45 | 15.14 | 12.96 | 6.21 | 3.54 | 3.60 | 6.13 | 0.24 | 0.14 | 2.93 | 0.47 | 3.34 | ||||||||||
#D137/1 | 67.21 | 12.20 | 0.45 | 3.83 | 1.46 | 5.58 | 3.04 | 2.29 | 0.08 | 0.32 | 0.22 | 3.27 | ||||||||||
#D138/3 | 62.75 | 14.73 | 1.00 | 5.69 | 3.44 | 3.94 | 3.05 | 1.96 | 0.26 | 0.64 | 0.20 | 1.95 | ||||||||||
#D140/1 | 39.19 | 16.20 | 8.32 | 1.76 | 2.79 | 15.80 | 2.68 | 11.30 | 0.16 | 1.26 | 0.24 | 11.30 | ||||||||||
#D139/1 | 46.55 | 13.53 | 5.76 | 6.23 | 7.07 | 11.10 | 3.02 | 3.84 | 0.18 | 1.54 | 0.28 | 3.84 | ||||||||||
#D138/1 | 48.87 | 14.92 | 2.74 | 7.51 | 7.54 | 10.10 | 2.71 | 2.72 | 0.28 | 1.30 | 0.22 | 2.72 | ||||||||||
样品号 | 总量 | σ | Mg# | AR | A/CNK | DI | SI | Na2O/K2O | Sc | V | Cr | Co | ||||||||||
3706-WXG01 | 101.33 | 1.43 | 0.41 | 2.52 | 0.84 | 73.59 | 12.08 | 2.07 | 0.35 | 28.20 | 23.20 | 2.52 | ||||||||||
3707-WXG01 | 106.69 | 5.75 | 0.44 | 1.37 | 0.74 | 30.21 | 25.98 | 5.94 | 29.40 | 518.00 | 432.00 | 40.50 | ||||||||||
PM012-WXG22 | 106.15 | 4.79 | 0.26 | 4.79 | 0.90 | 52.09 | 12.39 | 25.94 | 21.70 | 346.00 | 4.67 | 32.50 | ||||||||||
#D137/1 | 99.90 | 1.17 | 0.38 | 1.85 | 0.71 | * | 13.19 | 1.33 | 6.37 | * | 161.10 | 5.10 | ||||||||||
#D138/3 | 99.60 | 1.27 | 0.48 | 1.73 | 1.08 | * | 22.72 | 1.56 | 15.74 | * | 119.50 | 22.74 | ||||||||||
#D140/1 | 100.00 | 4.20 | 0.35 | 1.33 | 0.47 | * | 10.39 | 0.24 | 27.82 | * | 266.60 | 36.50 | ||||||||||
#D139/1 | 99.90 | 4.11 | 0.53 | 1.37 | 0.55 | * | 27.27 | 0.79 | 39.36 | * | 213.30 | 46.07 | ||||||||||
#D138/1 | 99.80 | 2.20 | 0.57 | 1.34 | 0.66 | * | 32.47 | 1.00 | 29.38 | * | 303.60 | 27.48 | ||||||||||
样品号 | Ni | Ba | Hf | Ta | W | Tl | Rb | Sr | Zr | Nb | Th | U | ||||||||||
3706-WXG01 | 10.40 | 436.00 | 4.20 | 0.54 | 0.71 | 0.51 | 63.50 | 210.00 | 87.70 | 5.98 | 7.81 | 2.25 | ||||||||||
3707-WXG01 | 72.10 | 211.00 | 3.39 | 0.15 | 0.45 | 0.11 | 10.70 | 140.00 | 132.00 | 1.58 | 0.37 | 0.17 | ||||||||||
PM012-WXG22 | 6.20 | 118.00 | 12.00 | 1.01 | 0.54 | 0.18 | 4.84 | 55.20 | 517.00 | 10.30 | 3.95 | 1.30 | ||||||||||
#D137/1 | 29.12 | 115.50 | 2.96 | 0.18 | * | * | 103.90 | 202.10 | 84.42 | 15.60 | 9.35 | * | ||||||||||
#D138/3 | 66.38 | 127.90 | 3.30 | 1.01 | * | * | 72.31 | 155.80 | 99.05 | 17.44 | 11.20 | * | ||||||||||
#D140/1 | 118.60 | 37.02 | 2.43 | 0.10 | * | * | 54.76 | 135.70 | 86.92 | 15.21 | 0.95 | * | ||||||||||
#D139/1 | 95.74 | 41.26 | 1.66 | 0.39 | * | * | 24.53 | 257.30 | 42.85 | 15.99 | 2.01 | * | ||||||||||
