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塔里木盆地中央隆起带寒武系-奥陶系白云岩成岩相及其地球化学特征

宁博 李百强 吴珍珍 高建文 陈斌 赵月帅 王锐

宁博, 李百强, 吴珍珍, 高建文, 陈斌, 赵月帅, 王锐. 塔里木盆地中央隆起带寒武系-奥陶系白云岩成岩相及其地球化学特征[J]. 地质科技通报, 2022, 41(4): 46-56. doi: 10.19509/j.cnki.dzkq.2021.0257
引用本文: 宁博, 李百强, 吴珍珍, 高建文, 陈斌, 赵月帅, 王锐. 塔里木盆地中央隆起带寒武系-奥陶系白云岩成岩相及其地球化学特征[J]. 地质科技通报, 2022, 41(4): 46-56. doi: 10.19509/j.cnki.dzkq.2021.0257
Ning Bo, Li Baiqiang, Wu Zhenzhen, Gao Jianwen, Chen Bin, Zhao Yueshuai, Wang Rui. Diagenetic facies of dolomite and geochemical characteristics across the Cambrian-Ordovician transitions in the Central Uplift Zone, Tarim Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(4): 46-56. doi: 10.19509/j.cnki.dzkq.2021.0257
Citation: Ning Bo, Li Baiqiang, Wu Zhenzhen, Gao Jianwen, Chen Bin, Zhao Yueshuai, Wang Rui. Diagenetic facies of dolomite and geochemical characteristics across the Cambrian-Ordovician transitions in the Central Uplift Zone, Tarim Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(4): 46-56. doi: 10.19509/j.cnki.dzkq.2021.0257

塔里木盆地中央隆起带寒武系-奥陶系白云岩成岩相及其地球化学特征

doi: 10.19509/j.cnki.dzkq.2021.0257
基金项目: 

国家"十三五"科技重大专项专题 2017ZX05005-002-004

中央高校基本科研业务费专项资金资助项目 JZ2021HGQB0284

陕西省自然科学基础研究计划项目 2019JQ-151

详细信息
    作者简介:

    宁博(1990-), 男, 工程师, 主要从事油气地质研究工作。E-mail: 919107789@qq.com

    通讯作者:

    李百强(1989-), 男, 博士后, 主要从事沉积学、碳酸盐岩储层地质与成岩作用等方面的研究工作。E-mail: 15249246598@163.com

  • 中图分类号: P588.245;P618.13

Diagenetic facies of dolomite and geochemical characteristics across the Cambrian-Ordovician transitions in the Central Uplift Zone, Tarim Basin

  • 摘要:

    成岩相识别与划分有助于碳酸盐岩储层分类评价及预测。为了明确塔里木盆地中央隆起带寒武系-奥陶系的白云岩成岩相类型及特征, 通过岩心描述、常规及铸体薄片观察、X衍射分析以及粒度分析等方法, 首先对其岩相学特征进行了详细研究并对成岩相类型进行了划分, 在此基础上, 结合O、C稳定同位素测试方法以及Fe、Mn、Sr、Li、U等常、微量元素测试技术探讨了各类白云岩成岩相的地球化学特征并建立了各类成岩相的模式。研究结果表明, 塔里木盆地中央隆起带寒武系-奥陶系白云岩成岩相可划分为准同生云化亚相(PD-F)、浅埋藏隐伏回流渗透云化亚相(SLRD-F)、浅埋藏活跃回流渗透云化亚相(SARD-F)、表生风化壳岩溶亚相(WK-F)和构造破碎亚相(TF-F)共5类。其中, PD-F模式的白云岩云化流体主要来自咸化海水并受部分淡水影响, 表现出O同位素负偏, Fe、Mn、Sr和Li质量分数明显偏高的特征; SARD-F模式的白云岩基本形成于正常海水, 个别样品受到埋藏溶蚀或重结晶作用以及淡水影响, 整体表现为O同位素值与奥陶纪海水一致, Fe、Mn、Sr质量分数相对较低的特点; SLRD-F模式的白云岩形成环境相对封闭, 受淡水影响较小, 表现为O同位素值与海水一致, Fe、Mn质量分数相对较低, Sr质量分数相对较高的特征; WK-F模式的白云岩样品由于经历表生淡水溶蚀作用和埋藏期的白云化作用, 具有O同位素负偏, Fe、U质量分数较高, Sr质量分数较低的特征; TF-F模式的白云岩样品受到构造热液的影响, 具有O同位素负偏, Fe、Mn、U、Li质量分数低的特征。

     

  • 图 1  塔里木盆地构造区划及采样位置示意图

    Figure 1.  Sketch map of the structure and sampling point locations in the Tarim Basin

    图 2  塔里木盆地下古生界白云岩成岩相特征

    A.砂屑球粒泥晶膏质云岩,HT1井6 436.8 m,中寒武统沙依里克组;B.云斑灰云岩, SN7井7 104.00 m,下奥陶统蓬莱坝组;C.云斑云灰岩, SN7井7 100.05 m, 下奥陶统蓬莱坝组;D.中晶残余砂屑鮞粒白云岩,YB7井6 162.4 m, 下奥陶统蓬莱坝组;E.残余颗粒结构白云岩, 残余双壳类生物碎屑,SN7井7 078.71 m, 下奥陶统鹰山组;F.残余颗粒细晶白云岩, HT1井6 162.4 m,上寒武统丘里塔格组;G.马鞍形中晶白云岩, GL1井6 335.50 m, 下奥陶统蓬莱坝组;H.残余骨架结构,环带白云石,BT5井4 809.42 m,上寒武统丘里塔格组;I.构造角砾中-粗晶白云岩,晶间孔发育,YB5井6 742.80 m,下奥陶统鹰山组;J.角砾状粗-中晶云岩,YQ6井7 315.82 m,上寒武统丘里塔格组;K.中-粗晶残余砂屑云岩,YB5井6 741.40 m,下奥陶统蓬莱坝组;L.中-粗晶残余砂屑云岩,发育溶蚀孔洞,YB5井6 741.40 m,下奥陶统蓬莱坝组

