Dating and reconstruction of protoliths of the Laojunmiao Group and its indications for basement in eastern Junggar, Xinjiang
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摘要:
老君庙岩群出露于准噶尔盆地东北緣，发育一套高绿片岩相-角闪岩相变质岩，其形成时代和构造背景长期以来存在争议。对钾长糜棱片岩进行锆石U-Pb定年，结果显示老君庙岩群年龄值主要集中在500~54OMa之间，少数为新元古代早期（740~920Ma），根据最年轻的峰值年龄（约520Ma）将老君庙岩群时代重新厘定为早寒武世。利用岩石地球化学特征对老君庙岩群进行原岩恢复，显示其具有大陆壳的特征，原岩建造类似复理石建造，其形成的构造环境应属陆緣海环境。关于准噶尔盆地基底属性的问题一直没有定论，通过本次研究，结合区域资料，认为东准噶尔地区存在前寒武基底。
Abstract:The Laojunmiao Group which is exposed on the northeastern margin of the Runggar basin consists of metamorphic complex of high greenschist facies to amphibolite facies. Its formation age and tectonic setting has been controversial for a long time. Zircon U-Pb dating of K-feldspar mylonite schist yielded a number of ages which are mostly concentrated on 500~544Ma with, a few belonging to early Neoproterozoic(740~920Ma).According to the youngest peak age(~520Ma), the age of Laojunmiao Group is redefined as early Cambrian.The lithogeochemical characteristics of Laojunmiao Group show that it has the characteristics of the continental crust, the protoliths formation is similar to a set of flysch formation and its tectonic environment should belong to the continental margin sea.As the problem in regard of the basement properties of funggar basin has not been conclusive yet, the results of this study in combination with, regional data can prove the existence of Precambrian basement in Eastern Junggar.
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Keywords:
- Laojunmiao Group /
- zircon U-Pb /
- reconstruction of protoliths /
- Eastern Junggar /
- basement
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图 1 研究区地质简图(据参考文献①修改)
1—第四系堆积物；2—新近系；3—侏罗系；4—三叠系；5—二叠系；6—石炭系；7—泥盆系；8—志留系；9—寒武系；10—泥盆纪-石炭纪增生混杂岩带；11—花岗岩体；12—超基性岩；13—地质界线；14—断层及编号；15—采样点；➊—卡拉麦里断裂；➋—清水-苏吉泉断裂
Figure 1. Simplified geological map of the study area
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图 2 老君庙岩群锆石阴极发光(CL)图像、测点及年龄
Figure 2. CL images, analytical spots and ages of zircons from Laojunmiao Group
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图 3 老君庙岩群锆石U-Pb谐和图(a)及年龄概率分布直方图(b)
Figure 3. U-Pb concordia diagram(a)and relative probability histogram(b)of the zircons in Laojunmiao Group
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图 4 老君庙岩群稀土元素配分模式图(球粒陨石标准化值据参考文献[25])
Figure 4. Rare earth element distribution pattern of Laojunmiao Group
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图 5 老君庙岩群微量元素蛛网图(原始地幔标准化值据参考文献[26])