#D138/1 | 81.55 | 52.99 | 0.86 | 0.31 | * | * | 45.38 | 378.00 | 20.49 | 8.69 | 1.55 | * | ||||||||||
样品号 | Cs | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | ||||||||||
3706-WXG01 | 2.53 | 20.30 | 36.30 | 4.25 | 15.00 | 2.74 | 0.71 | 2.51 | 0.38 | 2.10 | 0.42 | 1.37 | ||||||||||
3707-WXG01 | 0.47 | 3.61 | 9.89 | 1.68 | 8.98 | 3.19 | 1.20 | 3.41 | 0.70 | 5.13 | 1.08 | 3.17 | ||||||||||
PM012-WXG22 | 0.47 | 19.70 | 49.50 | 7.55 | 35.20 | 10.20 | 2.76 | 9.62 | 2.00 | 12.40 | 2.54 | 7.47 | ||||||||||
#D137/1 | * | 40.98 | 79.18 | 8.29 | 29.45 | 6.05 | 1.23 | 6.16 | 0.82 | 4.45 | 0.85 | 2.84 | ||||||||||
#D138/3 | * | 43.99 | 92.75 | 10.80 | 46.00 | 8.10 | 1.67 | 8.27 | 1.26 | 7.28 | 1.39 | 4.07 | ||||||||||
#D140/1 | * | 5.96 | 11.64 | 2.65 | 11.70 | 2.88 | 0.98 | 3.40 | 0.68 | 4.59 | 0.97 | 2.91 | ||||||||||
#D139/1 | * | 9.71 | 24.07 | 2.52 | 18.50 | 5.41 | 1.74 | 6.52 | 1.30 | 8.71 | 1.75 | 4.98 | ||||||||||
#D138/1 | * | 8.31 | 18.43 | 4.59 | 21.28 | 4.04 | 1.20 | 4.76 | 0.90 | 6.02 | 1.28 | 3.63 | ||||||||||
样品号 | Tm | Yb | Lu | Y | REE | LREE | HREE | LREE/ HREE | δEu | (La/Sm)N | (La/Yb)N | (Gd/Yb)N | ||||||||||
3706-WXG01 | 0.19 | 1.38 | 0.20 | 12.60 | 87.85 | 79.30 | 8.55 | 9.27 | 0.81 | 4.66 | 9.92 | 1.47 | ||||||||||
3707-WXG01 | 0.46 | 3.07 | 0.44 | 29.70 | 46.01 | 28.55 | 17.46 | 1.64 | 1.11 | 0.71 | 0.79 | 0.90 | ||||||||||
PM012-WXG22 | 1.02 | 7.03 | 1.00 | 69.20 | 167.99 | 124.91 | 43.08 | 2.90 | 0.84 | 1.21 | 1.89 | 1.10 | ||||||||||
#D137/1 | 0.36 | 2.58 | 0.37 | 21.80 | 183.61 | 165.18 | 18.43 | 8.96 | 0.61 | 4.26 | 10.71 | 1.93 | ||||||||||
#D138/3 | 0.58 | 3.71 | 0.53 | 25.60 | 230.40 | 203.31 | 27.09 | 7.50 | 0.62 | 3.42 | 7.99 | 1.80 | ||||||||||
#D140/1 | 0.41 | 2.75 | 0.41 | 20.90 | 51.93 | 35.81 | 16.12 | 2.22 | 0.96 | 1.30 | 1.46 | 1.00 | ||||||||||
#D139/1 | 0.72 | 4.42 | 0.59 | 30.20 | 90.94 | 61.95 | 28.99 | 2.14 | 0.89 | 1.13 | 1.48 | 1.19 | ||||||||||
#D138/1 | 0.52 | 3.19 | 0.41 | 35.90 | 78.56 | 57.85 | 20.71 | 2.79 | 0.84 | 1.29 | 1.76 | 1.20 |
Fig. 6 Chondrite-normalized REE patterns (a) and MORB-normalized trace element spidergram (b) of volcanic rocks in the Kalaletashi Group (data of D137/1, D138/3, D140/1, D139/1 and D138/1 from reference [5])
样号 | 点号 | 176Lu/177Hf±1σ | 176Yb/177Hf±1σ | 176Hf/177Hf±1σ | Hfi | εHf(t)±1σ | tDM/Ga | tDM2/Ga | t/Ma |
---|---|---|---|---|---|---|---|---|---|
