地学前缘 ›› 2023, Vol. 30 ›› Issue (4): 283-298.DOI: 10.13745/j.esf.sf.2023.2.41
王涛(), 李积清*(
), 韩杰, 王泰山, 李玉龙, 袁博武
收稿日期:
2022-05-23
修回日期:
2023-02-24
出版日期:
2023-07-25
发布日期:
2023-07-07
通信作者:
*李积清(1985—) ,男,高级工程师,主要从事矿产勘查及区域成矿规律研究工作。E⁃mail: lijiqing8999@163.com
作者简介:
王 涛(1977-),男,高级工程师,主要从事矿产勘查及区域成矿规律研究工作。E-mail: qhddywt@sina.com
基金资助:
WANG Tao(), LI Jiqing*(
), HAN Jie, WANG Taishan, LI Yulong, YUAN Bowu
Received:
2022-05-23
Revised:
2023-02-24
Online:
2023-07-25
Published:
2023-07-07
摘要:
东昆仑中段大格勒地区稀有和稀土矿化碱性杂岩体的发现,打开了东昆仑稀有、稀土矿找矿突破口。本次含稀土矿化石英正长岩的发现,进一步拓展了该区稀土矿找矿空间,对该区战略性矿产找矿工作和科学研究具有重要意义。本文对大水沟东地区石英正长岩的年代学、地球化学和Hf同位素研究,揭示了稀土矿化石英正长岩岩石成因、岩浆源区和构造背景。获得岩石锆石U-Pb年龄为(400.2±3.7) Ma,属早泥盆世;岩石属于准铝质碱性系列,具有高SiO2(64.11%~66.20%)、富Al2O3(15.98%~16.19%)、富碱(Na2O+K2O)含量(11.31%~11.85%),尤其富钾K2O(7.24%~8.18%),低Ti2O(0.38%~0.44%)、CaO(1.13%~1.86%)、MgO(0.13%~0.22%)特征。A/CNK值为0.9~0.98,富集Rb、K、Ba、Th等大离子亲石元素,亏损Nb、Ta、Ti、P等高场强元素,10000Ga/Al值为2.84~3.4,Zr含量为(751.30~1 034.85)×10-6,(Zr+Nb+Ce+Y)含量为(881.49~1 210.16)×10-6,锆石饱和温度为905.76~931.41 ℃,高的Y/Nb值(1.87~2.45)和构造图解指示,石英正长岩为A2型花岗岩,结合区域构造岩浆演化资料表明其形成于碰撞后伸展环境。锆石εHf(t)值为-0.76~1.41,二阶段(tDM2)Hf模式年龄为1 435~1 303 Ma,表明稀土矿化石英正长岩来源于幔源高温玄武质岩浆底侵中元古代长英质地壳部分熔融的产物。
中图分类号:
王涛, 李积清, 韩杰, 王泰山, 李玉龙, 袁博武. 东昆仑大水沟东地区稀土矿化石英正长岩地球化学、年代学及Hf同位素特征[J]. 地学前缘, 2023, 30(4): 283-298.
WANG Tao, LI Jiqing, HAN Jie, WANG Taishan, LI Yulong, YUAN Bowu. Geochemistry, geochronology and Hf isotopic characteristics of rare earth-bearing quartz syenite in eastern Dashuigou, East Kunlun[J]. Earth Science Frontiers, 2023, 30(4): 283-298.
图1 东昆仑造山带地质简图 (据文献[9]修改) 1-下-中元古界;2-寒武系-奥陶系;3-志留系;4-泥盆系;5-石炭系;6-石炭系-二叠系;7-三叠系;8-侏罗系;9-寒武纪-奥陶纪花岗岩;10-志留纪-泥盆纪花岗岩;11-二叠纪-三叠纪花岗岩;12-镁铁-超镁铁质岩;13-区域性断裂及编号;14-一般断裂;15-研究区;16-湖泊;17-河流。
Fig.1 Geological sketch map of the East Kunlun orogenic belt. Modified after [9].
图2 大水沟东地区地质简图(a)和碱性杂岩体放大示意图(b) 1-第四系;2-中元古界小庙岩组;3-金水口岩群;4-早泥盆世二长花岗岩;5-早泥盆世正长岩;6-早泥盆世花岗闪长岩;7-早泥盆世石英正长岩;8-早泥盆世角闪正长岩;9-志留纪闪长岩;10-中寒武世花岗闪长岩;11-新元古代英云闪长岩;12-碱性杂岩;13-花岗岩脉;14-辉长岩脉;15-火成碳酸岩脉;16-辉石岩脉;17-实测断层及编号;18-铌矿体及编号;19-稀土矿化体及编号;20-探槽及编号;21-品位厚度;22-采样位置。
Fig.2 (a) Geological sketch map of eastern Dashuigou and (b) enlargement of the outlined alkaline complex
分析点号 | 元素含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||
DX-01 | 193.3 | 353.3 | 0.55 | 0.525 96 | 0.016 37 | 0.062 39 | 0.000 69 | 429.1 | 10.9 | 390.1 | 4.2 |
DX-02 | 134.5 | 278.5 | 0.48 | 0.518 58 | 0.015 03 | 0.064 66 | 0.000 73 | 424.2 | 10.1 | 403.9 | 4.4 |
DX-03 | 156.4 | 307.5 | 0.51 | 0.503 77 | 0.030 67 | 0.063 41 | 0.000 70 | 414.2 | 20.7 | 396.3 | 4.2 |
DX-04 | 105.2 | 232.1 | 0.45 | 0.503 20 | 0.015 80 | 0.064 62 | 0.000 79 | 413.9 | 10.7 | 403.7 | 4.8 |
DX-05 | 103.4 | 172.1 | 0.60 | 0.476 07 | 0.018 62 | 0.066 05 | 0.000 87 | 395.4 | 12.8 | 412.3 | 5.2 |
DX-06 | 134.7 | 268.5 | 0.50 | 0.527 69 | 0.015 84 | 0.064 58 | 0.000 67 | 430.3 | 10.5 | 403.4 | 4.1 |
DX-07 | 168.1 | 346.5 | 0.49 | 0.549 48 | 0.014 71 | 0.065 29 | 0.000 76 | 444.7 | 9.6 | 407.7 | 4.6 |