Figure 5. Primitive mantle-normalized trace element spidegrams of Laojunmiao Group
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图 6 老君庙岩群Si-((al+fm)-(c+alk))图解[27]
Figure 6. Si-((al+fm)-(c+alk)) diagram of Laojunmiao Group
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图 7 老君庙岩群log(SiO2/Al2O3)-log(Na2O/K2O)图解[28]
Figure 7. log(SiO2/Al2O3)-log(Na2O/K2O)diagram of Laojunmiao Group
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图 8 东准噶尔地区碎屑锆石年龄统计(不含大于1000Ma的数据)
Figure 8. Diagrams of the detrital zircon ages in Eastern Junggar
表 1 老君庙岩群LA-ICP-MS锆石U-Th-Pb测年结果
Table 1 Data of LA-ICP-MS U-Th-Pb dating of zircons from Laojunmiao Group
测点号 含量/10-6 Th/U 同位素比值 年龄/Ma Pb Th U 206Pb/238U 1σ 207Pb/235U 1σ 207Pb/206Pb 1σ 206Pb/238U 1σ 1 27 16 58 0.28 0.1474 0.0023 1.610 0.062 0.0793 0.0031 886.2 12.9 2 184 255 449 0.57 0.0853 0.0010 0.688 0.014 0.0585 0.0013 527.9 5.8 3 117 146 255 0.57 0.0852 0.0013 0.772 0.047 0.0701 0.0080 527.2 7.8 4 148 189 636 0.30 0.0826 0.0005 0.674 0.012 0.0590 0.0010 511.7 3.3 5 455 479 369 1.30 0.1214 0.0009 1.098 0.020 0.0655 0.0012 738.5 5.4 6 194 147 279 0.52 0.1509 0.0013 1.494 0.030 0.0716 0.0014 906.0 7.4 7 193 283 358 0.79 0.0834 0.0007 0.643 0.015 0.0558 0.0013 516.3 4.3 8 119 168 259 0.65 0.0833 0.0008 0.684 0.020 0.0597 0.0017 515.5 4.8 9 185 261 328 0.80 0.0845 0.0008 0.703 0.016 0.0601 0.0013 523.1 4.5 10 131 189 284 0.66 0.0843 0.0009 0.724 0.019 0.0622 0.0016 521.9 5.4 11 301 196 846 0.23 0.1531 0.0012 1.560 0.025 0.0735 0.0011 918.3 6.6 12 162 209 409 0.51 0.0857 0.0011 0.729 0.021 0.0618 0.0017 529.9 6.5 13 167 149 303 0.49 0.1318 0.0012 1.202 0.027 0.0660 0.0015 798.4 6.9 14 176 91 824 0.11 0.1523 0.0012 1.497 0.026 0.0711 0.0013 913.7 6.8 15 125 191 236 0.81 0.0825 0.0012 0.692 0.063 0.0593 0.0039 510.8 7.4 16 167 241 362 0.67 0.0804 0.0008 0.705 0.022 0.0632 0.0019 498.6 4.9 17 152 98 317 0.31 0.1401 0.0024 1.589 0.046 0.0812 0.0017 845.1 13.7 18 182 265 422 0.63 0.0841 0.0008 0.681 0.014 0.0585 0.0012 520.6 4.8 19 85 113 255 0.44 0.0841 0.0009 0.688 0.020 0.0594 0.0018 520.7 5.8 20 305 428 818 0.52 0.0854 0.0007 0.688 0.014 0.0582 0.0012 528.3 4.3 21 112 144 302 0.48 0.0865 0.0010 0.748 0.034 0.0633 0.0034 534.9 5.9 22 138 187 333 0.56 0.0837 0.0009 0.704 0.021 0.0610 0.0019 517.9 5.5 23 150 108 342 0.32 0.1521 0.0013 1.496 0.030 0.0713 0.0015 912.5 7.5 24 114 153 284 0.54 0.0870 0.0009 0.736 0.031 0.0614 0.0026 537.7 5.6 25 101 92 129 0.71 0.1430 0.0018 1.381 0.037 0.0702 0.0019 861.7 10.3 26 167 738 218 3.39 0.1376 0.0016 1.373 0.033 0.0723 0.0017 831.1 8.9 
