Zircon U-Pb Chronology of Volcanic Rocks in the Hailaer Basin, NE China and Its Geological Implications
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摘要: 海拉尔盆地位于大兴安岭西侧，盆内存在多套火山-沉积岩组合.通过对海拉尔盆地Chu8井等4处火山岩样品进行的锆石LA-ICP-MS U-Pb年代学研究，探讨了海拉尔盆地火山岩的形成时代和构造背景，为盆内和邻区地层对比以及大兴安岭地区构造演化提供了依据.研究区4个火山岩样品的锆石均呈自形-半自形晶，显示出典型的岩浆生长环带，结合其高的Th/U比值(0.22~1.50)，说明其属于岩浆成因.测年结果表明，海拉尔盆地布达特群确实存在时代为晚三叠世-早侏罗世(214.4±4.3 Ma)的火山岩，结合前人研究，可将盆内火山作用划分为4期：分别为中-晚石炭世基底岩浆岩(320~290 Ma)；晚三叠世-早侏罗世早期布特达特群火山碎屑岩组(224~197 Ma)；晚侏罗世-早白垩世早期塔木兰沟组(152~138 Ma)；早白垩世晚期铜钵庙组(128~117 Ma).大兴安岭地区各期岩浆作用的地球化学特征、时空分布特征以及盆地地震剖面特征表明，中-晚石炭世基底岩浆岩(320~290 Ma)是额尔古纳-兴安地块和松嫩地块碰撞造山后的伸展背景下形成的；晚三叠世-早侏罗世早期火山岩(224~197 Ma)是古亚洲洋闭合后的伸展背景下形成的，该期火山岩的发现说明古亚洲洋构造域对大兴安岭地区的影响至少延续到早侏罗世早期(197 Ma)，而该区域蒙古-鄂霍茨克洋的俯冲碰撞最早可能开始于早侏罗世以后；晚侏罗世-早白垩世早期(152~138 Ma)和早白垩世晚期(128~117 Ma)火山岩的形成均与蒙古-鄂霍茨克洋碰撞闭合后的伸展作用有关.盆内部分火山岩样品中存在古元古代-新元古代捕获的锆石，这表明额尔古纳地块和兴安地块很可能存在着元古代结晶基底.Abstract: The Hailaer basin is located in the west of the Great Xing'an Range, and there are many sets of volcanic sedimentary rocks in the basin. Determining the age of the formation of volcanic rocks can provide reliable evidence for the stratigraphic correlation of the basin and the Great Xing'an Range, and the tectonic evolution in Northeast China as well. LA-ICP-MS zircon U-Pb dating for 4 volcanic rock samples from coring well in the Hailaer basin (HB) is presented in this paper. Their formation time and tectonic setting focusing on the intra-/inter-basinal stratigraphic correlation are discussed. The dating results show that volcanic rocks with ages of Late Triassic-early Early Jurassic (214.4±4.3 Ma) do exist in the HB. And the whole volcanic succession in the region can be subdivided into 4 stages of eruption including Middle-Late Carboniferous (320-290 Ma), Late Triassic-early Early Jurassic (224-197 Ma), Late Jurassic-early Early Cretaceous (152-138 Ma), and late Early Cretaceous (128-117 Ma). Combined with geochemical characteristics, temporal and spatial distribution characteristics of the magma in the Great Xing'an Range area, as well as the characteristics of the seismic profile of the basin, it is suggested that the Middle-Late Carboniferous magmatic rocks (320-290 Ma) were probably formed in a post-collision extensional setting related to the collision and merging of the Songnen and Ergun-Xing'an blocks. The Late Triassic-early Early Jurassic volcanic rocks (224-197 Ma) were probably formed in a post-collision extensional setting related to the closure of Paleo-Asian Ocean, which indicates Paleo-Asian Ocean tectonic domain affects the Great Xing'an Range area extended to the early Early Jurassic at least and the collision of the Mongolia Okhotsk Ocean possibly started in the early Jurassic at the earliest. The Late Jurassic-early Early Cretaceous (152-138 Ma) and the Late Early Cretaceous (128-117 Ma) volcanic rocks were probably formed in a post-collision extensional setting related to the closure of Mongolia Okhotsk Ocean. Some ages of Paleoproterozoic-Neoproterozoic zircon dating are obtained, which might have been captured from some crystal rocks of Proterozoic crystalline basement in the blocks underneath the HB.