DX-08 | 170.4 | 271.5 | 0.63 | 0.469 83 | 0.013 70 | 0.064 46 | 0.000 67 | 391.1 | 9.5 | 402.7 | 4.1 |
DX-09 | 98.8 | 240.6 | 0.41 | 0.487 59 | 0.016 03 | 0.065 35 | 0.000 83 | 403.3 | 10.9 | 408.1 | 5.0 |
DX-10 | 110.0 | 230.0 | 0.48 | 0.505 32 | 0.016 26 | 0.064 08 | 0.000 68 | 415.3 | 11.0 | 400.4 | 4.1 |
DX-11 | 110.4 | 257.0 | 0.43 | 0.470 54 | 0.013 91 | 0.063 05 | 0.000 69 | 391.6 | 9.6 | 394.1 | 4.2 |
DX-12 | 145.1 | 269.1 | 0.54 | 0.469 28 | 0.029 03 | 0.063 05 | 0.000 69 | 390.7 | 20.1 | 394.1 | 4.2 |
DX-13 | 290.0 | 477.1 | 0.61 | 0.458 51 | 0.012 40 | 0.061 24 | 0.000 65 | 383.2 | 8.6 | 383.2 | 4.0 |
DX-14 | 45.9 | 66.1 | 0.69 | 0.525 12 | 0.024 58 | 0.063 54 | 0.001 93 | 428.6 | 16.4 | 397.1 | 11.7 |
DX-15 | 27.7 | 41.1 | 0.67 | 0.459 99 | 0.028 34 | 0.062 37 | 0.001 17 | 384.2 | 19.7 | 390.0 | 7.1 |
DX-16 | 137.30 | 305.10 | 0.45 | 0.511 68 | 0.018 42 | 0.063 14 | 0.000 84 | 419.6 | 12.4 | 394.7 | 5.1 |
DX-17 | 52.00 | 154.90 | 0.34 | 0.512 35 | 0.020 75 | 0.065 76 | 0.000 92 | 420.0 | 13.9 | 410.6 | 5.6 |
DX-18 | 118.50 | 220.70 | 0.54 | 0.492 03 | 0.015 32 | 0.063 45 | 0.000 73 | 406.3 | 10.4 | 396.6 | 4.4 |
DX-19 | 221.40 | 376.00 | 0.59 | 0.520 00 | 0.010 00 | 0.070 00 | 0.000 00 | 427.0 | 8.8 | 409.2 | 4.3 |
DX-20 | 125.86 | 268.42 | 0.47 | 0.510 00 | 0.010 00 | 0.070 00 | 0.000 00 | 418.7 | 10.0 | 408.2 | 4.8 |
DX-21 | 20.22 | 33.58 | 0.60 | 0.470 00 | 0.030 00 | 0.070 00 | 0.000 00 | 394.3 | 20.8 | 410.9 | 7.9 |
表1 大水沟东地区石英正长岩LA-ICP-MS锆石U-Pb定年数据
Table 1 LA-ICP-MS zircon U-Pb dating data
分析点号 | 元素含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/235U | 1σ | 206Pb/238U | 1σ | 207Pb/235U | 1σ | 206Pb/238U | 1σ | ||
DX-01 | 193.3 | 353.3 | 0.55 | 0.525 96 | 0.016 37 | 0.062 39 | 0.000 69 | 429.1 | 10.9 | 390.1 | 4.2 |
DX-02 | 134.5 | 278.5 | 0.48 | 0.518 58 | 0.015 03 | 0.064 66 | 0.000 73 | 424.2 | 10.1 | 403.9 | 4.4 |
DX-03 | 156.4 | 307.5 | 0.51 | 0.503 77 | 0.030 67 | 0.063 41 | 0.000 70 | 414.2 | 20.7 | 396.3 | 4.2 |
DX-04 | 105.2 | 232.1 | 0.45 | 0.503 20 | 0.015 80 | 0.064 62 | 0.000 79 | 413.9 | 10.7 | 403.7 | 4.8 |
DX-05 | 103.4 | 172.1 | 0.60 | 0.476 07 | 0.018 62 | 0.066 05 | 0.000 87 | 395.4 | 12.8 | 412.3 | 5.2 |
DX-06 | 134.7 | 268.5 | 0.50 | 0.527 69 | 0.015 84 | 0.064 58 | 0.000 67 | 430.3 | 10.5 | 403.4 | 4.1 |
DX-07 | 168.1 | 346.5 | 0.49 | 0.549 48 | 0.014 71 | 0.065 29 | 0.000 76 | 444.7 | 9.6 | 407.7 | 4.6 |
DX-08 | 170.4 | 271.5 | 0.63 | 0.469 83 | 0.013 70 | 0.064 46 | 0.000 67 | 391.1 | 9.5 | 402.7 | 4.1 |
DX-09 | 98.8 | 240.6 | 0.41 | 0.487 59 | 0.016 03 | 0.065 35 | 0.000 83 | 403.3 | 10.9 | 408.1 | 5.0 |
DX-10 | 110.0 | 230.0 | 0.48 | 0.505 32 | 0.016 26 | 0.064 08 | 0.000 68 | 415.3 | 11.0 | 400.4 | 4.1 |
DX-11 | 110.4 | 257.0 | 0.43 | 0.470 54 | 0.013 91 | 0.063 05 | 0.000 69 | 391.6 | 9.6 | 394.1 | 4.2 |
DX-12 | 145.1 | 269.1 | 0.54 | 0.469 28 | 0.029 03 | 0.063 05 | 0.000 69 | 390.7 | 20.1 | 394.1 | 4.2 |
DX-13 | 290.0 | 477.1 | 0.61 | 0.458 51 | 0.012 40 | 0.061 24 | 0.000 65 | 383.2 | 8.6 | 383.2 | 4.0 |
