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    鄂尔多斯盆地塔然高勒地区直罗组砂岩源区构造背景与物源分析

    俞礽安 朱强 文思博 涂家润 彭胜龙 司庆红 唐永香

    俞礽安, 朱强, 文思博, 涂家润, 彭胜龙, 司庆红, 唐永香, 2020. 鄂尔多斯盆地塔然高勒地区直罗组砂岩源区构造背景与物源分析. 地球科学, 45(3): 829-843. doi: 10.3799/dqkx.2020.001
    引用本文: 俞礽安, 朱强, 文思博, 涂家润, 彭胜龙, 司庆红, 唐永香, 2020. 鄂尔多斯盆地塔然高勒地区直罗组砂岩源区构造背景与物源分析. 地球科学, 45(3): 829-843. doi: 10.3799/dqkx.2020.001
    Yu Reng'an, Zhu Qiang, Wen Sibo, Tu Jiarun, Peng Shenglong, Si Qinghong, Tang Yongxiang, 2020. Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin. Earth Science, 45(3): 829-843. doi: 10.3799/dqkx.2020.001
    Citation: Yu Reng'an, Zhu Qiang, Wen Sibo, Tu Jiarun, Peng Shenglong, Si Qinghong, Tang Yongxiang, 2020. Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin. Earth Science, 45(3): 829-843. doi: 10.3799/dqkx.2020.001

    鄂尔多斯盆地塔然高勒地区直罗组砂岩源区构造背景与物源分析

    doi: 10.3799/dqkx.2020.001
    基金项目: 

    中国地质调查局项目 DD20190119

    国家重点研发计划项目 2018YFC0604200

    详细信息
      作者简介:

      俞礽安(1980-), 男, 高级工程师, 主要从事矿产勘查和理论研究

    • 中图分类号: P597

    Tectonic Setting and Provenance Analysis of Zhiluo Formation Sandstone of Tarangaole Area in the Ordos Basin

    • 摘要: 目前关于鄂尔多斯盆地塔然高勒地区直罗组沉积期物源和区域沉积-构造背景等问题尚缺研究,在一定程度上制约了直罗组物源变化的整体评价.对塔然高勒地区含铀层位直罗组下段砂岩进行了岩石地球化学、碎屑锆石U-Pb测年研究.结果显示,研究区直罗组下段源区岩石类型主要为长英质沉积岩和少量中性岩浆岩;源岩构造背景为活动大陆边缘-大陆边缘弧环境.综合微量、稀土元素特征和获得的锆石U-Pb定年数据,认为塔然高勒地区直罗组的物源主要来自大青山-乌拉山等地区的孔兹岩、TTG片麻岩、麻粒岩和镁铁质-超镁铁质层状侵入岩以及阴山地区形成于华力西期-印支期-燕山期的岩浆岩,直罗组下段砂体展布特征清楚地反映了研究区及相邻铀矿床由北向南的物源供给方向;研究区直罗组下段发现的三叠纪碎屑锆石表明三叠纪时期直罗组下段沉积时印支期侵入岩已被抬升至地表提供了物源,直罗组下段上亚段的年轻物源组分比例比下亚段的大.

       

    • 图  1  鄂尔多斯盆地北部区域地质简图

      年龄数据主要据陈印等(2017)雷开宇等(2017)

      Fig.  1.  Simplified map of northern Ordos Basin

      图  2  研究区直罗组岩石学特征

      a.鄂尔多斯盆地东北部神山沟地区宏观地层露头;b.塔然高勒地区钻孔柱状图;c、d.塔然高勒地区直罗组下段中粗粒砂岩岩心、薄片.Qrt.石英;Pl.斜长石;Bit.黑云母

      Fig.  2.  Petrographic characteristics of Zhiluo Formation in study area

      图  3  研究区直罗组下段砂体等厚图

      Fig.  3.  Contour map of sand thickness of the lower part of Zhiluo Formation in study area

      图  4  研究区直罗组砂岩微量元素MORB标准化蛛网图(a)和稀土元素球粒陨石标准化配分模式(b)

      图a、b中标准化数据分别据Pearce(1984)Boynton(1984)

      Fig.  4.  MORB-normalized trace element spider diagram (a) and chondrite-normalized REE pattern (b) of sandstone of Zhiluo Formation in study area