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Key words:
- chronology /
- Hailaer basin /
- volcanic rocks /
- Xing'anling Group /
- Budate Group /
- tectonic evolution /
- petrology
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图 1 海拉尔盆地构造分区及取样钻井位置
国境线据中国地质图(1:5 000 000)，地质出版社，2002年第二版；据李萍萍等(2010)
Fig. 1. Sketch showing subdivision of Hailar basin and drilling sites
图 2 海拉尔盆地地层序列柱状图(a)和取样井岩性柱状图(b)
图a据万传彪(2006)
Fig. 2. Column showing stratigraphic sequence of Hailaer basin (a) and lithologic features of drilling samples (b)
图 3 海拉尔盆地火山岩的部分锆石阴极发光照片
Fig. 3. Cathodoluminescence images of representative zircons from volcanic rocks in Hailar basin
图 4 海拉尔盆地火山岩的锆石U-Pb谐和图
Fig. 4. Concordia plots of zircons from volcanic rocks in Hailar basin
图 5 海拉尔盆地火山岩单颗粒锆石U-Pb测年数据分布(n=1 141)(a)，及其对应火山岩样品年龄分布(n=50)(b)
部分年龄数据据李萍萍等(2010)、赵磊等(2013)、Meng et al.(2013)和Li et al.(2014)
Fig. 5. Histograms for the single zircon ages (n=1 141) (a) and corresponding volcanic rocks ages (n=50) (b) in Hailar basin
表 1 海拉尔盆地火山岩锆石LA-ICP-MS U-Pb分析结果
Table 1. LA-ICP-MS zircon U-Pb analytical data for volcanic rocks from Hailar basin
样品号 Th(10-6) U(10-6) Pb(10-6) Th/U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 年龄(Ma) 207Pb/206U 1σ 207Pb/235U 1σ 206Pb/238U 1σ C8-1 822 895 106 0.92 0.049 4 0.002 9 0.155 6 0.008 7 0.023 3 0.000 4 165 132 147.0 7.7 148.0 2.4 C8-2 633 840 85 0.75 0.053 4 0.003 0 0.171 9 0.009 8 0.023 4 0.000 3 346 131 161.0 8.5 149.0 2.1 C8-3 547 716 84 0.76 0.052 4 0.003 1 0.165 4 0.009 2 0.023 2 0.000 4 306 135 155.0 8.0 148.0 2.3 C8-4 503 594 75 0.85 0.051 2 0.003 4 0.158 8 0.010 4 0.023 3 0.000 4 250 147 150.0 9.1 148.0 2.6 C8-5 763 898 106 0.85 0.049 5 0.002 9 0.158 5 0.009 4 0.023 3 0.000 4 172 136 149.0 8.2 149.0 2.2 C8-6 1 072 1 162 132 0.92 0.050 6 0.002 3 0.163 3 0.007 5 0.023 4 0.000 3 220 107 154.0 6.6 149.0 1.8 C8-7 634 808 97 0.78 0.053 6 0.003 2 0.169 6 0.010 1 0.023 3 0.000 3 354 135 159.0 8.7 149.0 2.1 C8-8 1 380 981 194 1.41 0.050 5 0.002 4 0.182 6 0.008 1 0.026 5 0.000 4 300 131 154.0 8.1 147.0 2.2 C8-9 642 749 81 0.86 0.052 1 0.003 0 0.163 8 0.009 3 0.023 1 0.000 3 502 122 172.0 9.0 148.0 2.1 C8-10 553 742 80 0.75 0.057 3 0.003 2 0.184 6 0.010 5 0.023 3 0.000 3 169 159 149.0 9.7 149.0 2.3 C8-11 475 668 67 0.71 0.049 4 0.003 6 0.157 5 0.011 1 0.023 3 0.000 4 