内蒙古东乌旗瓦窑地区奥陶纪铜山组沉积时代及构造环境判别

于洋, 陈智斌, 周文孝, 薄海军. 内蒙古东乌旗瓦窑地区奥陶纪铜山组沉积时代及构造环境判别[J]. 地质通报, 2017, 36(10): 1814-1822.
引用本文: 于洋, 陈智斌, 周文孝, 薄海军. 内蒙古东乌旗瓦窑地区奥陶纪铜山组沉积时代及构造环境判别[J]. 地质通报, 2017, 36(10): 1814-1822.
YU Yang, CHEN Zhibin, ZHOU Wenxiao, BO Haijun. Tectonic background and deposition epoch of the Tongshan Formation in Wayao area of Dong Ujimqin Banner, Inner Mongolia[J]. Geological Bulletin of China, 2017, 36(10): 1814-1822.
Citation: YU Yang, CHEN Zhibin, ZHOU Wenxiao, BO Haijun. Tectonic background and deposition epoch of the Tongshan Formation in Wayao area of Dong Ujimqin Banner, Inner Mongolia[J]. Geological Bulletin of China, 2017, 36(10): 1814-1822.

内蒙古东乌旗瓦窑地区奥陶纪铜山组沉积时代及构造环境判别

  • 基金项目:
    中国地质调查局项目《内蒙古1:5万阿拉坦合力大队等5幅区域地质矿产调查》(编号:1212011120702)和《内蒙古1:5万硝泡子等5幅区域地质矿产调查》(编号:1212011220448)
详细信息
    作者简介: 于洋(1989-), 男, 硕士, 工程师, 从事区域地质调查研究。E-mail:yuyang198900@126.com
  • 中图分类号: P534.62

Tectonic background and deposition epoch of the Tongshan Formation in Wayao area of Dong Ujimqin Banner, Inner Mongolia

  • 铜山组作为内蒙古北疆兴安地层区早古生代的沉积记录,其沉积环境、成岩时代及构造环境的研究是认识兴蒙造山系早期构造演化的理想窗口。对出露于内蒙古东乌旗瓦窑地区的奥陶纪铜山组进行沉积序列、沉积相及沉积物特征研究,结果显示铜山组为一套陆源碎屑浊积岩。首次获得铜山组中夹层凝灰岩LA-ICP-MS锆石U-Pb年龄为458.5±2.6Ma,显示其沉积时代为中奥陶世-晚奥陶世早期。碎屑岩地球化学分析揭示,铜山组物源区主要具活动大陆边缘和大陆岛弧特征。结合区域地质资料,推测其为活动大陆边缘环境下浊积扇沉积的产物。

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  • 图 1  内蒙古中部及邻区构造地质简图(a,据参考文献[4]修改)、内蒙古阿拉坦合力地区奥陶系分布简图(b)和瓦窑地区铜山组地质简图(c)

    Figure 1. 

    图 2  东乌旗瓦窑铜山组沉积相综合柱状图

    Figure 2. 

    图 3  瓦窑铜山组凝灰岩典型锆石阴极发光图像及锆石U-Pb年龄谐和图

    Figure 3. 

    图 4  瓦窑铜山组砂岩主量元素SiO2/Al2O3-Na2O/K2O分类图解(a)[26]和Hf -La/Th图解(b)[27]

    Figure 4. 

    图 5  瓦窑铜山组砂岩K2O/Na2O-SiO2/Al2O3构造环境判别图解[30]

    Figure 5. 

    图 6  瓦窑铜山组砂岩微量元素的构造环境判别图[30]

    Figure 6. 

