Zircon U-Pb Ages and Its Geological Significance of the Granitic Rocks in the Yichun-Hegang Region, Southeastern Xiao Hinggan Mountains
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摘要: 小兴安岭地区花岗质岩浆的活动期次，对讨论东北地区的构造演化具有重要意义.锆石U-Pb年龄测定结果表明，小兴安岭东南部伊春-鹤岗地区花岗质岩浆活动可分为4期：寒武纪-奥陶纪(508~447 Ma)、中-晚二叠世(266~259 Ma)、早-中三叠世(244~231 Ma)、晚三叠世(222~200 Ma).根据花岗质岩石的Sr、Yb地球化学特征，结合兴蒙造山带东端构造演化历史，认为该区中-晚二叠世花岗质岩石多属于喜马拉雅型花岗岩，可能形成于华北板块与西伯利亚板块碰撞过程中；早-中三叠世花岗岩属于埃达克质岩石，岩浆起源于加厚地壳，形成于两大板块碰撞后的继续挤压造山阶段；晚三叠世花岗质岩石多属浙闽-南岭型花岗岩，与古亚洲洋闭合造山后岩石圈的伸展体制有关.Abstract: The stages of the granitoid in the Xiao Hinggan Mountains is the key to the tectonic evolution of Northeast China. Using zircon U-Pb dating results by laser ablation inductively coupled plasma mass spectrometer (LA-ICP-MS), the granitoids from Yichun-Hegang regional in the east Xiao Hinggan Mountains can be grouped into Cambrian-Ordovician (508-447 Ma), Middle-Late Permian (266-259 Ma), Early-Middle Triassic (244-231 Ma), and Late Triassic (222-200 Ma). Considering the evolution history of Xing'an-Mongolia orogenic belt (XMOB), the granitoids can be divided into different types on the basis of their Sr and Yb contents. The Middle Permian granitoids shows the characteristics of Himalayan-type granite, and was related to collision of North China craton with the Siberian craton. The Early-Middle Triassic granitoids shows the characteristics of Adakite, which originated from the thickened crust. Late Triassic granitoids shows the characteristics of Zhemin-Nanling-type granite. The formations of Triassic granitoids are related to the continued collision and extension after closure of the Paleo-Asian Ocean, respectively.
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Key words:
- granite /
- zircon U-Pb dating /
- Xiao Hinggan Mountains /
- tectonic setting /
- geochemistry
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图 1 研究区地质简图
据黑龙江省地质局区域地质测量队(1971)的1∶20万金山屯幅和黑龙江省地质局第一区测量队(1979)的1∶20万萝北县幅地质图修订
Fig. 1. Sketch geological map of the study area
图 2 研究区花岗质岩石锆石U-Pb年龄谐和图
Fig. 2. Concordia U-Pb plots of zircons from granitoids in study area
图 4 花岗岩类型地球化学判别图解(图a底图据张旗等，2008；图b据Thiéblemont and Tegyey, 1994)
图a中：Ⅰ.埃达克型花岗岩；Ⅱ.喜马拉雅型花岗岩；Ⅲ.广西型花岗岩；Ⅳ.浙闽型花岗岩；Ⅴ.南岭型花岗岩
Fig. 4. Discrimination diagrams for geochemistry
表 1 研究区花岗质岩石锆石LA-ICP-MS U-Pb分析结果
Table 1. LA-ICP-MS zircon U-Pb data of granitoids in study area
样品测点 含量 同位素比值 年龄(Ma) 232Th 238U 232Th/238U 207Pb/206Pb±1σ 207Pb/235U±1σ 206Pb/238U±1σ 207Pb/235U±1σ 206Pb/238U±1σ 1002-1-01 252.76 443.69 0.57 0.053 37±0.001 55 0.302 04±0.008 58 0.041 05±0.000 38 268±7 259±2 1002-1-02 101.99 195.32 0.52 0.052 31±0.002 37 0.297 18±0.013 21 0.041 43±0.000 48 264±10 262±3 1002-1-03 33.39 124.14 0.27 0.061 68±0.003 71 0.355 36±0.020 23 0.042 34±0.000 73 309±15 267±5 1002-1-04 60.71 123.63 0.49 0.052 73±0.002 79 0.297 80±0.015 23 0.041 50±0.000 55 265±12 262±3 1002-1-05 339.88 422.30 0.80 0.053 77±0.001 58 0.308 12±0.008 97 0.041 52±0.000 36 273±7 262±2 1002-1-06 205.16 395.76 0.52 0.050 94±0.001 71 0.289 54±0.009 56 0.041 24±0.000 35 258±8 261±2 1002-1-07 402.27 446.88 0.90 0.053 67±0.001 56 0.300 87±0.008 96 0.040 67±0.000 39 267±7 257±2 1002-1-08 374.29 481.31 0.78 0.056 15±0.001 74 0.319 67±0.009 20 0.041 39±0.000 37 282±7 261±2 1002-1-09 60.83 116.15 0.52 0.057 70±0.003 23 0.322 80±0.017 96 0.041 05±0.000 66 284±14 259±4 1002-1-10 44.65 115.54 0.39 0.055 58±0.003 54 0.322 30±0.019 74 0.042 24±0.000 75 284±15 267±5 1002-1-11 174.70 244.73 0.71 0.056 05±0.002 27 0.313 80±0.012 71 0.040 75±0.000 49 277±10 257±3 1002-1-12 54.34 