PM012- U-Pb22 | 1 | 0.005 700±0.000 144 | 0.186 482±0.003 267 | 0.282 859±0.000 042 | 0.282 635 | 0.97±0.46 | 0.87 | 1.23 | 264 |
3 | 0.002 616±0.000 061 | 0.084 061±0.002 997 | 0.282 850±0.000 040 | 0.282 699 | 3.14±0.47 | 0.77 | 1.09 | 261 | |
4 | 0.003 366±0.000 121 | 0.108 388±0.003 162 | 0.282 965±0.000 038 | 0.282 699 | 3.14±0.47 | 0.77 | 1.09 | 260 | |
6 | 0.003 393±0.000 028 | 0.114 835±0.001 699 | 0.282 877±0.000 040 | 0.282 466 | -5.07±0.41 | 1.10 | 1.61 | 262 | |
7 | 0.003 356±0.000 100 | 0.111 448±0.002 593 | 0.282 894±0.000 047 | 0.282 671 | 2.16±0.46 | 0.82 | 1.15 | 261 | |
10 | 0.003 859±0.000 057 | 0.132 344±0.003 999 | 0.282 895±0.000 044 | 0.282 748 | 4.95±0.49 | 0.71 | 0.98 | 264 | |
12 | 0.001 437±0.000 037 | 0.047 473±0.001 025 | 0.282 911±0.000 019 | 0.282 708 | 3.54±0.43 | 0.76 | 1.07 | 264 | |
16 | 0.001 011±0.000 031 | 0.034 068±0.001 153 | 0.282 936±0.000 019 | 0.282 604 | -0.15±0.50 | 0.91 | 1.30 | 263 | |
18 | 0.004 979±0.000 081 | 0.155 917±0.002 541 | 0.282 728±0.000 104 | 0.282 686 | 2.72±0.51 | 0.80 | 1.12 | 262 | |
3706- U-Pb01 | 1 | 0.001 204±0.000 007 | 0.038 580±0.000 396 | 0.282 641±0.000 013 | 0.282 633 | 1.33±0.56 | 0.87 | 1.22 | 284 |
2 | 0.000 620±0.000 023 | 0.018 640±0.000 629 | 0.282 702±0.000 014 | 0.282 669 | 2.60±0.61 | 0.83 | 1.14 | 285 | |
4 | 0.000 433±0.000 006 | 0.013 031±0.000 227 | 0.282 701±0.000 013 | 0.282 622 | 0.94±0.63 | 0.88 | 1.25 | 285 | |
6 | 0.000 696±0.000 005 | 0.021 798±0.000 112 | 0.282 469±0.000 012 | 0.282 644 | 1.69±0.61 | 0.86 | 1.20 | 283 | |
8 | 0.002 774±0.000 070 | 0.092 411±0.001 171 | 0.282 940±0.000 029 | 0.282 377 | -7.76±0.59 | 1.23 | 1.80 | 283 | |
9 | 0.001 133±0.000 036 | 0.034 207±0.001 102 | 0.282 677±0.000 013 | 0.282 829 | 8.26±1.46 | 0.64 | 0.78 | 284 | |
10 | 0.001 494±0.000 051 | 0.041 647±0.001 687 | 0.282 755±0.000 014 | 0.282 836 | 8.49±1.41 | 0.60 | 0.77 | 284 | |
11 | 0.000 922±0.000 023 | 0.026 243±0.000 537 | 0.282 713±0.000 012 | 0.282 947 | 12.45±1.33 | 0.43 | 0.51 | 284 | |
12 | 0.001 084±0.000 040 | 0.032 054±0.001 004 | 0.282 610±0.000 014 | 0.282 859 | 9.36±1.42 | 0.57 | 0.71 | 286 | |
13 | 0.001 007±0.000 019 | 0.030 552±0.000 495 | 0.282 691±0.000 015 | 0.282 877 | 9.94±1.66 | 0.54 | 0.67 | 284 | |
14 | 0.000 838±0.000 027 | 0.026 433±0.000 877 | 0.282 638±0.000 016 | 0.282 925 | 11.67±1.03 | 0.46 | 0.56 | 285 | |