    表 1  铜山组砂岩粒度参数(括号内为图解法)

    Table 1.  Grain size parameters of sandstones in Tongshan Formation

    序号平均值(Mz)标准偏差(σ)偏度(SK)峰度(K)
    b0220-1-21.93 (1.84)1.55 (1.34)1.53 (-0.23)8.41 (0.99)
    b0220-4-12.70 (2.42)1.49 (1.40)2.81 (0.37)10.77 (3.13)
    b0220-8-21.78 (1.55)1.72 (1.77)2.33 (0.23)9.45 (1.95)
    b0220-8-32.47 (2.25)1.30 (0.70)3.20 (0.04)14.63 (1.03)
    b0222-12-12.24 (1.86)2.02 (2.01)1.73 (0.15)6.09 (2.23)
    b0222-12-21.92 (1.75)1.25 (0.65)3.58 (0.09)18.54 (1.01)
    注:江汉油田实验室测试
    下载: 导出CSV

    表 2  瓦窑铜山组英安质晶屑凝灰岩LA-ICP-MS锆石U-Th-Pb同位素数据

    Table 2.  LA-ICP-MS zircon U-Th-Pb isotope data for dacite volcanic tuffs of Tongshan Formation from Wayao area

    分析点号含量/10-6Th/U同位素比值年龄/Ma
    ThU207Pb/206Pb207Pb/235U206Pb/238U208Pb/232Th206Pb/238U207Pb/235U
    1181930.570.05810.00090.6570.0100.08210.00070.03320.000550945138
    2161740.450.06070.00190.6800.0230.08120.00140.04010.0017504952718
    3618100.270.05670.00060.5810.0060.07430.00110.03050.000246274655
    4607720.360.05810.00070.5900.0080.07360.00070.03250.001045854716
    5677850.360.05770.00050.6540.0060.08210.00070.03400.001050945115
    6232580.800.05870.00120.5940.0140.07350.00080.03300.0004457547311
    7628350.240.05460.00060.5560.0060.07380.00080.03190.000345954495
    8535990.280.06130.00070.7090.0090.08390.00080.04740.001151955447
    9526860.260.05620.00060.5800.0060.07480.00090.03290.000246554655
    10485920.480.05870.00130.5900.0160.07290.00110.03430.0005453747112
    11414850.250.05620.00260.6300.0330.08140.00100.04530.0022504649626
    121088080.970.05960.00250.6890.0360.08380.00080.06770.0006519553228
    13525450.510.05980.00120.6840.0140.08300.00110.04480.0015514752911
    14161890.660.05550.00180.5710.0200.07470.00080.02960.0005464545916
    15232690.600.06020.00120.6010.0130.07240.00060.03420.0006450447810
    16222050.590.11850.00411.5240.0580.09330.00130.03610.0010575894035
    17323430.470.06230.00260.7000.0350.08140.00120.04350.0010504853827
    18291960.740.06020.00090.6720.0120.08090.00090.03150.000350265229
    19921960.670.06920.00100.8840.0170.09260.00110.03740.0010571764312
    20491930.390.06700.00070.6870.0090.07430.00100.02990.000646265317
    21681740.400.06420.00060.6590.0070.07440.00100.03750.001146365145
    22358100.610.05590.00100.5700.0130.07390.00110.02610.0006460745810
    23671870.350.06050.00140.6180.0190.07410.00150.03080.0006461948815
    24227851.310.07450.00160.7480.0180.07270.00080.02940.0004453556714
    25622580.500.06440.00130.64500.0150.07320.00090.03480.0010455650812
    26608350.290.05900.00070.6050.0070.07440.00070.03260.000646244805
    27535990.730.05720.00070.6420.0090.08150.00070.02610.000450545047
    28806860.350.06770.00071.2640.0130.13540.00140.04900.001681988308
    29545920.480.05940.00060.6070.0060.07410.00120.02820.000446174824
    301672421.440.09080.00521.0480.0740.08370.00150.04330.0016518972852
    下载: 导出CSV

    表 3  瓦窑铜山组中砂岩地球化学数据

    Table 3.  Geochemical data of sandstones from the Tongshan Formation in Wayao area