      图  5  研究区直罗组砂岩碎屑锆石CL图(a、c)和LA-ICP MS U-Pb年龄谐和图(b、d)

      图a、b为UZK45钻孔样品,图c、d为UZK50钻孔样品;图a、c中年龄单位为Ma

      Fig.  5.  CL images(a, c)and LA-ICP MS U-Pb concordia diagrams(b, d)of zircons from Zhiluo Formation sandstone in study area

      图  6  研究区直罗组砂岩碎屑锆石年龄与Th/U关系

      Fig.  6.  The relation between age and Th/U of detrital zircons from Zhiluo Formation sandstone in study area

      图  7  研究区直罗组砂岩碎屑锆石年龄谱

      Fig.  7.  Distribution histograms of detrital zircon ages from Zhiluo Formation sandstone in study area

      图  8  研究区直罗组砂岩F1-F2(a)和Hf-La/Th(b)源区环境判别图

      Fig.  8.  F1-F2 (a) and Hf-La/Th (b) discrimination diagrams of Zhiluo Formation sandstone in study area

      图  9  砂岩源区大地构造背景主量元素判别

      Fig.  9.  Major elements composition of sandstones for tectonic setting discrimination

      图  10  直罗组砂岩的Th-Sc-Zr/10和La-Th-Sc源区构造背景判别图

      A.大洋岛弧;B.大陆岛弧;C.活动大陆边缘;D.被动大陆边缘

      Fig.  10.  Th-Sc-Zr/10 and La-Th-Sc diagrams of Zhiluo Formation sandstone for tectonic setting discrimination

      图  11  鄂尔多斯盆地直罗组砂岩锆石U-Pb年龄谱与邻区锆石年龄谱对比

      图a据张龙等(2016);图c据王盟等(2013);图d~h据雷开宇等(2017).图中n为统计年龄数

      Fig.  11.  Comparison of detrital zircon ages from Zhiluo Formation sandstone in the Ordos Basin with zircon ages of neighboring areas

      表  1  研究区直罗组砂岩主量元素分析结果(%)

      Table  1.   Major elements (%) analytical data of Zhiluo Formation sandstone from Ordos Basin

      地区 编号 SiO2 Al2O3 FeO TFe2O3 CaO CaO* MgO K2O Na2O TiO2 P2O5 MnO LOI CIA*
      塔然高勒 UZK4-1 66.72 14.29 1.38 6.13 0.75 0.75 1.77 3.38 1.95 0.67 0.13 0.09 4.12 70.15
      塔然高勒 UZK4-2 71.45 12.42 2.38 3.09 1.81 1.81 1.45 3.32 1.58 0.58 0.10 0.07 4.04 64.92
      塔然高勒 UZK4-3 66.58 13.81 1.21 5.78 0.94 0.94 1.59 3.48 1.92 0.56 0.11 0.10 5.14 68.54
      塔然高勒 UZK4-8 61.25 12.55 0.93 6.13 5.62 1.97 1.74 2.85 1.78 0.45 0.09 0.21 7.32 67.62
      塔然高勒 UZK4-10 53.09 9.02 0.27 1.78 16.60 1.97 0.78 2.30 1.73 0.34 0.09 0.34 13.92 62.51
      塔然高勒 UZK16-2 74.65 12.23 1.40 2.65 1.11 1.11 1.12 3.38 1.97 0.40 0.08 0.04 2.39 65.44
      塔然高勒 UZK16-3 73.42 12.98 1.29 2.94 0.92 0.92 1.09 3.53 2.15 0.56 0.09 0.04 2.27 66.29
      塔然高勒 UZK16-4 63.86 11.31 1.66 8.50 1.38 1.38 0.92 2.98 1.85 1.00 0.13 0.08 8.00 64.55
      塔然高勒 UZK27-1 69.10 14.22 2.22 4.15 0.64 0.64 2.29 3.31 2.08 0.82 0.15 0.05 3.17 70.22
      塔然高勒 UZK27-2 69.68 13.51 1.51 3.67 1.03 1.03 1.31 3.16 3.54 0.63 0.13 0.06 3.29 63.61
      塔然高勒 UZK27-4 74.42 12.07 1.02 2.11 1.50 1.50 1.00 3.65 2.12 0.31 0.08 0.05 2.70 62.41
      塔然高勒 UZK4-6 72.30 11.93 0.68 1.60 3.08 3.08 0.97 3.32 1.78 0.34 0.08 0.07 4.56 59.32
      OIA 58.83 17.11 5.52 1.95 5.83 3.65 1.60 4.10 1.06 0.26 0.15
      CIA 70.69 14.04 3.05 4.82 2.68 1.97 1.89 3.21 0.64 0.16 0.10
      ACM 73.86 12.89 1.58 3.06 2.48 1.23 2.90 2.77 0.46 0.09 0.10
      PCM 81.95 8.41 1.76 3.28 1.89 1.39 1.71 1.07 0.49 0.12 0.05
      UCC 66.60 15.4 5.04 3.59 2.48 2.80 3.27 0.64 0.15 0.10
      注:为消除碳酸钙胶结物的影响,同时考虑到华北地区大部分TTG岩系及各类中酸性岩浆岩的CaO < 5%,取含量 < 5%的样品的平均值(1.97)作为含量 > 5%的样品的CaO含量,记作CaO*. OIA.洋岛,CIA.大陆岛弧,ACM.活动大陆边缘,PCM.被动大陆边缘;上述数据源自Bhatia(1983).UCC.大陆上地壳,数据源自Rudnik et al.(2003).LOI为烧失量;CIA*表示沉积岩物源区化学分异指数;CIA*=[Al2O3/(Al2O3+CaO*+Na2O+K2O)]×100,式中各氧化物含量均为摩尔质量.
      下载: 导出CSV

