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    北黄海盆地东部坳陷侏罗纪西南物源-沉积体系与源区构造背景

    高丹 程日辉 沈艳杰 王嘹亮 胡小强

    高丹, 程日辉, 沈艳杰, 王嘹亮, 胡小强, 2016. 北黄海盆地东部坳陷侏罗纪西南物源-沉积体系与源区构造背景. 地球科学, 41(7): 1171-1187. doi: 10.3799/dqkx.2016.095
    引用本文: 高丹, 程日辉, 沈艳杰, 王嘹亮, 胡小强, 2016. 北黄海盆地东部坳陷侏罗纪西南物源-沉积体系与源区构造背景. 地球科学, 41(7): 1171-1187. doi: 10.3799/dqkx.2016.095
    Gao Dan, Cheng Rihui, Shen Yanjie, Wang Liaoliang, Hu Xiaoqiang, 2016. Southwestern Provenance-Sedimentary System and Provenance Tectonic Setting of Eastern Sag in the North Yellow Sea Basin. Earth Science, 41(7): 1171-1187. doi: 10.3799/dqkx.2016.095
    Citation: Gao Dan, Cheng Rihui, Shen Yanjie, Wang Liaoliang, Hu Xiaoqiang, 2016. Southwestern Provenance-Sedimentary System and Provenance Tectonic Setting of Eastern Sag in the North Yellow Sea Basin. Earth Science, 41(7): 1171-1187. doi: 10.3799/dqkx.2016.095

    北黄海盆地东部坳陷侏罗纪西南物源-沉积体系与源区构造背景

    doi: 10.3799/dqkx.2016.095
    基金项目: 

    中国地质调查项目 GZH200700405

    国家青年科学基金项目 41402087

    详细信息
      作者简介:

      高丹(1990-),女,博士,主要从事沉积学与储层地质方面研究. E-mail: gaodan14@mails.jlu.edu.cn

      通讯作者:

      程日辉, E-mail:chengrh@jlu.edu.cn

    • 中图分类号: P624

    Southwestern Provenance-Sedimentary System and Provenance Tectonic Setting of Eastern Sag in the North Yellow Sea Basin

    • 摘要: 物源-沉积体系是原始储层物性的主要影响因素,与源区构造背景的综合分析是油气勘探工作的基础.北黄海盆地是位于苏鲁造山带-临津江造山带北侧中朝板块上中-新生代转换伸展断陷盆地.地震和钻井资料证实东部坳陷西南部有中-上侏罗统三角洲砂体发育.岩心和测井上可识别的沉积类型包括分流河道、决口扇、河口坝和远砂坝等,地震反射结构显示出来自西南方向的沉积物进积.砂岩样品的岩矿组成显示,碎屑中存在花岗质成分和酸性火山岩成分.泥岩元素地球化学特征显示其物质成分以长英质为主,推测源区为克拉通或再旋回造山带.砂岩Dickinson图解表明,不仅存在来自克拉通或再旋回造山带的成分,而且存在火山弧造山带的成分.综合分析认为,北黄海盆地东部坳陷西南物源区为再旋回造山带,花岗质成分来自西南盆缘的基底花岗质岩石的风化,而火山岩成分可能是同期火山喷发的产物,也可能是先前火山岩的风化产物.

       

    • 图  1  北黄海盆地大地构造、东部坳陷及钻井位置

      陈亮等(2008)杜民等(2014a, 2014b)

      Fig.  1.  Tectonic map of the North Yellow Sea basin and the location of the eastern sag and the drilling area

      图  2  北黄海盆地东部坳陷中-上侏罗统过B2和B3井地震解释剖面

      a.整个构造-地层解释剖面;b.部分地震剖面;c.部分解释剖面

      Fig.  2.  The Seismic profile and its interpretation of the middle-upper Jurassic of the eastern sag in the North Yellow Sea basin with Well B2 and Well B3

      图  3  北黄海盆地东部坳陷中-上侏罗统盆地充填序列

      LST.低位体系域;EST.湖扩体系域;HST.高位体系域

      Fig.  3.  The middle-upper Jurassic filling succession of the Eastern sag, the North Yellow Sea basin