DX-14 | 45.9 | 66.1 | 0.69 | 0.525 12 | 0.024 58 | 0.063 54 | 0.001 93 | 428.6 | 16.4 | 397.1 | 11.7 |
DX-15 | 27.7 | 41.1 | 0.67 | 0.459 99 | 0.028 34 | 0.062 37 | 0.001 17 | 384.2 | 19.7 | 390.0 | 7.1 |
DX-16 | 137.30 | 305.10 | 0.45 | 0.511 68 | 0.018 42 | 0.063 14 | 0.000 84 | 419.6 | 12.4 | 394.7 | 5.1 |
DX-17 | 52.00 | 154.90 | 0.34 | 0.512 35 | 0.020 75 | 0.065 76 | 0.000 92 | 420.0 | 13.9 | 410.6 | 5.6 |
DX-18 | 118.50 | 220.70 | 0.54 | 0.492 03 | 0.015 32 | 0.063 45 | 0.000 73 | 406.3 | 10.4 | 396.6 | 4.4 |
DX-19 | 221.40 | 376.00 | 0.59 | 0.520 00 | 0.010 00 | 0.070 00 | 0.000 00 | 427.0 | 8.8 | 409.2 | 4.3 |
DX-20 | 125.86 | 268.42 | 0.47 | 0.510 00 | 0.010 00 | 0.070 00 | 0.000 00 | 418.7 | 10.0 | 408.2 | 4.8 |
DX-21 | 20.22 | 33.58 | 0.60 | 0.470 00 | 0.030 00 | 0.070 00 | 0.000 00 | 394.3 | 20.8 | 410.9 | 7.9 |
图5 大水沟东石英正长岩LA-ICP-MS锆石U-Pb年龄谐和图(a)和加权平均值图(b)
Fig.5 U-Pb concordia diagram (a) and histogram of zircon U-Pb ages to obtain weighted mean age (b) for quartz syenite
样品号 | wB/% | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | |
DX-1 | 65.64 | 0.39 | 16.19 | 1.41 | 1.93 | 0.06 | 0.16 | 1.49 | 3.74 | 8.00 | 0.07 | 0.54 | 99.62 |
DX-2 | 65.53 | 0.42 | 16.12 | 1.22 | 2.25 | 0.06 | 0.18 | 1.49 | 3.67 | 8.18 | 0.07 | 0.47 | 99.66 |
DX-3 | 66.20 | 0.38 | 16.12 | 1.93 | 1.78 | 0.06 | 0.13 | 1.13 | 4.07 | 7.24 | 0.04 | 0.54 | 99.62 |
DX-4 | 64.11 | 0.51 | 15.98 | 1.49 | 2.90 | 0.07 | 0.22 | 1.86 | 3.67 | 7.89 | 0.08 | 0.56 | 99.34 |
DX-5 | 65.23 | 0.44 | 16.10 | 1.32 | 2.33 | 0.06 | 0.17 | 1.49 | 3.66 | 8.14 | 0.07 | 0.53 | 99.54 |
样品号 | wB/10-6 | ||||||||||||
Li | Be | B | V | Cr | Co | Ni | Cu | Zn | Ga | Rb | Sr | Zr | |
DX-1 | 17.20 | 1.22 | 11.38 | 4.57 | 1.73 | 0.71 | 0.91 | 3.96 | 78.79 | 24.32 | 180.25 | 55.85 | 751.30 |
DX-2 | 14.38 | 1.05 | 11.03 | 4.97 | 1.86 | 0.75 | 1.07 | 3.47 | 83.49 | 24.47 | 185.53 | 55.48 | 846.16 |
DX-3 | 11.94 | 1.42 | 13.37 | 4.59 | 1.76 | 0.99 | 0.94 | 3.99 | 107.83 | 28.99 | 153.43 | 53.79 | 813.36 |
DX-4 | 12.11 | 1.30 | 10.72 | 6.27 | 2.22 | 0.96 | 1.10 | 4.19 | 102.21 | 24.01 | 176.99 | 53.08 | 1 034.85 |
DX-5 | 10.90 | 1.25 | 12.16 | 4.98 | 1.83 | 0.79 | 0.98 | 3.65 | 87.24 | 24.50 | 186.20 | 53.56 | 895.26 |
样品号 | wB/10-6 | ||||||||||||
Nb | Sn | Cs | Ba | Hf | Ta | W | Tl | Pb | Bi | Th | U | La | |
DX-1 | 19.49 | 4.00 | 5.95 | 699.41 | 14.18 | 0.86 | 0.69 | 1.18 | 25.18 | 0.08 | 6.23 | 1.00 | 33.20 |
DX-2 | 21.82 | 4.03 | 6.05 | 646.50 | 16.49 | 0.95 | 0.71 | 1.16 | 25.22 | 0.09 | 5.37 | 1.13 | 30.50 |
DX-3 | 22.88 | 2.36 | 3.66 | 346.29 | 17.17 | 1.07 | 0.92 | 1.05 | 25.57 | 0.06 | 22.09 | 2.53 | 146.00 |
DX-4 | 25.34 | 4.56 | 5.57 | 628.40 | 20.33 | 1.17 | 0.73 | 1.12 | 24.37 | 0.29 | 8.60 | 1.32 | 44.20 |
DX-5 | 22.78 | 3.88 | 5.92 | 587.87 | 17.25 | 1.04 | 0.78 | 1.22 | 25.57 | 0.11 | 4.99 | 1.14 | 27.80 |
样品号 | wB/10-6 | ||||||||||||
Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | |
DX-1 | 73.60 | 9.85 | 44.90 | 9.89 | 1.36 | 9.14 | 1.36 | 7.47 | 1.43 | 4.01 | 0.61 | 4.30 | 0.76 |
DX-2 | 67.80 | 9.32 | 43.70 | 10.40 | 1.31 | 9.53 | 1.46 | 8.07 | 1.57 | 4.37 | 0.66 | 4.69 | 0.87 |
DX-3 | 300.00 | 36.30 | 143.00 | 22.60 | 1.00 | 16.60 | 2.33 | 11.80 | 2.26 | 6.30 | 0.89 | 6.04 | 1.02 |
DX-4 | 99.70 | 13.50 | 60.80 | 13.50 | 1.25 | 12.70 | 1.81 | 10.20 | 2.01 | 5.53 | 0.82 | 5.93 | 1.08 |
DX-5 | 65.20 | 9.11 | 43.10 | 10.30 | 1.29 | 10.10 | 1.54 | 8.49 | 1.69 | 4.59 | 0.70 | 4.90 | 0.88 |
样品号 | wB/10-6 | LREE/ HREE | LaN/ YbN | δEu | δCe | 104Ga/Al | A/NK | A/CNK | σ | ||||
Y | Sc | ∑REE | LREE | HREE | |||||||||
DX-1 | 37.09 | 6.07 | 201.93 | 172.86 | 29.08 | 5.94 | 5.54 | 0.43 | 0.99 | 2.84 | 1.09 | 0.93 | 6.05 |
DX-2 | 39.86 | 6.55 | 194.18 | 162.96 | 31.21 | 5.22 | 4.66 | 0.39 | 0.98 | 2.87 | 1.08 | 0.92 | 6.20 |
DX-3 | 56.04 | 3.61 | 695.24 | 648.01 | 47.23 | 13.72 | 17.33 | 0.15 | 0.98 | 3.40 | 1.11 | 0.98 | 5.48 |
DX-4 | 50.30 | 8.65 | 272.89 | 232.87 | 40.02 | 5.82 | 5.34 | 0.29 | 0.99 | 2.84 | 1.10 | 0.90 | 6.27 |
DX-5 | 42.59 | 6.82 | 189.60 | 156.73 | 32.87 | 4.77 | 4.06 | 0.38 | 1.00 | 2.87 | 1.09 | 0.92 | 6.21 |
样品号 | R1 | R2 | Mg# | TFeO | Rb/Sr | Rb/Nb | Zr/Hf | Nb/Ta | Y/Nb | Zr/Nb | Ce/Pb | Nd/Th | Tzr/℃ |
DX-1 | 1 138.00 | 492.00 | 0.05 | 3.23 | 3.23 | 9.25 | 52.98 | 22.66 | 1.90 | 38.55 | 2.92 | 7.21 | 905.76 |
DX-2 | 1 115.00 | 491.00 | 0.05 | 3.38 | 3.34 | 8.50 | 51.31 | 22.97 | 1.83 | 38.78 | 2.69 | 8.14 | 916.73 |
DX-3 | 1 223.00 | 449.00 | 0.03 | 3.54 | 2.85 | 6.71 | 47.37 | 21.38 | 2.45 | 35.55 | 11.73 | 6.47 | 923.83 |
DX-4 | 1 082.00 | 532.00 | 0.05 | 4.29 | 3.33 | 6.98 | 50.90 | 21.66 | 1.99 | 40.84 | 4.09 | 7.07 | 931.41 |
DX-5 | 1 109.00 | 490.00 | 0.05 | 3.55 | 3.48 | 8.17 | 51.90 | 21.90 | 1.87 | 39.30 | 2.55 | 8.64 | 923.07 |
表2 大水沟东地区石英正长岩(样品DX)主量(%)、微量(10-6)及稀土元素分析数据
Table 2 Analysis data of major (%), trace (10-6) and rare earth elements of quartz syenite (sample DX) in Dashuigou east area
样品号 | wB/% | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | |
DX-1 | 65.64 | 0.39 | 16.19 | 1.41 | 1.93 | 0.06 | 0.16 | 1.49 | 3.74 | 8.00 | 0.07 | 0.54 | 99.62 |
DX-2 | 65.53 | 0.42 | 16.12 | 1.22 | 2.25 | 0.06 | 0.18 | 1.49 | 3.67 | 8.18 | 0.07 | 0.47 | 99.66 |
DX-3 | 66.20 | 0.38 | 16.12 | 1.93 | 1.78 | 0.06 | 0.13 | 1.13 | 4.07 | 7.24 | 0.04 | 0.54 | 99.62 |
DX-4 | 64.11 | 0.51 | 15.98 | 1.49 | 2.90 | 0.07 | 0.22 | 1.86 | 3.67 | 7.89 | 0.08 | 0.56 | 99.34 |
DX-5 | 65.23 | 0.44 | 16.10 | 1.32 | 2.33 | 0.06 | 0.17 | 1.49 | 3.66 | 8.14 | 0.07 | 0.53 | 99.54 |
样品号 | wB/10-6 | ||||||||||||
Li | Be | B | V | Cr | Co | Ni | Cu | Zn | Ga | Rb | Sr | Zr | |
DX-1 | 17.20 | 1.22 | 11.38 | 4.57 | 1.73 | 0.71 | 0.91 | 3.96 | 78.79 | 24.32 | 180.25 | 55.85 | 751.30 |
DX-2 | 14.38 | 1.05 | 11.03 | 4.97 | 1.86 | 0.75 | 1.07 | 3.47 | 83.49 | 24.47 | 185.53 | 55.48 | 846.16 |
DX-3 | 11.94 | 1.42 | 13.37 | 4.59 | 1.76 | 0.99 | 0.94 | 3.99 | 107.83 | 28.99 | 153.43 | 53.79 | 813.36 |