    元素SiO2TiO2AI2O3Fe2O3FeOMgOMnOTFeCaOK2OP2O5Na2O烧失量RbSrBaNbZrHfThCrCoNiScLaCePrNdSmEuGdTbDyHoErTmYbLuYV
    HF0220-1-278.290.269.800.511.330.950.051.842.023.650.122.170.85143.8161.8678.85.97156.35.1910.7125.33.6211.594.6223.1645.685.3520.694.050.683.870.593.550.72.010.312.010.3219.3229.83
    HF0220-5-262.790.6817.341.834.382.940.116.210.365.590.101.182.70233.570.25594.814.17225.96.5014.0576.210.5252.7117.4451.9298.6211.7444.678.581.217.001.236.961.33.680.594.020.6136.50103.7
    HF0220-8-377.290.2510.770.850.900.650.061.751.624.100.102.500.91138.2171.3795.66.48135.54.389.5826.23.0511.424.7026.2042.645.7020.803.970.783.550.593.340.661.950.352.020.3019.4828.81
    HF0220-9-182.500.218.281.590.370.850.101.963.230.520.091.241.0217.76307.3450.35.27120.43.928.2525.93.1616.953.7516.0730.063.7514.602.700.662.510.432.590.551.580.271.680.2614.3126.89
    HF0222-12-283.330.157.990.170.770.390.050.940.853.460.051.701.0975.89120.0660.18.61105.63.527.6718.43.1511.923.9415.0029.603.4112.952.450.622.190.352.190.441.280.201.350.2211.5320.42
    注:主量元素含量单位为%,微量和稀土元素含量为10-6
    下载: 导出CSV
  • [1]

    Sengör A M C, Natal' in B A, Burtman V S. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J]. Nature, 1993, 364:299-307. doi: 10.1038/364299a0

    [2]

    杨文麟, 骆满生, 王成刚, 等.兴蒙造山系新元古代-古生代沉积盆地演化[J].地球科学, 2014, 39(8):1155-1168. http://d.wanfangdata.com.cn/Periodical/dqkx201408017

    [3]

    陈彦, 张志诚, 李可等.内蒙古苏尼特左旗北奥陶系砂岩物源分析及其地质意义[J].地质通报, 2014, 33(9):1308-1319. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20140905&journal_id=gbc

    [4]

    叶琴, 于洋, 高曦, 等.内蒙古阿拉坦合力苏木汗贝布敦昭奥陶纪裸河组的重新厘定及其意义[J].地质通报, 2013, 32(10):1548-1557. doi: 10.3969/j.issn.1671-2552.2013.10.006 http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20131005&journal_id=gbc

    [5]

    黑龙江地矿局.黑龙江省区域地质志[M].北京:地质出版社, 1993:509-584.

    [6]

    内蒙古自治区地质矿产局.内蒙古自治区岩石地层[M].武汉:中国地质大学出版社, 1996:1-36.

    [7]

    肖文交, 舒良树, 高俊, 等.中亚造山带大陆动力学过程与成矿作用[J].新疆地质, 2008, 26(1):4-8. http://d.wanfangdata.com.cn/Periodical/xjdz200801002

    [8]

    Xiao W J, Li S Z, Santosh M, et al. Orogenic belts in Central Asia:Correlations and connections[J]. Journal of Asian Earth Sciences, 2012, 49:1-6. doi: 10.1016/j.jseaes.2012.03.001

    [9]

    黑龙江地矿局.黑龙江省区域地质志[M].北京:地质出版社, 1993:509-584.

    [10]

    内蒙古自治区地质矿产局.内蒙古自治区岩石地层[M].武汉:中国地质大学出版社, 1996:1-36.

    [11]

    李迎春, 汪岩, 吴淦国, 等.大兴安岭北段扎兰屯地区铜山组源区特征地球化学及碎屑锆石U-Pb年代学制约[J].中国地质, 2013, 40(2):391-402. http://d.wanfangdata.com.cn/Periodical/zgdizhi201302003

    [12]

    南润善, 朱慈英, 郑月娟, 等.内蒙古-兴安区奥陶纪生物组合和古地理某些特征[J].中国地层典, 1992, (6):1-57.