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表 2 老君庙岩群主量、微量及稀土元素组成
Table 2 Compositions of major, trace and rare earth elements in Laojunmiao Group
样品号 QY-1 QY-2 QY-3 QY-4 QY-5 QY-6 QY-7 QY-8 QY-9 QY-10 QY-11 QY-12 QY-13 SiO2 69.75 69.0 70.15 62.92 62.21 61.69 64.58 66.25 77.48 63.36 79.87 62.79 60.79 TiO2 0.29 0.35 0.31 0.71 0.66 0.58 0.38 0.39 0.50 0.48 0.11 0.77 0.77 Al2O3 13.47 15.31 13.74 15.33 14.20 12.11 9.36 9.81 8.13 10.48 3.52 12.37 12.97 Fe2O3 0.81 1.03 0.88 1.38 1.72 0.96 0.71 0.58 1.12 1.40 0.67 0.90 1.67 FeO 1.35 1.78 1.62 4.60 3.97 4.24 2.90 3.24 1.90 2.74 1.28 5.00 4.39 MnO 0.05 0.05 0.04 0.09 0.09 0.11 0.10 0.11 0.07 0.13 0.10 0.09 0.09 MgO 1.00 1.74 0.89 4.09 3.71 3.70 2.65 2.81 1.15 2.85 0.85 3.70 4.10 CaO 2.64 0.71 2.76 1.62 3.66 5.96 7.15 5.53 2.59 6.78 6.65 3.48 3.83 Na2O 5.86 6.49 5.96 2.70 3.36 3.06 2.60 3.08 3.49 3.44 1.20 2.90 2.31 K2O 0.74 0.72 0.69 2.51 1.74 1.18 0.87 0.61 0.29 0.57 0.15 1.06 1.74 P2O5 0.07 0.09 0.08 0.17 0.17 0.15 0.12 0.11 0.16 0.13 0.07 0.18 0.19 烧失量 3.23 3.23 1.86 3.55 4.39 6.21 7.53 6.19 3.12 7.17 5.97 5.31 5.85 合计 99.4 100.7 99.2 100.2 100.3 100.4 99.3 99.1 100.2 99.8 100.3 99.1 99.2 Rb 26.9 29.6 24.1 89.2 53.1 39.2 34.6 25.5 13.6 22.4 6.5 44.5 74.1 Sr 121.5 223 178.5 188 300 277 243 169.5 101.5 186.5 143.5 114 139 Ba 65.9 93.7 83.1 491 469 303 196 159 77.4 159 158 191 352 Th 6.13 7.2 6.21 9.23 7.92 7.4 4.92 5.8 11.9 6.38 2.51 12.55 14.45 U 0.95 1.24 1.16 2.65 2.19 2.38 0.95 1.18 3.23 0.9 0.43 1.68 2.51 Nb 5.8 4.5 3.7 8.8 7.8 6.7 4.5 4.9 7.4 5.5 1.8 8.6 9 Ta 0.2 0.1 0.2 0.4 0.6 0.4 0.42 0.43 0.64 0.47 0.16 0.68 0.72 Zr 80 113 80 163 151 168 85 101 299 133 34 240 252 Hf 2.4 3.4 2.5 4.6 4.1 4.7 2.3 2.7 7.5 3.5 0.9 6.3 6.4 P 285.5 367.1 326.3 693.4 693.4 611.8 489.5 448.7 652.6 530.3 285.5 734.2 775 Ti 2320 2800 2480 5680 5280 4640 3040 3120 4000 3840 880 6160 6160 La 17.6 18.8 13.2 24.6 23.3 21.3 15 16.8 27.1 19.3 5.2 32 37.5 Ce 30.7 34.7 24.2 51.8 48.5 44.1 31.3 33.4 56.5 38.9 10.9 68.6 77.9 Pr 3.24 3.61 2.58 5.92 5.7 5.1 3.52 3.79 6.33 4.47 1.37 7.43 8.29 Nd 11.4 12.6 9.1 23.1 22 20.5 13.9 14.9 24.7 17.7 5.7 29 32.1 Sm 1.94 2.05 1.55 4.92 4.96 4.08 2.7 2.98 4.89 3.47 1.26 5.39 6.08 Eu 0.5 0.57 0.44 1.13 1.2 0.99 0.63 0.65 0.93 0.81 0.25 1.09 1.24 Gd 1.55 1.61 1.21 4.46 4.46 3.81 2.42 2.57 4.56 3.19 1.3 4.44 5.23 Tb 0.2 0.25 0.2 0.74 0.73 0.59 0.36 0.38 