      表  2  研究区直罗组砂岩微量元素和稀土元素(10-6)分析结果

      Table  2.   Trace elements (10-6) and rare earth elements (10-6) analytical data of Zhiluo Formation sandstone in study area

      样品编号 塔然高勒 上地壳
      UZK 4-1 UZK 4-2 UZK 4-3 UZK 4-8 UZK 4-10 UZK 16-2 UZK 16-3 UZK 16-4 UZK 27-1 UZK 27-2 UZK 27-4 UZK 4-6
      Cu 16.40 7.95 14.40 12.40 6.63 8.49 9.42 16.00 13.10 11.80 4.77 6.63
      Pb 13.3 15.7 13.9 14.9 11.0 59.4 19.0 20.9 43.0 10.9 11.6 13.4
      Zn 60.5 32.1 39.8 37.5 25.3 21.1 40.0 43.5 52.2 33.7 14.3 37.5
      Cr 69.7 58.0 68.7 54.4 28.8 29.7 41.9 56.0 78.4 49.1 22.2 29.3 35
      Ni 17.8 11.5 17.0 17.1 10.2 9.4 11.6 23.7 20.2 16.9 8.4 9.6 20
      Co 9.01 5.88 8.78 8.22 7.40 5.21 6.90 11.70 11.30 9.70 5.16 4.58 10
      Li 27.3 17.9 26.2 21.6 9.2 11.0 14.0 11.9 35.4 15.9 10.3 10.6
      Rb 98.1 89.1 99.3 79.2 58.1 86.3 97.1 82.3 102.0 94.9 90.1 85.6 110
      Cs 2.78 2.11 2.55 2.16 1.40 1.18 1.44 1.56 1.76 1.37 1.23 1.48
      Sr 242 295 241 227 277 336 317 318 219 213 292 302 350
      Ba 941 1 040 922 742 801 533 775 686 357 659 832 978 700
      V 74.3 145.0 82.4 64.1 36.1 71.3 48.7 95.0 189.0 64.4 31.4 34.6 60
      Sc 9.91 6.20 8.92 10.00 7.46 6.68 6.33 5.89 6.04 8.33 6.07 7.40
      Nb 12.80 10.70 11.60 8.29 5.82 7.35 9.86 19.10 14.20 11.10 6.29 6.54 25
      Ta 0.88 0.69 0.76 0.54 0.38 0.43 0.60 1.05 0.84 0.68 0.39 0.45
      Zr 275 187 222 197 106 123 183 495 340 323 103 104 240
      Hf 7.75 5.38 6.08 5.48 2.97 3.58 5.24 13.30 9.30 9.24 3.02 3.12 5.8
      Be 2.05 1.34 1.94 1.59 1.16 1.20 1.38 1.48 1.60 1.34 1.14 1.06
      Ga 17.2 13.4 16.5 16.8 10.6 11.5 13.1 12.5 17.1 13.9 11.4 12.5
      U 14.40 1.97 29.00 8.51 3.98 0.79 24.80 24.40 4.66 1.29 18.70 14.60 2.5
      Th 6.66 6.24 6.08 6.49 3.45 2.25 2.83 7.63 3.24 3.52 1.78 3.63 10.5
      La 34.40 35.10 29.60 42.20 30.30 8.51 7.83 24 14.8 11.1 6.61 21 30
      Ce 48.9 57.0 37.8 55.6 47.0 16.6 15.1 67.1 41.2 25.6 14.1 32.8 64