298 184 149.0 10.0 148.0 2.6 C8-12 441 524 67 0.84 0.052 3 0.004 1 0.157 5 0.011 4 0.023 3 0.000 4 167 156 146.0 9.3 149.0 2.6 C8-13 373 527 53 0.71 0.049 2 0.003 5 0.154 1 0.010 6 0.023 3 0.000 4 165 110 148.0 6.6 148.0 1.9 C8-14 1 320 968 143 1.36 0.049 4 0.002 4 0.157 2 0.007 5 0.023 2 0.000 3 409 126 164.0 8.3 149.0 2.0 C8-15 632 801 83 0.79 0.055 0 0.003 1 0.175 5 0.009 6 0.023 3 0.000 3 189 122 147.0 7.0 146.0 1.8 C8-16 790 858 103 0.92 0.049 7 0.002 6 0.155 8 0.007 9 0.022 9 0.000 3 309 141 149.0 8.2 142.0 1.9 C8-17 1 113 741 129 1.50 0.052 5 0.003 2 0.158 2 0.009 3 0.022 3 0.000 3 154 119 148.0 7.2 148.0 2.0 C8-18 833 1 017 108 0.82 0.049 1 0.002 6 0.157 0 0.008 2 0.023 3 0.000 3 572 152 172.0 11.5 146.0 2.4 C8-19 481 584 68 0.82 0.059 1 0.004 1 0.184 5 0.013 4 0.022 9 0.000 4 167 113 149.0 6.6 148.0 2.0 C8-20 1 278 1 089 151 1.17 0.049 2 0.002 4 0.157 6 0.007 5 0.023 3 0.000 3 298 122 158.0 7.6 149.0 2.1 C8-21 821 904 96 0.91 0.052 3 0.002 8 0.168 0 0.008 8 0.023 3 0.000 3 209 130 151.0 7.3 149.0 1.9 C8-22 1 031 1 148 127 0.90 0.050 3 0.002 8 0.160 3 0.008 4 0.023 3 0.000 3 302 107 159.0 6.6 150.0 2.2 C8-23 1 094 1 117 131 0.98 0.052 4 0.002 4 0.169 5 0.007 6 0.023 5 0.000 3 191 134 150.0 7.4 148.0 2.4 C8-24 639 777 88 0.82 0.049 9 0.002 8 0.158 8 0.008 5 0.023 3 0.000 4 333 97 160.0 8.1 153.0 2.1 C8-25 717 878 93 0.82 0.051 7 0.002 9 0.170 3 0.009 4 0.024 1 0.000 3 300 218 220.0 18.1 223.0 5.0 C5-1 90 11 63 0.69 0.052 2 0.004 9 0.242 0 0.022 1 0.035 2 0.000 8 295 292 227.0 21.5 225.0 4.4 C5-2 70 13 51 0.73 0.052 2 0.005 9 0.250 0 0.026 5 0.035 5 0.000 7 345 223 225.0 19.0 224.0 3.8 C5-3 85 15 69 0.82 0.053 2 0.005 3 0.248 4 0.023 4 0.035 4 0.000 6 328 211 231.0 19.2 220.0 4.0 C5-4 73 12 70 0.97 0.053 0 0.004 9 0.255 6 0.023 8 0.034 8 0.000 6 350 253 214.0 20.7 212.0 3.9 C5-5 70 12 69 0.98 0.053 5 0.005 8 0.234 7 0.025 2 0.033 5 0.000 6 309 272 231.0 21.7 232.0 5.1 C5-6 58 14 57 0.98 0.052 6 0.005 6 0.255 9 0.026 8 0.036 6 0.000 8 572 263 236.0 23.2 222.0 4.8 C5-7 58 8 45 0.78 0.059 1 0.007 1 0.261 4 0.028 8 0.035 1 0.000 8 354 183 217.0 15.6 206.0 3.2 C5-8 102 27 148 1.45 0.053 6 0.004 3 0.238 3 0.019 0 0.032 6 0.000 5 391 263 226.0 22.9 214.0 4.4 C5-9 66 10 44 0.67 0.054 5 0.006 3 0.248 7 0.028 1 0.033 8 0.000 7 420 368 224.0 32.6 216.0 4.6 C5-10 50 12 39 0.78 0.055 