DX-4 | 12.11 | 1.30 | 10.72 | 6.27 | 2.22 | 0.96 | 1.10 | 4.19 | 102.21 | 24.01 | 176.99 | 53.08 | 1 034.85 |
DX-5 | 10.90 | 1.25 | 12.16 | 4.98 | 1.83 | 0.79 | 0.98 | 3.65 | 87.24 | 24.50 | 186.20 | 53.56 | 895.26 |
样品号 | wB/10-6 | ||||||||||||
Nb | Sn | Cs | Ba | Hf | Ta | W | Tl | Pb | Bi | Th | U | La | |
DX-1 | 19.49 | 4.00 | 5.95 | 699.41 | 14.18 | 0.86 | 0.69 | 1.18 | 25.18 | 0.08 | 6.23 | 1.00 | 33.20 |
DX-2 | 21.82 | 4.03 | 6.05 | 646.50 | 16.49 | 0.95 | 0.71 | 1.16 | 25.22 | 0.09 | 5.37 | 1.13 | 30.50 |
DX-3 | 22.88 | 2.36 | 3.66 | 346.29 | 17.17 | 1.07 | 0.92 | 1.05 | 25.57 | 0.06 | 22.09 | 2.53 | 146.00 |
DX-4 | 25.34 | 4.56 | 5.57 | 628.40 | 20.33 | 1.17 | 0.73 | 1.12 | 24.37 | 0.29 | 8.60 | 1.32 | 44.20 |
DX-5 | 22.78 | 3.88 | 5.92 | 587.87 | 17.25 | 1.04 | 0.78 | 1.22 | 25.57 | 0.11 | 4.99 | 1.14 | 27.80 |
样品号 | wB/10-6 | ||||||||||||
Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | |
DX-1 | 73.60 | 9.85 | 44.90 | 9.89 | 1.36 | 9.14 | 1.36 | 7.47 | 1.43 | 4.01 | 0.61 | 4.30 | 0.76 |
DX-2 | 67.80 | 9.32 | 43.70 | 10.40 | 1.31 | 9.53 | 1.46 | 8.07 | 1.57 | 4.37 | 0.66 | 4.69 | 0.87 |
DX-3 | 300.00 | 36.30 | 143.00 | 22.60 | 1.00 | 16.60 | 2.33 | 11.80 | 2.26 | 6.30 | 0.89 | 6.04 | 1.02 |
DX-4 | 99.70 | 13.50 | 60.80 | 13.50 | 1.25 | 12.70 | 1.81 | 10.20 | 2.01 | 5.53 | 0.82 | 5.93 | 1.08 |
DX-5 | 65.20 | 9.11 | 43.10 | 10.30 | 1.29 | 10.10 | 1.54 | 8.49 | 1.69 | 4.59 | 0.70 | 4.90 | 0.88 |
样品号 | wB/10-6 | LREE/ HREE | LaN/ YbN | δEu | δCe | 104Ga/Al | A/NK | A/CNK | σ | ||||
Y | Sc | ∑REE | LREE | HREE | |||||||||
DX-1 | 37.09 | 6.07 | 201.93 | 172.86 | 29.08 | 5.94 | 5.54 | 0.43 | 0.99 | 2.84 | 1.09 | 0.93 | 6.05 |
DX-2 | 39.86 | 6.55 | 194.18 | 162.96 | 31.21 | 5.22 | 4.66 | 0.39 | 0.98 | 2.87 | 1.08 | 0.92 | 6.20 |
DX-3 | 56.04 | 3.61 | 695.24 | 648.01 | 47.23 | 13.72 | 17.33 | 0.15 | 0.98 | 3.40 | 1.11 | 0.98 | 5.48 |
DX-4 | 50.30 | 8.65 | 272.89 | 232.87 | 40.02 | 5.82 | 5.34 | 0.29 | 0.99 | 2.84 | 1.10 | 0.90 | 6.27 |
DX-5 | 42.59 | 6.82 | 189.60 | 156.73 | 32.87 | 4.77 | 4.06 | 0.38 | 1.00 | 2.87 | 1.09 | 0.92 | 6.21 |
样品号 | R1 | R2 | Mg# | TFeO | Rb/Sr | Rb/Nb | Zr/Hf | Nb/Ta | Y/Nb | Zr/Nb | Ce/Pb | Nd/Th | Tzr/℃ |
DX-1 | 1 138.00 | 492.00 | 0.05 | 3.23 | 3.23 | 9.25 | 52.98 | 22.66 | 1.90 | 38.55 | 2.92 | 7.21 | 905.76 |
DX-2 | 1 115.00 | 491.00 | 0.05 | 3.38 | 3.34 | 8.50 | 51.31 | 22.97 | 1.83 | 38.78 | 2.69 | 8.14 | 916.73 |
DX-3 | 1 223.00 | 449.00 | 0.03 | 3.54 | 2.85 | 6.71 | 47.37 | 21.38 | 2.45 | 35.55 | 11.73 | 6.47 | 923.83 |
DX-4 | 1 082.00 | 532.00 | 0.05 | 4.29 | 3.33 | 6.98 | 50.90 | 21.66 | 1.99 | 40.84 | 4.09 | 7.07 | 931.41 |
DX-5 | 1 109.00 | 490.00 | 0.05 | 3.55 | 3.48 | 8.17 | 51.90 | 21.90 | 1.87 | 39.30 | 2.55 | 8.64 | 923.07 |
图6 大水沟东石英正长岩地球化学分类图 a-侵入岩TAS分类图解-底图据文献[20];b-A/CNK-A/NK图解-底图据文献[21];c-AR-SiO2岩浆系列判别图-底图据文献[22],碱度率(AR) =[Al2O3+CaO+(Na2O+K2O)]/[Al2O3+CaO-(Na2O+K2O)];d-SiO2-(K2O+Na2O-CaO)岩浆分类判别图解-底图据文献[23]。
Fig.6 Geochemical classification diagrams for quartz syenite. Basemaps from [20⇓⇓-23].