19 | 0.001 658±0.000 032 | 0.048 565±0.000 763 | 0.282 677±0.000 017 | 0.282 875 | 9.89±1.54 | 0.55 | 0.68 | 285 | |
20 | 0.000 873±0.000 019 | 0.025 403±0.000 414 | 0.282 626±0.000 018 | 0.282 903 | 10.88±0.66 | 0.49 | 0.61 | 284 | |
21 | 0.001 080±0.000 014 | 0.032 663±0.000 554 | 0.282 650±0.000 017 | 0.282 931 | 11.88±0.65 | 0.45 | 0.55 | 285 | |
23 | 0.000 861±0.000 054 | 0.025 701±0.002 011 | 0.282 381±0.000 017 | 0.282 702 | 3.78±3.63 | 0.83 | 1.07 | 285 |
Table 3 In-situ zircon Lu-Hf isotope compositions of volcanic rocks in the Kalaletashi Group
样号 | 点号 | 176Lu/177Hf±1σ | 176Yb/177Hf±1σ | 176Hf/177Hf±1σ | Hfi | εHf(t)±1σ | tDM/Ga | tDM2/Ga | t/Ma |
---|---|---|---|---|---|---|---|---|---|
PM012- U-Pb22 | 1 | 0.005 700±0.000 144 | 0.186 482±0.003 267 | 0.282 859±0.000 042 | 0.282 635 | 0.97±0.46 | 0.87 | 1.23 | 264 |
3 | 0.002 616±0.000 061 | 0.084 061±0.002 997 | 0.282 850±0.000 040 | 0.282 699 | 3.14±0.47 | 0.77 | 1.09 | 261 | |
4 | 0.003 366±0.000 121 | 0.108 388±0.003 162 | 0.282 965±0.000 038 | 0.282 699 | 3.14±0.47 | 0.77 | 1.09 | 260 | |
6 | 0.003 393±0.000 028 | 0.114 835±0.001 699 | 0.282 877±0.000 040 | 0.282 466 | -5.07±0.41 | 1.10 | 1.61 | 262 | |
7 | 0.003 356±0.000 100 | 0.111 448±0.002 593 | 0.282 894±0.000 047 | 0.282 671 | 2.16±0.46 | 0.82 | 1.15 | 261 | |
10 | 0.003 859±0.000 057 | 0.132 344±0.003 999 | 0.282 895±0.000 044 | 0.282 748 | 4.95±0.49 | 0.71 | 0.98 | 264 | |
12 | 0.001 437±0.000 037 | 0.047 473±0.001 025 | 0.282 911±0.000 019 | 0.282 708 | 3.54±0.43 | 0.76 | 1.07 | 264 | |
16 | 0.001 011±0.000 031 | 0.034 068±0.001 153 | 0.282 936±0.000 019 | 0.282 604 | -0.15±0.50 | 0.91 | 1.30 | 263 | |
18 | 0.004 979±0.000 081 | 0.155 917±0.002 541 | 0.282 728±0.000 104 | 0.282 686 | 2.72±0.51 | 0.80 | 1.12 | 262 | |
3706- U-Pb01 | 1 | 0.001 204±0.000 007 | 0.038 580±0.000 396 | 0.282 641±0.000 013 | 0.282 633 | 1.33±0.56 | 0.87 | 1.22 | 284 |
2 | 0.000 620±0.000 023 | 0.018 640±0.000 629 | 0.282 702±0.000 014 | 0.282 669 | 2.60±0.61 | 0.83 | 1.14 | 285 | |
4 | 0.000 433±0.000 006 | 0.013 031±0.000 227 | 0.282 701±0.000 013 | 0.282 622 | 0.94±0.63 | 0.88 | 1.25 | 285 | |
6 | 0.000 696±0.000 005 | 0.021 798±0.000 112 | 0.282 469±0.000 012 | 0.282 644 | 1.69±0.61 | 0.86 | 1.20 | 283 | |
8 | 0.002 774±0.000 070 | 0.092 411±0.001 171 | 0.282 940±0.000 029 | 0.282 377 | -7.76±0.59 | 1.23 | 1.80 | 283 | |
9 | 0.001 133±0.000 036 | 0.034 207±0.001 102 | 0.282 677±0.000 013 | 0.282 829 | 8.26±1.46 | 0.64 | 0.78 | 284 | |