    Figure 2.  Petrographic characteristics of the Lower Paleozoic dolomite in the Tarim Basin

    图 3  塔里木盆地下古生界白云岩δ18O和δ13C散点图

    Figure 3.  Crossplot of δ18O and δ13C of the Lower Paleozoic dolomite in the Tarim Basin

    图 4  塔里木盆地下古生界白云岩Fe、Mn质量分数散点图

    Figure 4.  Crossplot of Fe and Mn contents of the Lower Paleozoic dolomite in the Tarim Basin

    图 5  塔里木盆地下古生界白云岩Sr、U质量分数散点图

    Figure 5.  Crossplot of Sr and U contents of the Lower Paleozoic dolomite in the Tarim Basin

    图 6  塔里木盆地下古生界白云岩Li、U质量分数散点图

    Figure 6.  Crossplot of Fe and U contents of the Lower Paleozoic dolomite in the Tarim Basin

    图 7  研究区不同成岩相模式图

    Figure 7.  Patterns of different diagenetic facies in the study area

    表  1  塔里木盆地下古生界白云岩元素分析数据

    Table  1.   Element concentrations of the Lower Paleozoic dolomite in the Tarim Basin

    样品编号 深度/m 层位 白云岩成岩相类型 白云石有序度 δ18O/‰ δ13C/‰ Mn Fe Sr Li U
    wB/% wB/10-6
    BT5-26 5 218.84 阿瓦塔格组 PD-F / -6.50 -2.24 0.008 0 0.315 0 6 710.828 302.062 1.367
    BT5-27 5 219.13 0.90 -7.09 -0.98 0.007 8 0.143 4 12 703.565 6.896 0.719
    BT5-29 5 219.80 / -6.31 -1.67 0.003 4 0.130 4 11 055.838 31.577 1.371
    BT5-31 5 220.55 0.61 -6.47 -1.38 0.010 1 0.449 3 1 114.320 633.177 2.175
    BT5-32 5 221.55 / -7.09 -0.86 0.006 4 0.318 8 1 376.951 297.174 1.589
    BT5-36 5 223.48 1 -7.22 -0.23 0.004 8 0.158 4 1 439.824 21.517 2.176
    SN7-33 7 098.18 蓬莱坝组 SLRD-F / -5.02 -1.03 0.003 4 0.166 6 161.614 1.965 0.419
    SN7-34 7 098.71 / -5.23 -0.95 0.003 2 0.157 5 180.707 2.158 0.749
    SN7-36 7 100.05 0.82 -6.78 -1.97 0.002 1 0.070 4 276.677 0.609 0.819
    SN7-38 7 103.41 0.79 -5.29 -1.87 0.003 3 0.141 1 226.082 2.447 0.819
    SN7-42 7 134.25 0.80 -4.94 -1.86 0.002 8 0.125 7 312.775 2.258 0.719
    YB5-13 6 743.20 SARD-F / -6.23 -1.51 0.006 6 0.214 7 174.313 1.319 2.487
    YB5-14 6 839.70 / -6.98 -0.84 0.004 5 0.274 7 101.637 0.630 0.950
    YB5-7 6 605.20 / -6.37 -0.81 0.005 8 0.166 0 2.407 139.924 0.959
    BT5-21 4 810.54 丘里塔格组 0.89 -5.58 -1.18 0.003 2 0.141 8 132.155 2.657 1.908
    BT5-24 4 812.49 0.99 -5.58 -0.71 0.003 1 0.079 4 81.046 0.359 0.609
    BT5-55 5 784.32 肖尔布拉克组 1 -5.71 0.48 0.021 6 0.133 6 120.575 1.036 2.132
    YQ6-7 7 117.93 丘里塔格组 WK-F / / / 0.003 7 0.374 1 64.396 5.761 6.412
    YQ6-9 7 118.59 0.79 / / 0.004 3 0.334 0 50.162 3.368 2.192
    YQ6-10-1 7 118.89 / / / 0.004 1 0.398 9 51.851 3.661 4.351
    BT5-14 4 807.68 / -6.29 -1.07 0.003 3 0.192 6 106.202 2.122 0.911
    BT5-17 4 808.62 / -6.50 -0.99 0.004 8 0.183 9 64.152 1.157 1.756
    BT5-19 4 809.77 / -6.11 -1.25 0.003 8 0.131 1 101.641 1.472 1.312
    YB5-10 6 741.00 蓬莱坝组 TF-F / -7.63 -1.08 0.004 3 0.121 6 63.272 0.531 1.101
    YB5-11 6 741.40 0.89 -7.09 -1.27 0.004 6 0.082 1 72.537 0.309 0.828
    YB5-12 6 742.80 / -7.59 -0.84 0.003 0 0.073 8 67.097 0.359 1.487
    YB5-15 6 840.80 / -7.05 -0.50 0.002 1 0.025 2 139.034 1.715 0.888
    YB5-16 6 841.20 0.92 -7.13 -1 0.002 9 0.013 2 85.456 1.057 3.669
    YB5-18 6 842.50 / -7.02 -0.54 0.001 8 0.075 4 60.131 5.283 0.870
    注:PD-F.准同生云化亚相;SLRD-F.浅埋藏隐伏回流渗透云化亚相;SARD-F.浅埋藏活跃回流渗透云化亚相;WK-F.表生风化壳岩溶亚相;TF-F.构造破碎亚相
    下载: 导出CSV
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