0.71 0.47 0.19 0.61 0.73 Dy 1.18 1.26 1.07 4.46 4.11 3.36 2.26 2.45 4.7 2.91 1.27 3.79 4.51 Ho 0.22 0.25 0.21 0.95 0.82 0.67 0.48 0.51 0.98 0.61 0.29 0.79 0.86 Er 0.59 0.71 0.6 2.72 2.37 1.89 1.37 1.48 2.92 1.71 0.92 2.27 2.5 Tm 0.09 0.11 0.09 0.44 0.35 0.28 0.2 0.22 0.44 0.27 0.15 0.36 0.37 Yb 0.6 0.73 0.6 2.63 1.87 1.39 1.51 2.77 1.71 2.45 1.13 2.45 2.52 Lu 0.1 0.11 0.1 0.41 0.34 0.3 0.21 0.22 0.41 0.27 0.21 0.37 0.4 Y 6.5 6.7 6.4 24.5 21.1 18 13.5 14 31.4 17 9 22.9 25.8 ∑REE 76.4 84.1 61.6 153 142.2 126.8 89.2 95.9 169.3 112.8 181.5 206 LR/HR 5.93 6.17 4.87 2.69 2.89 3.12 3.02 3.11 2.46 3.01 3.78 3.8 CeN/YbN 13.23 12.3 10.43 5.09 5.65 6.1 5.82 5.72 5.28 5.88 7.24 8.0 δEu 0.85 0.93 0.95 0.72 0.77 0.76 0.74 0.7 0.59 0.73 0.66 0.66 RbN/YbN 14.76 13.35 13.22 11.16 7.87 6.9 8.19 5.56 1.62 4.31 5.98 9.68 (al+fm)- (c+alk) 22 47 22 47 24 2 -17 -5 12 -10 24 23 Si尼格里值 507 522 497 445 399 378 421 474 803 396 455 413 注：QY-1~QY-6为白云母钾长糜棱片岩；QY-7、QY-9、QY-10和QY-13为斜长绿泥石英片岩；QY-8为斜长二云母石英片岩；QY-11为石英脉；QY-12为黑云母斜长片岩；数据由广州澳实分析检测公司测试；主量元素含量单位为%，微量和稀土元素含量单位为10-6
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成守德, 王广瑞, 杨树德, 等.新疆古板块构造[J].新疆地质, 1986, (2):3-28. http://d.old.wanfangdata.com.cn/Thesis/Y056005 黄汲清, 任纪舜, 姜春发, 等.中国大地构造基本轮廓[J].地质学报, 1977, 51(2):19-37. http://www.cnki.com.cn/Article/CJFDTotal-DZXE197702002.htm 陈哲夫, 梁云海.新疆多旋回构造与板块运动[J].新疆地质, 1991, (2):95-107. http://www.cnki.com.cn/Article/CJFDTotal-XJDI199102000.htm 李锦轶, 何国琦, 徐新, 等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报, 2006, 80(1):148-168. doi: 10.3321/j.issn:0001-5717.2006.01.017 张海祥, 牛贺才, Sato H, 等.新疆北部晚古生代埃达克岩、富铌玄武岩组合:古亚洲洋板块南向俯冲的证据[J].高校地质学报, 2004, 10(1):106-113. doi: 10.3969/j.issn.1006-7493.2004.01.010 张招崇, 周刚, 闫升好, 等.阿尔泰山南缘晚古生代火山岩的地质地球化学特征及其对构造演化的启示[J].地质学报, 2007, 81(3):344-358. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200703007 马瑞士, 舒良树, 孙家齐.东天山构造演化与成矿[M].北京:地质出版社, 1997. 李锦轶, 朱宝清.新疆东准噶尔卡拉麦里地区晚古生代板块构造的基本特征[J].地质论评, 1990, 36(4):305-316. doi: 10.3321/j.issn:0371-5736.1990.04.003 李锦轶.新疆东准噶尔蛇绿岩的基本特征和侵位历史[J].岩石学报, 1995, (s1):73-84. http://www.cnki.com.cn/Article/CJFDTotal-YSXB5S1.005.htm 何国琦, 李茂松, 贾进斗, 等.论新疆东准噶尔蛇绿岩的时代及其意义[J].北京大学学报(自然科学版), 2001, 37(6):852-858. doi: 10.3321/j.issn:0479-8023.2001.06.017 唐红峰, 苏玉平, 刘丛强, 等.新疆北部卡拉麦里斜长花岗岩的锆石U-Pb年龄及其构造意义[J].大地构造与成矿学, 2007, 31(1):110-117. doi: 10.3969/j.issn.1001-1552.2007.01.013 汪帮耀, 姜常义, 李永军, 等.新疆东准噶尔卡拉麦里蛇绿岩的地球化学特征及大地构造意义[J].矿物岩石, 2009, 29(3):74-82. doi: 10.3969/j.issn.1001-6872.2009.03.012 赵恒乐, 许凡, 张冀, 等.