图7 大水沟东石英正长岩球粒陨石稀土元素配分图(a)和原始地幔微量元素蛛网图(b) (底图据文献[26])
Fig.7 Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element diagram (b) for rock samples. Modified from [26].
样品 | 年龄/Ma | 176Hf/177Hf | 1σ | 176Lu/177Hf | 176Yb/177Hf | εHf(t) | tDM1 | tDM2 | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|
DX-01 | 403.9 | 0.282 540 | 0.000 010 | 0.001 113 | 0.044 294 | 0.41 | 1 009 | 1 368 | -0.97 |
DX-02 | 396.3 | 0.282 539 | 0.000 012 | 0.001 311 | 0.051 702 | 0.17 | 1 016 | 1 379 | -0.96 |
DX-03 | 403.7 | 0.282 536 | 0.000 011 | 0.001 045 | 0.041 787 | 0.26 | 1 013 | 1 376 | -0.97 |
DX-04 | 412.3 | 0.282 533 | 0.000 012 | 0.001 359 | 0.052 788 | 0.28 | 1 025 | 1 382 | -0.96 |
DX-05 | 403.4 | 0.282 523 | 0.000 012 | 0.001 203 | 0.048 519 | -0.27 | 1 036 | 1 409 | -0.96 |
DX-06 | 407.7 | 0.282 534 | 0.000 012 | 0.001 185 | 0.048 016 | 0.25 | 1 019 | 1 380 | -0.96 |
DX-07 | 402.7 | 0.282 573 | 0.000 011 | 0.001 646 | 0.065 856 | 1.41 | 976 | 1 303 | -0.95 |
DX-08 | 408.1 | 0.282 528 | 0.000 011 | 0.001 146 | 0.045 338 | 0.04 | 1 027 | 1 393 | -0.97 |
DX-09 | 400.4 | 0.282 537 | 0.000 011 | 0.000 953 | 0.036 483 | 0.26 | 1 009 | 1 374 | -0.97 |
DX-10 | 394.1 | 0.282 513 | 0.000 010 | 0.001 094 | 0.044 003 | -0.76 | 1 047 | 1 435 | -0.97 |
DX-11 | 394.1 | 0.282 534 | 0.000 011 | 0.000 933 | 0.036 074 | 0.02 | 1 013 | 1 385 | -0.97 |
DX-12 | 383.2 | 0.282 558 | 0.000 011 | 0.002 967 | 0.121 009 | 0.13 | 1 034 | 1 369 | -0.91 |
DX-13 | 390.0 | 0.282 558 | 0.000 011 | 0.000 924 | 0.031 704 | 0.81 | 978 | 1 332 | -0.97 |
DX-14 | 394.7 | 0.282 526 | 0.000 012 | 0.001 793 | 0.074 012 | -0.47 | 1 048 | 1 417 | -0.95 |
DX-15 | 396.6 | 0.282 523 | 0.000 010 | 0.001 048 | 0.041 184 | -0.35 | 1 031 | 1 409 | -0.97 |
表3 大水沟东地区石英正长岩锆石原位Hf同位素数据表
Table 3 Results of in situ zircon Hf isotope analysis
样品 | 年龄/Ma | 176Hf/177Hf | 1σ | 176Lu/177Hf | 176Yb/177Hf | εHf(t) | tDM1 | tDM2 | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|
DX-01 | 403.9 | 0.282 540 | 0.000 010 | 0.001 113 | 0.044 294 | 0.41 | 1 009 | 1 368 | -0.97 |
DX-02 | 396.3 | 0.282 539 | 0.000 012 | 0.001 311 | 0.051 702 | 0.17 | 1 016 | 1 379 | -0.96 |
DX-03 | 403.7 | 0.282 536 | 0.000 011 | 0.001 045 | 0.041 787 | 0.26 | 1 013 | 1 376 | -0.97 |
DX-04 | 412.3 | 0.282 533 | 0.000 012 | 0.001 359 | 0.052 788 | 0.28 | 1 025 | 1 382 | -0.96 |
DX-05 | 403.4 | 0.282 523 | 0.000 012 | 0.001 203 | 0.048 519 | -0.27 | 1 036 | 1 409 | -0.96 |
DX-06 | 407.7 | 0.282 534 | 0.000 012 | 0.001 185 | 0.048 016 | 0.25 | 1 019 | 1 380 | -0.96 |
DX-07 | 402.7 | 0.282 573 | 0.000 011 | 0.001 646 | 0.065 856 | 1.41 | 976 | 1 303 | -0.95 |
DX-08 | 408.1 | 0.282 528 | 0.000 011 | 0.001 146 | 0.045 338 | 0.04 | 1 027 | 1 393 | -0.97 |
DX-09 | 400.4 | 0.282 537 | 0.000 011 | 0.000 953 | 0.036 483 | 0.26 | 1 009 | 1 374 | -0.97 |
DX-10 | 394.1 | 0.282 513 | 0.000 010 | 0.001 094 | 0.044 003 | -0.76 | 1 047 | 1 435 | -0.97 |
DX-11 | 394.1 | 0.282 534 | 0.000 011 | 0.000 933 | 0.036 074 | 0.02 | 1 013 | 1 385 | -0.97 |
DX-12 | 383.2 | 0.282 558 | 0.000 011 | 0.002 967 | 0.121 009 | 0.13 | 1 034 | 1 369 | -0.91 |
DX-13 | 390.0 | 0.282 558 | 0.000 011 | 0.000 924 | 0.031 704 | 0.81 | 978 | 1 332 | -0.97 |
DX-14 | 394.7 | 0.282 526 | 0.000 012 | 0.001 793 | 0.074 012 | -0.47 | 1 048 | 1 417 | -0.95 |
DX-15 | 396.6 | 0.282 523 | 0.000 010 | 0.001 048 | 0.041 184 | -0.35 | 1 031 | 1 409 | -0.97 |
图8 大水沟东石英正长岩A型花岗岩判别图解 a-(Zr+Nb+Ce+Y)-K2O+Na2O)/CaO图解,底图据文献[33];b-(Zr+Nb+Ce+Y)-TFeO/MgO图解,底图据文献[33];c-10000Ga/Al-Ce图解,底图据文献[33];d-10000Ga/Al-Ce图解,底图据文献[33]。
Fig.8 Tectonic discrimination diagrams for quartz syenite
图9 大水沟东石英正长岩锆石Hf同位素176Hf/177Hf-t(Ma)图解(a)和εHf(t)-t(Ma)图解(b) (底图据文献[27])
Fig.9 Zircon 176Hf/177Hf-t (a) and εHf(t)-t (b) diagrams for quartz syenite. Modified from [27].