    [13]

    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. http://d.wanfangdata.com.cn/Periodical/zgdizhi200901001

    [14]

    罗根明, 张克信, 林启祥, 等.西秦岭地区晚二叠世-早三叠世沉积相分析和沉积古环境再造[J].沉积学报, 2007, 25(3):332-342. http://d.wanfangdata.com.cn/Periodical/cjxb200703002

    [15]

    Pikering K. T, Stow D A V, Watson M P, et al. Deepwater facies, process and models:a review and classification scheme for modernand ancient sediments[J]. Earth Science Review, 1986, 23:75-174. doi: 10.1016/0012-8252(86)90001-2

    [16]

    Stow D A V, Johansson M. Deep water massive sands:nature, origin and hydrocarbon implications[J]. Marine and Petroleum Geology, 2000, 17(1):145-174.

    [17]

    Bouma A H. Coarse-grained and fine-grained turbidite systems as endmember models:applicability and dangers[J]. Marine and Petroleum Geology, 2000, 17(1):137-143.

    [18]

    晋慧娟, 李育慈.西秦岭造山带中三叠统复理石相研究[J].沉积学报, 2001, 19(3):321-326. http://d.wanfangdata.com.cn/Periodical/cjxb200103001

    [19]

    方爱民, 侯泉林, 李继亮, 等.西昆仑库地混杂岩带中深海浊积岩的浊积相划分及其特征[J].地质科学, 2003, 38(1):1-12. http://d.wanfangdata.com.cn/Periodical/dzkx200301001

    [20]

    Anne G, Bruno S, David P, et al. Present morphology and depositional architecture of a sandy confined submarine system; the Golo turbidite system(eastern margin of Corsica)[J]. Geological Society, London, Special Publications, 2004, 222(1):59-89. doi: 10.1144/GSL.SP.2004.222.01.05

    [21]

    Mutti E, Ricci Lucchi F. Turbidites of the morthern Apennines:Introduction of facies analysis(English translation, 1978)[J]. Int. Geol. Rev., 1972, (22):125-166.

    [22]

    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

    [23]

    Hoskin P W O, Schaltegger U. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochemistry, 2003, (53):27-62.

    [24]

    Rubatto D, Gebauer D. Use of cathodoluminescence for U-Pb zircon dating by ion Microprobe:Some examples from the Western Alps[J]. Cathodoluminescence in Geoscience. Berlin:Springer, 2000:373-400.

    [25]

    Müller A, O' Brien P J, Kennedy A, et al. Linking growth episodes of zircon and metamorphic texture to zircon chemistry:An Example from the ultra-high-temperature granulites of Rogaland (SW Norway)[J]. Geological Society, London, Special Publications, 2003, 220:65-81. doi: 10.1144/GSL.SP.2003.220.01.04

    [26]

    Pettijhon F J, Potter P E, Siever R. Sand and Sandstone[M]. Newyork:Springer Verlag, 1972:1-618.

    [27]

    Long X P, Sun M, Yuan C, et al. Early Paleozoic sedimentary record of the Chinese Altai:Implications for its tectonic evolution[J]. Sedimentary Geology, 2008, 208(3):88-100.

    [28]

    许德如, 马驰, Nonna B C, 等.海南岛北西部邦溪地区奥陶纪火山碎屑沉积岩岩石学矿物学和地球化学:源区及构造环境暗示[J].地球化学, 2007, 36(1):11-26 http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqhx200701001&dbname=CJFD&dbcode=CJFQ

    [29]

    Floyd P A, Leveridge B E. Tectonic environment of the Devonian Gramscatho Basin, South Comwall:Framework mode and geochemical evidence from turbiditic sandstone[J]. Journal of Geology Society London, 1987, 144(4):531-542. doi: 10.1144/gsjgs.144.4.0531

    [30]

    Bhatia M R. Plate tectonics and geochemical composition of sandstones[J]. Geology, 1983, 91(6):611-627. doi: 10.1086/628815

    [31]

    Roser B P, Korsch R J.Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio[J]. Journal of Geology, 1986, (94):635-650.

    [32]

    Murray R W B M R J. Rare earth elements anindicators of different marine depositional environments in chert and shale[J]. Geolo-gy, 1990, (18):228-271.

    鞠文信, 贺宏云, 康小龙, 等. 东乌珠穆沁旗幅(L50C003002)1∶25万区域地质调查报告, 2007.

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收稿日期:  2016-05-06
修回日期:  2017-03-13
刊出日期:  2017-10-25

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