东准噶尔卡拉麦里蛇绿岩形成时代、地质特征及构造意义[J].新疆地质, 2012, 30(2):161-164. doi: 10.3969/j.issn.1000-8845.2012.02.008 黄岗, 牛广智, 王新录, 等.新疆东准噶尔卡拉麦里蛇绿岩的形成时代和侵位时限——来自辉绿岩和凝灰岩LA-ICP-MS锆石U-Pb年龄的证据[J].地质通报, 2012, 31(8):1267-1278. doi: 10.3969/j.issn.1671-2552.2012.08.006 韩琼.东准噶尔卡拉麦里成矿带金矿成矿规律与成矿模式研究[D].新疆大学硕士学位论文, 2014. 闫晓兰, 李逸凡, 刘红涛, 等.新疆卡拉麦里造山型金矿系统[J].新疆地质, 2014, 32(3):328-333. doi: 10.3969/j.issn.1000-8845.2014.03.008 陈伟志, 顾雪祥, 章永梅, 等.新疆东准噶尔金水泉金矿床地质特征、成矿时代及其地质意义[J].地质通报, 2019, 38(7):1240-1255. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201907016 Anderson T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology, 2002, 192(1/2):59-79. https://www.sciencedirect.com/science/article/pii/S000925410200195X
Ludwig K R.Isoplot /Ex version 2.49:A geochronological toolkit for Microsoft Excel[M].Berkeley:Berkeley Geochronology Center Special Publication, 2003:1-56. https://www.researchgate.net/publication/215580284_Users_Manual_for_IsoplotEx_Rev_249
路远发.Geokit:一个用VBA构建的地球化学工具软件包[J].地球化学, 2004, 33(5):459-464. doi: 10.3321/j.issn:0379-1726.2004.05.004 Vavra G, Schmid R, Gebauer D.Internal morphology, habit and U-Th-Pb microanalysis of amphibolite-to-granulite facies zircons:Geochronology of the ivrea zone(Southern Alps)[J].Contributions to Mineralogy and Petrology, 1999, 134(4):380-404. doi: 10.1007/s004100050492
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. doi: 10.3321/j.issn:0023-074X.2004.16.002 Gehrels G E, Johnsson M J, Howell D G.Detrital zircon geochronology of the Adams argillite and Nation River Formation, East-Central Alaska, U.S.A[J].Journal of Sedimentary Research, 1999, 69(1):135-144. doi: 10.2110/jsr.69.135
Cawood P A, Nemchin A A.Provenance record of a rift basin:U/Pb ages of detrital zircons from the Perth basin, West Australia[J].Sedimentary Geology, 2000, 134(3):209-234. https://www.sciencedirect.com/science/article/abs/pii/S0037073800000440
Boynton W V.Chapter 3-Cosmochemistry of the Rare Earth Elements:Meteorite Studies[J].Developments in Geochemistry, 1984:63-114. https://www.sciencedirect.com/science/article/pii/B9780444421487500083
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: 10.1144/GSL.SP.1989.042.01.19
Simonen A.Stratigraphy and sedimentation of the Svecofennidic, early Archean supracrustal rocks in southwestern Finland[J].Bulletin of the Geological Society of Finland, 1953, 160:1-64. https://www.sciencedirect.com/science/article/pii/030192688690015X
Pettijohn F J, Potter P E, Siever R.Sand and Sandstone[M].Springer, 1972.