2 0.008 9 0.246 5 0.040 0 0.034 1 0.000 7 520 325 224.0 25.6 222.0 5.2 C5-11 51 9 47 0.91 0.057 8 0.008 6 0.246 3 0.031 4 0.035 0 0.000 8 524 271 219.0 23.2 206.0 5.1 C5-12 59 11 52 0.87 0.057 9 0.007 2 0.240 1 0.028 3 0.032 4 0.000 8 276 252 213.0 23.4 210.0 4.4 C5-13 63 13 70 1.12 0.051 8 0.006 2 0.233 6 0.028 4 0.033 2 0.000 7 354 258 207.0 22.8 201.0 4.2 C5-14 65 10 61 0.94 0.053 6 0.006 2 0.225 9 0.027 5 0.031 6 0.000 7 457 249 210.0 20.1 204.0 4.2 C5-15 79 25 138 1.74 0.056 2 0.006 3 0.229 7 0.024 4 0.032 2 0.000 7 461 265 213.0 21.0 204.0 4.5 C5-16 61 12 54 0.88 0.056 2 0.006 7 0.233 6 0.025 5 0.032 2 0.000 7 361 311 226.0 24.6 221.0 5.4 C5-17 53 12 53 1.00 0.053 8 0.007 3 0.249 5 0.030 3 0.034 9 0.000 9 254 222 219.0 20.2 211.0 4.5 C5-18 66 17 84 1.27 0.051 3 0.005 3 0.240 5 0.024 6 0.033 2 0.000 7 365 56 247.0 5.3 235.0 2.1 B2-1 2 962 479 1 943 0.66 0.053 8 0.001 3 0.275 8 0.006 7 0.037 1 0.000 3 2 390 26 2 269.0 15.9 2 120.0 16.7 B2-2 665 774 432 0.65 0.154 0 0.002 4 8.339 8 0.145 5 0.389 4 0.003 6 524 46 515.0 8.7 510.0 4.5 B2-3 1 997 275 432 0.22 0.057 8 0.001 2 0.660 5 0.014 3 0.082 3 0.000 7 2 478 31 2 485.0 18.7 2 489.0 23.5 B2-4 1 238 1 609 557 0.45 0.161 1 0.002 9 10.558 8 0.212 2 0.471 3 0.005 4 828 61 706.0 15.2 663.0 6.7 B2-5 499 268 445 0.89 0.066 6 0.001 9 1.003 9 0.030 1 0.108 4 0.001 2 432 88 136.0 5.3 120.0 1.4 B2-6 1 925 111 889 0.46 0.055 4 0.002 3 0.143 8 0.006 0 0.018 8 0.000 2 320 89 192.0 6.5 183.0 2.1 B2-7 1 328 138 790 0.59 0.052 8 0.002 0 0.208 4 0.007 8 0.028 8 0.000 3 2 483 28 2 447.0 17.7 2 387.0 18.3 B2-8 1 116 1 233 400 0.36 0.162 5 0.002 8 10.133 7 0.192 7 0.448 2 0.004 1 122 -92 127.0 5.2 127.0 1.5 W49-1 1 917 159 1 456 0.76 0.048 3 0.002 2 0.133 3 0.005 9 0.019 9 0.000 2 65 89 123.0 4.3 127.0 1.4 W49-2 1 984 163 1 542 0.78 0.047 3 0.001 9 0.129 3 0.004 8 0.019 9 0.000 2 200 -71 127.0 6.3 127.0 1.6 W49-3 1 341 81 726 0.54 0.048 7 0.002 6 0.133 8 0.007 1 0.019 9 0.000 3 228 61 121.0 4.2 116.0 1.0 W49-4 732 74 680 0.93 0.050 7 0.001 9 0.126 7 0.004 7 0.018 2 0.000 2 506 89 329.0 10.7 308.0 3.0 W49-5 221 28 55 0.25 0.057 3 0.002 3 0.382 5 0.014 6 0.048 9 0.000 5 332 76 299.0 8.6 297.0 3.0 W49-6 266 27 61 0.23 0.053 0 0.001 8 0.342 4 0.011 3 0.047 2 0.000 5 165 132 147.0 7.7 148.0 2.4 
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