120.42 0.45 0.053 29±0.002 93 0.303 85±0.016 34 0.041 71±0.000 58 269±13 263±4 1002-1-13 69.72 156.46 0.45 0.053 08±0.002 34 0.300 63±0.012 50 0.041 69±0.000 51 267±10 263±3 1002-1-14 52.58 127.77 0.41 0.062 43±0.004 11 0.359 09±0.022 30 0.042 08±0.000 66 261±19 262±4 1002-1-15 62.03 125.81 0.49 0.052 32±0.004 26 0.292 80±0.023 77 0.040 69±0.000 96 261±19 257±6 1002-1-16 42.57 102.54 0.42 0.054 11±0.003 31 0.296 76±0.018 23 0.040 62±0.000 60 264±14 257±4 1002-1-17 288.63 408.37 0.71 0.052 06±0.001 66 0.292 43±0.009 07 0.040 92±0.000 39 260±7 259±2 1002-1-18 67.93 145.07 0.47 0.054 53±0.002 84 0.311 03±0.016 26 0.041 51±0.000 57 275±13 262±4 1002-1-19 97.46 222.54 0.44 0.054 54±0.003 00 0.298 08±0.015 56 0.040 23±0.000 54 265±12 254±3 1002-1-20 147.76 204.22 0.72 0.053 67±0.003 20 0.295 31±0.016 75 0.040 63±0.000 58 263±13 257±4 P40-1-1 253.28 382.82 0.66 0.052 14±0.001 41 0.236 74±0.005 93 0.032 93±0.000 25 216±5 209±2 P40-1-2 475.73 555.59 0.86 0.051 92±0.001 08 0.232 77±0.004 31 0.032 51±0.000 21 212±4 206±1 P40-1-3 342.07 475.49 0.72 0.050 43±0.001 08 0.228 68±0.004 38 0.032 88±0.000 22 209±4 209±1 P40-1-4 252.31 407.51 0.62 0.051 95±0.001 16 0.237 34±0.004 76 0.033 13±0.000 23 216±4 210±1 P40-1-5 153.85 313.47 0.49 0.051 97±0.001 50 0.233 41±0.006 28 0.032 57±0.000 26 213±5 207±2 P40-1-7 239.80 437.63 0.55 0.051 88±0.001 19 0.235 75±0.004 92 0.032 95±0.000 23 215±4 209±1 P40-1-8 460.37 591.31 0.78 0.049 85±0.000 97 0.228 27±0.003 89 0.033 20±0.000 21 209±3 211±1 P40-1-9 404.23 594.35 0.68 0.052 70±0.001 40 0.234 27±0.005 74 0.032 23±0.000 25 214±5 204±2 P40-1-10 192.92 304.39 0.63 0.051 57±0.001 24 0.234 08±0.005 14 0.032 91±0.000 23 214±4 209±1 P40-1-11 303.36 475.04 0.64 0.050 05±0.001 64 0.228 62±0.007 10 0.033 12±0.000 29 209±6 210±2 P40-1-12 339.55 460.16 0.74 0.049 35±0.001 24 0.229 58±0.005 33 0.033 73±0.000 25 210±4 214±2 P40-1-13 201.08 315.03 0.64 0.048 97±0.001 80 0.226 83±0.007 97 0.033 58±0.000 32 208±7 213±2 P40-1-14 178.47 282.07 0.63 0.048 79±0.001 33 0.226 14±0.005 76 0.033 61±0.000 26 207±5 213±2 P40-1-15 220.31 364.41 0.60 0.050 01±0.001 21 0.227 23±0.005 04 0.032 95±0.000 24 208±4 209±1 P40-1-16 1 694.19 1 226.15 1.38 0.050 70±0.000 78 0.230 30±0.002 90 0.032 94±0.000 19 210±2 209±1 P40-1-17 331.03 504.26 0.66 0.049 46±0.001 00 0.224 49±0.004 03 0.032 92±0.000 22 206±3 209±1 P40-1-18 183.40 289.10 0.63 0.051 16±0.001 43 0.234 32±0.006 15 0.033 21±0.000 26 214±5 211±2 P40-1-19 275.19 514.77 0.53 0.050 19±0.001 05 0.232 28±0.004 39 0.033 56±0.000 23 212±4 213±1 P40-1-20 239.41 410.44 0.58 0.049 86±0.001 07 0.225 35±0.004 39 0.032 78±0.000 22 206±4 208±1 
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表 2 研究区花岗质岩石年龄测定结果
Table 2. Zircon U-Pb data of granitoids in study area
样品号 采样位置 岩性 表面年龄(Ma) 加权平均年龄(Ma) 1002-1 47°22.548′N、130°03.872′E 片麻状细粒角闪黑云母石英闪长岩 254~263 260±1 P6-3 47°22.060′N、130°04.000′E 中细粒黑云母二长花岗岩 257~264 261±1 1009-1 47°34.875′N、129°47.293′E 似斑状中细粒黑云母二长花岗岩 256~266 261±1 1006-1 47°23.964′N、129°54.369′E 似斑状细粒黑云母二长花岗岩 253~265 262±2 1007-1 47°24.941′N、129°43.466′E 似斑状中细粒黑云母二长花岗岩 255~268 264±1 P18-9 47°24.512′N、129°49.172′E 片麻状似斑状中细粒角闪黑云母二长花岗岩 256~265 260±1 P10-2 47°22.842′N、129°59.455′E 细粒黑云母花岗闪长岩 240~251 244±2 P10-1 47°22.842′N、129°59.455′E 似斑状中细粒黑云母花岗闪长岩 228~239 234±2 P24-4 47°24.883′N、129°40.958′E 花岗斑岩 205~217 210±2 P31-4 47°20.902′N、129°36.360′E 中粗粒黑云母二长花岗岩 208~215 211±1 1015-1 47°29.157′N、129°17.941′E 似斑状中粗粒黑云母二长花岗岩 204~217 212±2 P40-1 47°35.453′N、129°14.385′E 中粗粒黑云母角闪石英二长岩 204~214 209±1
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