李锦轶, 肖序常, 陈文.准噶尔盆地东部的前晚奥陶世陆壳基底——来自盆地东北缘老君庙变质岩的证据[J].地质通报, 2000, 19(3):297-67. doi: 10.3969/j.issn.1671-2552.2000.03.014 Rainbird R H, Hamiltom M A, Young G M.Detrital zircon geochronology and provenance of the Torridonian, NW Scotland[J].Journal of the Geological Society, 2001, 158(1):15-27. doi: 10.1144/jgs.158.1.15
Nelson D R.An assessment of the determination of depositional ages for precambrian clastic sedimentary rocks by U-Pb dating of detrital zircons[J].Sedimentary Geology, 2001, 141:37-60. https://www.sciencedirect.com/science/article/pii/S0037073801000677
Fedo C M, Sircombe K N, Rainbird R H.Detrital zircon analysis of the sedimentary record[J].Reviews in Mineralogy & Geochemistry, 2003, 53(1):277-303. doi: 10.2113-0530277/
Dickinson W R, Gehrels G E.Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata:A test against a Colorado Plateau Mesozoic database[J].Earth & Planetary Science Letters, 2009, 288(1):115-125. https://www.sciencedirect.com/science/article/pii/S0012821X09005469
Johnston S, Gehrels G, Valencia V, et al.Small-Volume U-Pb Zircon Geochronology by Laser Ablation-Multicollector-ICP-MS[J].Chemical Geology, 2009, 259(3):218-229. https://www.sciencedirect.com/science/article/pii/S0009254108005159
Lawton T F, Bradford B A.Correlation and Provenance of Upper Cretaceous(Campanian)Fluvial Strata, Utah, U.S.A.from Zircon U-Pb Geochronology and Petrography[J].Journal of Sedimentary Research, 2011, 81(78):495-512. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=7dd45a97b027e1e4e6f47af56b095b02
Robinson A C, Ducea M, Lapen T J.Detrital zircon and isotopic constraints on the crustal architecture and tectonic evolution of the northeastern Pamir[J].Tectonics, 2012, 31(2):1-16. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=10.1029/2011TC003013
Ludwig K R, Mundil R.Extracting reliable U-Pb ages and errors from complex populations of zircons from Phanerozoic tuffs[C]//Journal conference Abstract 12th Goldschmidt Conference, 2002.
Ludwig K R.User's Manual for isoplot 3.70.A geochronological toolkit for Microsoft Excel[M].Berkeley:Berkeley Geochronology Center Special Publication No.4, 2008. https://www.researchgate.net/publication/248255124_User''s_Manual_for_IsoplotEx
肖序常, 汤耀庆, 李锦轶.试论新疆北部大地构造演化[J].新疆地质科学, 1990, (1):47-68. http://www.cnki.com.cn/Article/CJFDTotal-XJDI199802000.htm 徐新忠, 王有学, 蒋亚明, 等.新-甘地震测深剖面的地壳速度结构及大地构造单元划分[J].新疆地质, 1992, 10(2):147-154. http://www.cnki.com.cn/Article/CJFD1992-XJDI199202006.htm 李春昱.中国板块构造的轮廓[J].地质科学院院报, 1980, 2(1):1-5. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=HY000001810336 Hsü K J.Relict Back-Arc Basins: Principles of Recognition and Possible New Examples from China[C]//Kleinspehn K L, Paola C.Frontiers in Sedimentary Geology, New Perspectives in Basin Analysis.Springer New York, 1988: 245-263.