      Pr 8.04 7.34 6.38 8.55 6.02 2.31 2.16 5.83 3.13 3.34 1.83 4.76 7.1
      Nd 29.00 25.90 21.80 30.40 21.90 8.97 8.25 22.10 11.40 13.40 7.39 17.30 26
      Sm 4.63 4.12 3.15 4.94 3.62 1.66 1.52 3.81 1.81 2.55 1.48 2.82 4.5
      Eu 1.01 1.11 0.79 1.29 1.09 0.81 0.73 0.99 0.46 0.77 0.79 0.88 0.88
      Gd 3.45 3.37 2.63 3.99 3.27 1.42 1.34 3.55 1.80 2.09 1.24 2.28 3.8
      Tb 0.49 0.49 0.36 0.56 0.46 0.20 0.19 0.52 0.23 0.31 0.20 0.32 2.2
      Dy 2.49 2.60 1.86 2.88 2.41 1.14 1.13 2.88 1.14 1.55 1.13 1.60 3.5
      Ho 0.48 0.50 0.38 0.56 0.48 0.22 0.23 0.57 0.22 0.30 0.22 0.31 0.8
      Er 1.40 1.44 1.10 1.63 1.30 0.63 0.64 1.66 0.72 0.91 0.62 0.86 2.3
      Tm 0.22 0.22 0.18 0.25 0.18 0.10 0.10 0.28 0.12 0.15 0.10 0.13 0.33
      Yb 1.52 1.52 1.18 1.61 1.14 0.72 0.75 1.90 0.90 1.03 0.68 0.87 2.2
      Lu 0.25 0.24 0.18 0.25 0.19 0.12 0.12 0.30 0.14 0.17 0.10 0.14 0.32
      Y 11.60 12.40 9.45 14.00 14.40 5.11 5.33 14.60 5.60 6.98 5.53 7.77 22
      (La/Yb)N 15.26 15.57 16.91 17.67 17.92 7.97 7.04 8.52 11.09 7.27 6.55 16.27
      Eu/Eu* 0.77 0.91 0.84 0.89 0.97 1.61 1.56 0.82 0.78 1.02 1.78 1.06
      (Sm/Nd)N 0.49 0.49 0.44 0.50 0.51 0.57 0.57 0.53 0.49 0.59 0.62 0.50
      (Gd/Yb)N 1.83 1.79 1.80 2.00 2.31 1.59 1.44 1.51 1.61 1.64 1.47 2.11
      下载: 导出CSV

      表  3  不同构造背景下砂岩的REE参数

      Table  3.   The REE geochemical parameters of sandstone in different tectonic settings

      构造背景 物源区类型 La(10-6 Ce(10-6 ΣREE(10-6 La/ Yb (La/Yb)N ΣLREE/ΣHREE Eu/ Eu*
      大洋岛弧 未切割的岩浆弧 8±1.7 19±3.7 58±10 4.2±1.3 2.8+0.9 3.8±0.9 1.04±0.11
      大陆岛弧 切割的岩浆弧 27±4.5 59±8.2 146±20 11±3.6 7.5±2.5 7.7±1.7 0.79±0.13
      活动大陆边缘 基底隆起 37 78 186 12.5 8.5 9.1 0.60
      被动大陆边缘 克拉通内构造高地 39 85 210 15.9 10.8 8.5 0.56
      塔然高勒(n=12) 25.38 46.22 95.13 19.37 12.34 11.15 1.07
      下载: 导出CSV
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