10 | 0.001 494±0.000 051 | 0.041 647±0.001 687 | 0.282 755±0.000 014 | 0.282 836 | 8.49±1.41 | 0.60 | 0.77 | 284 | |
11 | 0.000 922±0.000 023 | 0.026 243±0.000 537 | 0.282 713±0.000 012 | 0.282 947 | 12.45±1.33 | 0.43 | 0.51 | 284 | |
12 | 0.001 084±0.000 040 | 0.032 054±0.001 004 | 0.282 610±0.000 014 | 0.282 859 | 9.36±1.42 | 0.57 | 0.71 | 286 | |
13 | 0.001 007±0.000 019 | 0.030 552±0.000 495 | 0.282 691±0.000 015 | 0.282 877 | 9.94±1.66 | 0.54 | 0.67 | 284 | |
14 | 0.000 838±0.000 027 | 0.026 433±0.000 877 | 0.282 638±0.000 016 | 0.282 925 | 11.67±1.03 | 0.46 | 0.56 | 285 | |
19 | 0.001 658±0.000 032 | 0.048 565±0.000 763 | 0.282 677±0.000 017 | 0.282 875 | 9.89±1.54 | 0.55 | 0.68 | 285 | |
20 | 0.000 873±0.000 019 | 0.025 403±0.000 414 | 0.282 626±0.000 018 | 0.282 903 | 10.88±0.66 | 0.49 | 0.61 | 284 | |
21 | 0.001 080±0.000 014 | 0.032 663±0.000 554 | 0.282 650±0.000 017 | 0.282 931 | 11.88±0.65 | 0.45 | 0.55 | 285 | |
23 | 0.000 861±0.000 054 | 0.025 701±0.002 011 | 0.282 381±0.000 017 | 0.282 702 | 3.78±3.63 | 0.83 | 1.07 | 285 |
Fig.8 Th-Ta-Hf/3 (a) and Ta/Yb-Th/Yb (b) discrimination diagrams of volcanic rocks in the Kalaletashi Group (data of D137/1, D138/3, D140/1, D139/1 and D138/1 from reference [5])
[1] | 潘裕生. 西昆仑山构造特征与演化[J]. 地质科学, 1990, 25(3): 224-232. |
[2] | 毕华, 王中刚, 王元龙, 等. 西昆仑造山带构造-岩浆演化史[J]. 中国科学(D辑), 1999, 29(5): 398-406. |
[3] | 李荣社, 计文化, 杨永成, 等. 昆仑山及邻区地质[M]. 北京: 地质出版社, 2008: 1-400. |
[4] | 姜春发, 姜春发, 冯秉贵, 等. 昆仑开合构造[M]. 北京: 地质出版社, 1992: 200-227. |
[5] | 韩芳林, 崔建堂, 计文化, 等. 1∶250000伯力克幅(I44C001003)区域地质调查报告[M]. 武汉: 中国地质大学出版社, 2013: 1-181. |
[6] | 计文化, 韩芳林, 王炬川, 等. 西昆仑于田南部苏巴什蛇绿混杂岩的组成、地球化学特征及地质意义[J]. 地质通报, 2004, 23(12): 1196-1201. |
[7] | 温志刚, 胡成林, 王洪强, 等. 新疆西昆仑苏巴什蛇绿岩形成时代及其构造意义[J]. 西北地质, 2019, 52(4): 14-27. |
[8] | 李兴振, 尹福光. 东昆仑与西昆仑地质构造对比研究之刍议[J]. 地质通报, 2002, 21(11): 777-783. |
[9] | 杨万志, 张维洲, 屈迅. 西昆仑山东段库牙克断裂与康西瓦断裂、阿尔金断裂关系的地球化学证据[J]. 地质通报, 2005, 24(4): 316-321. |
[10] | 李博秦. 从地层角度探讨西昆仑麻扎—康西瓦—苏巴什结合带的演化过程[D]. 北京: 中国地质科学院, 2007: 1-155. |
[11] | 蒋幸福, 彭松柏, KUSKY T, 等. 江南造山带东段赣东北蛇绿岩的形成时代:来自辉长岩LA-ICP-MS锆石U-Pb年龄的证据[J]. 现代地质, 2017, 31(4): 697-704. |
[12] | 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. |
[13] | 彭陆, 李全忠, 柴发达, 等. 单颗粒锆石小束斑LA-ICP-MS原位微区U-Pb年龄的测定[J]. 合肥工业大学学报(自然科学版), 2017, 40(1): 110-116. |
[14] |
WU F Y, YANG Y H, XIE L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology[J]. Chemical Geology, 2006, 234(1/2): 105-126.