任纪舜.中国大地构造及其演化[M].北京:科学出版社, 1980:50-52. 王鸿祯.中国古地理图[M].北京:地图出版社, 1986. 吴庆福.论准噶尔中间地块的存在及其在哈萨克斯坦板块构造演化中的位置[C]//中国北方板块构造论文集(2).北京: 地质出版社, 1987: 29-38. 张前锋, 胡霭琴, 张国新, 等.新疆东准噶尔小石头泉前寒武纪变质岩的Sm-Nd等时线年龄证据[J].科学通报, 1996, 41(16):1498-1500. doi: 10.3321/j.issn:0023-074X.1996.16.016 费鼎, 张新初.准噶尔地区磁场解释及区域构造特征[J].地球物理学报, 1987, 30(5):459-468. doi: 10.3321/j.issn:0001-5733.1987.05.003 胡霭琴, 韦刚健.关于准噶尔盆地基底时代问题的讨论——据同位素年代学研究结果[J].新疆地质, 2003, 21(4):398-406. doi: 10.3969/j.issn.1000-8845.2003.04.004 李亚萍, 李锦轶, 孙桂华, 等.准噶尔盆地基底的探讨:来自原泥盆纪卡拉麦里组砂岩碎屑锆石的证据[J].岩石学报, 2007, 23(7):1577-1590. doi: 10.3969/j.issn.1000-0569.2007.07.003 王一剑, 刘洪军, 周娟萍, 等.东准噶尔卡姆斯特北海相火山-沉积岩碎屑锆石LA-ICP-MS U-Pb年龄及地质意义[J].现代地质, 2011, 25(6):1047-1058. doi: 10.3969/j.issn.1000-8527.2011.06.003 聂峰, 田晓丽, 李振生.东准造山带原泥盆系的形成时代及源区:碎屑锆石U-Pb年代学证据[J].地质科学, 2014, 49(2):695-717. doi: 10.3969/j.issn.0563-5020.2014.02.024 苏玉平, 郑建平, Griffin W L, 等.东准噶尔盆地巴塔玛依内山组火山岩锆石U-Pb年代及Hf同位素研究[J].科学通报, 2010, 55(30):2931-2943. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201030007 Ma X X, Shu L S, Santosh M, et al.Detrital zircon U-Pb geochronology and Hf isotope data from Central Tianshan suggesting a link with the Tarim Block:Implications on Proterozoic supercontinent history[J].Precambrian Research, 2012, 206-207:1-16. doi: 10.1016/j.precamres.2012.02.015
李忠, 彭守涛.天山南北麓中—新生界碎屑锆石U-Pb年代学记录、物源体系分析与陆内盆山演化[J].岩石学报, 2013, 29(3):739-755. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201303001 Shu L S, Deng X L, Zhu W B, et al.Precambrian tectonic evolution of the Tarim Block, NW China:New geochronological insights from the Quruqtagh domain[J].Journal of Asian Earth Sciences, 2011, 42(5):774-790. doi: 10.1016/j.jseaes.2010.08.018
朱文斌, 张志勇, 舒良树, 等.塔里木北缘前寒武基底隆升剥露史:来自磷灰石裂变径迹的证据[J].岩石学报, 2007, 23(7):1671-1682. doi: 10.3969/j.issn.1000-0569.2007.07.013 胡霭琴, 张国新, 张前锋, 等.阿尔泰造山带变质岩系时代问题的讨论[J].地质科学, 2002, 37(2):129-142. doi: 10.3321/j.issn:0563-5020.2002.02.001 刘源, 杨家喜, 胡健民, 等.阿尔泰构造带喀纳斯群时代的厘定及其意义[J].岩石学报, 2013, 29(3):887-898. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201303012 Kuzmichev A B, Bibikova E V, Zhuravlev D Z.Neoproterozoic(~800 Ma)orogeny in the Tuva-Mongolia Massif(Siberia):island arc-continent collision at the northeast Rodinia margin[J].Precambrian Research, 2001, 110(1):109-126. doi: 10.1016-S0301-9268(01)00183-8/
Todt W, Bibikova E V, Nutman A.Age of Palaeozoic granites and metamorphism in the Tuvino-Mongolian Massif of the Central Asian Mobile Belt:loss of a Precambrian microcontinent[J].Precambrian Research, 2001, 110(1):143-164. doi: 10.1016-S0301-9268(01)00185-1/
Dobretsov N L, Buslov M M, Yu U.Fragments of oceanic islands in accretion-collision areas of Gorny Altai and Salair, southern Siberia, Russia:early stages of continental crustal growth of the Siberian continent in Vendian-Early Cambrian time[J].Journal of Asian Earth Sciences, 2004, 23(5):673-690. doi: 10.1016/S1367-9120(03)00132-9