[1] | 许志琴, 杨经绥, 李文昌, 等. 青藏高原中的古特提斯体制与增生造山作用[J]. 岩石学报, 2013, 29(6): 1847-1860. |
[2] |
HAO L L, WANG Q, WYMAN D A, et al. First identification of postcollisional A-type magmatism in the Himalayan-Tibetan orogen[J]. Geology, 2019, 47(2): 187-190.
DOI URL |
[3] | 马昌前, 熊富浩, 尹烁, 等. 造山带岩浆作用的强度和旋回性: 以东昆仑古特提斯花岗岩类岩基为例[J]. 岩石学报, 2015, 31(12): 3555-3568. |
[4] | 熊富浩, 马昌前, 张金阳, 等. 东昆仑造山带早中生代镁铁质岩墙群LA-ICP-MS锆石U-Pb定年、元素和Sr-Nd-Hf同位素地球化学[J]. 岩石学报, 2011, 27(11): 3350-3364. |
[5] |
李五福, 王涛, 王秉璋, 等. 东昆仑大格勒地区稀有和稀土矿化碱性杂岩体的发现及意义[J/OL]. 大地构造与成矿学, 2022.[2022-2-28]. DOI: 10.16539/j.ddgzyckx.2021.06.010.
DOI |
[6] | 莫宣学, 罗照华, 邓晋福, 等. 东昆仑造山带花岗岩及地壳生长[J]. 高校地质学报, 2007, 13(3): 403-414. |
[7] | 王秉璋, 李积清, 付长垒, 等. 东昆仑布尔汗布达早古生代岩浆弧的形成与演化初探[J]. 地球科学, 2022, 47(4): 1253-1270. |
[8] | 潘桂棠, 肖庆辉, 陆松年, 等. 中国大地构造单元划分[J]. 中国地质, 2009, 36(1): 1-28, 255. |
[9] |
王秉璋, 潘彤, 任海东, 等. 东昆仑祁漫塔格寒武纪岛弧:来自拉陵高里河地区玻安岩型高镁安山岩/闪长岩锆石U-Pb年代学、地球化学和Hf同位素证据[J]. 地学前缘, 2021, 28(1): 318-333.
DOI |
[10] | 刘彬, 马昌前, 郭盼, 等. 东昆仑中泥盆世A型花岗岩的确定及其构造意义[J]. 地球科学:中国地质大学学报, 2013, 38(5): 947-962. |
[11] | 潘彤. 青海成矿单元划分[J]. 地球科学与环境学报, 2017, 39(1): 16-33. |
[12] |
ZONG K Q, KLEMD R, YUAN Y, et al. The assembly of Rodinia: the correlation of early Neoproterozoic (ca. 900 Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB)[J]. Precambrian Research, 2017, 290: 32-48.
DOI URL |
[13] |
HU Z C, ZHANG W, LIU Y S, et al. “wave” signal-smoothing and mercury-removing device for laser ablation quadrupole and multiple collector ICPMS analysis: application to lead isotope analysis[J]. Analytical Chemistry, 2015, 87(2): 1152-1157.
DOI URL |
[14] |
LIU Y S, HU Z C, GAO S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1/2): 34-43.
DOI URL |
[15] |
LIU Y, GAO S, HU Z, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-north China orogen: U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2): 537-571.
DOI URL |
[16] | LUDWIG K R. ISOPLOT 3.00: a geochronological toolkit for Microsoft Excel[J]. Berkeley Geochronology Center, Special Publication, 2003, 39: 91-445. |
[17] |
HU Z C, LIU Y S, GAO S, et al. Improved in situ Hf isotope ratio analysis of zircon using newly designed X skimmer cone and jet sample cone in combination with the addition of nitrogen by laser ablation multiple collector ICP-MS[J]. Journal of Analytical Atomic Spectrometry, 2012, 27(9): 1391.
DOI URL |
[18] | 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16): 1589-1604. |
[19] |
SLÁMA J, KOŠLER J, CONDON D J, et al. Plešovice zircon:a new natural reference material for U-Pb and Hf isotopic microanalysis[J]. Chemical Geology, 2008, 249(1/2): 1-35.
DOI URL |
[20] |
MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4): 215-224.
DOI URL |
[21] |
MANIAR P D, PICCOLI P M. Tectonic discrimination of granitoids[J]. Geological Society of America Bulletin, 1989, 101(5): 635-643.
DOI URL |
[22] |
WRIGHT J B. A simple alkalinity ratio and its application to questions of non-orogenic granite genesis[J]. Geological Magazine, 1969, 106(4): 370-384.
DOI URL |
[23] |
FROST B R, BARNES C G, COLLINS W J, et al. A geochemical classification for granitic rocks[J]. Journal of Petrology, 2001, 42(11): 2033-2048.
DOI URL |
[24] |
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 |
[25] |
陈志刚, 李永胜, 于晓飞, 等. 大兴安岭北段小柯勒河花岗斑岩地球化学、Hf同位素组成及锆石U-Pb定年[J]. 地学前缘, 2021, 28(4): 267-282.