DOI URL |
[15] |
BLICHERT-TOFT J, ALBARÈDE F. The Lu-Hf isotopic 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 |
[16] |
GRIFFIN W L, PEARSON N J, BELOUSOVA E, et al. The Hf isotope composition of cratonic mantle: LA-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1): 133-147.
DOI URL |
[17] |
LIANG Q, JING H, GREGOIRE D C. Determination of trace elements in granites by inductively coupled plasma mass spectrometry[J]. Talanta, 2000, 51(3): 507-513.
DOI URL |
[18] | WILSON M. Igneous Petrogenesis[M]. London: Unwin Hyman, 1989: 1-466. |
[19] | 王振, 叶培盛, 张绪教, 等. 藏北果芒错蛇绿岩中堆晶岩地球化学特征及其地质意义[J]. 现代地质, 2017, 31(3): 486-497. |
[20] |
BEA F, ARZAMASTSEV A, MONTERO P, et al. Anomalous alkaline rocks of Soustov, Kola: Evidence of mantle-derived metasomatic fluids affecting crustal materials[J]. Contributions to Mineralogy and Petrology, 2001, 140(5): 554-566.
DOI URL |
[21] | 周金城, 蒋少涌, 王孝磊, 等. 华南中侏罗世玄武岩的岩石地球化学研究——以福建藩坑玄武岩为例[J]. 中国科学(D辑), 2005, 35(10): 927-936. |
[22] |
WOOD D A. The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province[J]. Earth and Planetary Science Letters, 1980, 50(1): 11-30.
DOI URL |
[23] | PEARCE J A. Role of sub-continental lithosphere in magma genesis at destructive plate margins[M]//HAWKESWORTH C J, NORRY M J. Continental Basalts and Mantle Xenoliths. Nantwich: Shiva Publications, 1983: 230-249. |
[24] | 莫宣学, 邓晋福. 西藏—“三江”地区几对蛇绿岩-弧岩浆岩带的构造意义[M]// IGCP第321项中国工作组.亚洲的增生. 北京: 地震出版社, 1993: 61-64. |
[25] | 邓晋福, 莫宣学, 魏启荣, 等. 蛇绿混杂岩-俯冲岩浆弧的成对性及火山岩石构造组合推导的“三江”地区特提斯演化模型[M]//中国西部特提斯构造演化及成矿作用学术讨论会文集. 成都: 电子科技大学出版社, 1991: 1. |
[26] | 莫宣学, 邓晋福, 董方浏, 等. 西南三江造山带火山岩—构造组合及其意义[J]. 高校地质学报, 2001, 7(2): 121-138. |
[27] | 刘银, 李荣社, 计文化, 等. 金沙江缝合带西段蛇绿岩与弧火山岩成对性关系——来自地球化学和LA-ICP-MS锆石U-Pb年龄证据[J]. 地质通报, 2014, 33(7): 1076-1088. |
[28] | 李博秦, 计文化, 边小卫, 王峰, 李伟. 西昆仑麻扎构造混杂岩的组成及其地质意义[J]. 现代地质, 2007, 21(1): 78-86. |
[29] | 赖绍聪, 刘池阳. 青藏高原安多岛弧型蛇绿岩地球化学及成因[J]. 岩石学报, 2003, 19(4): 675-682. |
[30] | 侯广顺, 杨贺杰. 俯冲带环境下的火成岩岩石组合及其意义[J]. 科技信息, 2009(18): 21, 23. |
[31] | 李善平, 潘彤, 李永祥, 等. 青藏高原北羌塘盆地多彩地区蛇绿岩地球化学特征及构造环境[J]. 中国地质, 2010, 37(6): 1592-1606. |
[32] | 刘银. 当江—多彩俯冲型蛇绿岩及其岩浆弧特征——多彩蛇绿混杂岩构造环境及就位过程[D]. 北京: 中国地质大学(北京), 2011: 1-85. |
[33] | 魏博. 东昆仑中构造带(东段)蛇绿岩与岛弧型侵入岩地质特征及构造属性研究[D]. 西安: 长安大学, 2015: 1-141. |
Viewed | ||||||
Full text |
|
|||||
Abstract |
|
|||||