李文铅, 马华东, 王冉, 等.东天山康古尔塔格蛇绿岩SHRIMP年龄、Nd-Sr同位素特征及构造意义[J].岩石学报, 2008, 24(4):773-780. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200804016 李锦轶, 王克卓, 孙桂华, 等.东天山吐哈盆地南缘古生代活动陆缘残片:中亚地区古亚洲洋板块俯冲的地质记录[J].岩石学报, 2006, 22(5):1087-1102. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605004 徐学义, 夏林圻, 马中平, 等.北天山巴音沟蛇绿岩斜长花岗岩SHRIMP锆石U-Pb年龄及蛇绿岩成因研究[J].岩石学报, 2006, 22(1):83-94. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200601009 徐学义, 李向民, 马中平, 等.北天山巴音沟蛇绿岩形成于早石炭世:来自辉长岩LA-ICPMS锆石U-Pb年龄的证据[J].地质学报, 2006, 80(8):1168-1176. doi: 10.3321/j.issn:0001-5717.2006.08.010 王银喜, 顾连兴, 张遵忠, 等.博格达裂谷双峰式火山岩地质年代学与Nd-Sr-Pb同位素地球化学特征[J].岩石学报, 2006, 22(5):169-178. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605013 廖卓庭, 周宇星, 王克良, 等.新疆博格达山宽沟地区的石炭系[J].地层学杂志, 1992, 16(2):105-110. http://www.cnki.com.cn/Article/CJFDTotal-DCXZ199202002.htm 陈登超, 赵省民, 邓坚.新疆东部博格达山北侧石炭系碎屑锆石U-Pb定年及其地质意义[J].地质学报, 2010, 84(12):1770-1780. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201012006 简平, 刘敦一, 张旗, 等.蛇绿岩及蛇绿岩中浅色岩的SHRIMP U-Pb测年[J].地学前缘, 2003, 10(4):439-456. doi: 10.3321/j.issn:1005-2321.2003.04.012 肖文交, Windley B F, 阎全人, 等.北疆地区阿尔曼太蛇绿岩锆石SHRIMP年龄及其大地构造意义[J].地质学报, 2006, 80(1):32-37. doi: 10.3321/j.issn:0001-5717.2006.01.004 张元元, 郭召杰.准噶尔北部蛇绿岩形成时限新证据及其东、西准噶尔蛇绿岩的对比研究[J].岩石学报, 2010, 26(2):422-430. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201002006 张越, 陈隽璐, 孙吉明, 等.新疆东准噶尔阿尔曼太蛇绿岩中玄武岩地球化学特征及其地质意义[J].地质通报, 2019, 38(9):1431-1442. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201909003 Long X P, Yuan C, Sun M, et al.Geochemistry and U-Pb detrital zircon dating of Paleozoic graywackes in East Junggar, NW China:Insights into subduction-accretion processes in the southern Central Asian Orogenic Belt[J].Gondwana Research, 2012, 21(2/3):637-653. https://www.sciencedirect.com/science/article/abs/pii/S1342937X11001663
新疆维吾尔自治区地质矿产局.新疆维吾尔自治区区域地质志[M].北京:地质出版社, 1993. Xu B, Jian P, Zheng H F, et al.U-Pb zircon geochronology and geochemistry of Neoproterozoic volcanic rocks in the Tarim Block of northwest China:implications for the breakup of Rodinia supercontinent and Neoproterozoic glaciations[J].Precambrian Research, 2005, 136(2):107-123. doi: 10.1016/j.precamres.2004.09.007
Kwon S T, Tilton G R, Coleman R G, et al.Isotopic studies bearing on the tectonics of the West Junggar Region, Xinjiang, China[J].Tectonics, 1989, 8(4):719-727. doi: 10.1029/TC008i004p00719
肖序常, 汤耀庆, 冯益民.新疆北部及其邻区大地构造[M].北京:地质出版社, 1992:1-162. 杨海波, 高鹏, 李兵, 等.新疆西天山达鲁巴依蛇绿岩地质特征[J].新疆地质, 200523(2):123-126. doi: 10.3969/j.issn.1000-8845.2005.02.004 新疆维吾尔自治区地质调查院.新疆1:25万北山煤窑幅L46C004001区域地质调查报告.2018. 新疆第一区域地质调查大队.新疆东准噶尔地区1:5万L46E019004等6幅区域地质调查报告.2014. 新疆维吾尔自治区地质调查院.新疆1:25万纸房幅L46C004002区域地质调查报告.2000. 陕西省地质调查院.新疆1:25万滴水泉幅L46C003004区域地质调查报告.2015.
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