DOI |
[26] |
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 |
[27] | 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. |
[28] |
张晓旭, 苏尚国, 刘美玉, 等. 甘肃金川早古生代正长花岗岩锆石SHRIMP U-Pb年代学、岩石学、地球化学特征及其构造意义[J]. 地学前缘, 2021, 28(4): 283-298.
DOI |
[29] | 陈海福, 何书跃, 张爱奎, 等. 东昆仑卡尔却卡地区中志留世A型花岗岩岩石成因及构造环境[J]. 地质通报, 2021, 40(8): 1380-1393. |
[30] |
SUN J L, QIAN Y, LI J Y, et al. The late paleoproterozoic A-type granites in the Jiao-Liao-Ji Orogenic Belt, North China craton:petrogenesis and implications for post-collision extension[J]. Geochemistry International, 2021, 59(4), 388-412.
DOI |
刘彬, 马昌前, 蒋红安, 等. 东昆仑早古生代洋壳俯冲与碰撞造山作用的转换: 来自胡晓钦镁铁质岩石的证据[J]. 岩石学报, 2013, 29(6): 2093-2106. | |
[31] |
KING P L, WHITE A J R, CHAPPELL B W, et al. Characterization and origin of aluminous A-type granites from the Lachlan fold belt, southeastern Australia[J]. Journal of Petrology, 1997, 38(3): 371-391.
DOI URL |
[32] | LOISELLE M C, WONES D R. Characterization and origin of anorogenic granites[J]. Geological Society of America,Abstracts with Programs, 1979, 11(2): 448-468. |
[33] |
WHALEN J B, CURRIE K L, CHAPPELL B W. A-type granites: geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95(4): 407-419.
DOI URL |
[34] |
COLLINS W J, BEAMS S D, WHITE A J R, et al. Nature and origin of A-type granites with particular reference to southeastern Australia[J]. Contributions to Mineralogy and Petrology, 1982, 80(2): 189-200.
DOI URL |
[35] |
YANG J H, WU F Y, CHUNG S L, et al. A hybrid origin for the Qianshan A-type granite, northeast China: geochemical and Sr-Nd-Hf isotopic evidence[J]. Lithos, 2006, 89(1/2): 89-106.
DOI URL |
[36] |
PATIÑO DOUCE A E. Generation of metaluminous A-type granites by low-pressure melting of calc-alkaline granitoids[J]. Geology, 1997, 25(8): 743.
DOI URL |
[37] |
MINGRAM B, TRUMBULL R B, LITTMAN S, et al. A petrogenetic study of anorogenic felsic magmatism in the Cretaceous Paresis ring complex, Namibia: evidence for mixing of crust and mantle-derived components[J]. Lithos, 2000, 54(1/2): 1-22.
DOI URL |
[38] |
HARRIS C, MARSH J S, MILNER S C. Petrology of the alkaline core of the messum igneous complex, Namibia: evidence for the progressively decreasing effect of crustal contamination[J]. Journal of Petrology, 1999, 40(9): 1377-1397.
DOI URL |
[39] | 张超, 吴新伟, 刘永江, 等. 大兴安岭中段早二叠世A型花岗岩成因及对扎兰屯地区构造演化的制约[J]. 岩石学报, 2020, 36(4): 1091-1106. |
[40] |
CREASER R A, PRICE R C, WORMALD R J. A-type granites revisited: assessment of a residual-source model[J]. Geology, 1991, 19(2): 163.
DOI URL |
[41] | TAYLOR S R, MCLENNAN S M. The continental crust:its composition and evolution. An examination of the geochemical record preserved in sedimentar yrocks[M]. Oxford: Blackwell Scientific Publishing,1985. |
[42] | 李金超, 国显正, 孔会磊, 等. 东昆仑浪麦滩地区A型花岗岩年代学、地球化学特征及其地质意义[J]. 地质学报, 2021, 95(5): 1508-1522. |
[43] |
TURNER S P, FODEN J D, MORRISON R S. Derivation of some A-type magmas by fractionation of basaltic magma: an example from the Padthaway Ridge, South Australia[J]. Lithos, 1992, 28(2): 151-179.
DOI URL |
[44] | 王秉璋, 李五福, 金婷婷, 等. 东昆仑大格勒稀有金属矿化碳酸岩和橄榄岩斜锆石U-Pb年代学研究和找矿意义[J/OL]. 地球科学, 2022: 1-21. (2022-2-09). https://kns.cnki.net/kcms/detail/42.1874.P.20220809.0955.003.html. |
[45] |
EBY G N. Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications[J]. Geology, 1992, 20(7): 641.
DOI URL |
[46] |
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 |
[47] | 陆松年. 青藏高原北部前寒武纪地质初探[M]. 北京: 地质出版社, 2002. |
[48] | 郝梦楠, 熊富浩, 赵涵, 等. 东昆仑丘吉东沟地区泥盆纪花岗岩的成因机制及其对原特提斯造山作用的启示[J]. 矿物岩石, 2021, 41(2): 59-70. |
[49] | 张亮, 李碧乐, 刘磊, 等. 东昆仑五龙沟地区早泥盆世双峰式侵入岩年代学、地球化学及其地质意义[J]. 岩石学报, 2021, 37(7): 2007-2028. |
[50] | 王艺龙, 李艳军, 魏俊浩, 等. 东昆仑五龙沟地区晚志留世A型花岗岩成因: U-Pb年代学、地球化学、Nd及Hf同位素制约[J]. 地球科学, 2018, 43(4): 1219-1236. |
[51] | 郭通珍, 刘荣, 陈发彬, 等. 青海祁漫塔格山乌兰乌珠尔斑状正长花岗岩LA-MC-ICPMS锆石U-Pb定年及地质意义[J]. 地质通报, 2011, 30(8): 1203-1211. |
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