      图  4  沉积微相模式

      Fig.  4.  Models of sedimentary microfacies

      图  5  典型沉积微相特征

      a.B3井3 093.20~3 093.36 m井段(J3),分流河道,4个向上变细的正韵律;b.B3井3 090.78~3 090.88 m井段(J3),决口扇,砂泥混杂,波状层理;c.B3井3 091.06~3 091.18 m井段(J3),决口扇,砂泥混杂;d.B3井3 093.12 m井段(J3),沼泽;e.B3井3 212.64~3 212.70 m井段(J2),静水泥,含泥砾;f.B2井2 727.55~2 727.71 m井段(J3),远砂坝,透镜状层理;g.B2井2 955.90~2 956.00 m井段(J3),河口坝,斜层理;h.B2井2 956.43~2 956.57 m井段(J3),河口坝;i.B3井3 208.07~32 08.15 m井段(J2),浊流,薄层状发育

      Fig.  5.  Characteristics of typical sedimentary microfacies

      图  6  物质成分特征

      a~i.时代均为J3;a.样品B2-6(2 955.18~2 955.20 m)为花岗岩屑;b.样品B2-5(2 955.02~2 955.05 m)为花岗岩屑;c.样品B2-9(2 957.28~2 957.33 m)为流纹岩屑;d.样品B2-1(2 730.29~2 730.31 m)为火山炸裂晶屑;e.样品B2-9(2 957.28~2 957.33 m)为石英熔蚀;f.样品B2-5(2 955.02~2 955.05 m)为正长石;g.样品B3-2(3 094.32~3 094.38 m),其中① 低温石英、② 高温石英/凝灰质基质;h.样品B2-7(2 955.62~2 955.64 m),其中① 低温石英、② 高温石英/凝灰质基质;i.样品B3-1(3 094.62~3 094.66 m)为凝灰质基质;j.样品B2-8(2 955.98~2 956.00 m),其中① 长石、② 粘土质(伊利石);k.样品B2-7(2 955.62~2 955.64 m)为石英;l.样品B3-2(3 094.32~3 094.38 m),其中① 石英、② 粘土质(高岭石)

      Fig.  6.  Characteristics of material compositions

      图  7  中-上侏罗统主量元素构造环境判别图解

      a, b.底图据Bhatia(1983);c.底图据Roser and Korsch(1986);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.  7.  Major elements composition plots of the upper-middle Jurassic mudstones for tectonic setting discrimination

      图  8  中、上侏罗统Ni-TiO2(a)、La/Th-Hf(b)和碎屑岩源区主元素判别图解(c)

      a底图据Floyd et al.(1989);b底图据Taylor and McLennan(1985);c底图据Roser and Korsch(1988);P1.镁铁质的和少量中性火成岩源区;P2.主要中性火成岩源区(主要为安山岩);P3.长英质火成岩源区(大陆边缘弧);P4.古老的沉积体系或克拉通/再旋回造山带

      Fig.  8.  Ni-TiO2、Hf-La/Th and provenance discriminant function plots of the upper-middle Jurassic

      图  9  上侏罗统Dickinson图解

      底图据Dickinson and Sucaek(1979);黑色方块代表B2井样品;灰色三角形代表B3井样品

      Fig.  9.  The Dickinson diagram of the upper Jurassic

      图  10  东部坳陷中-上侏罗统西南沉积体系发育模式

      Fig.  10.  Model of the southwest sedimentary system of the upper-middle Jurassic in the Eastern sag

      表  1  碎屑组分含量(%)

      Table  1.   The percentage content of clastic component

      样品 深度(m) 定名 Qp Qm P K R T G Ls Tu Ca
      B2 B2-1 2 730.29 凝灰质含钙岩屑石英细砂岩 2 42 0 5 12 5 8 3 15 8
      B2-2 2 952.61 钙质凝灰质岩屑粗砂岩 20 31 0 2 14 2 4 5 4 19
      B2-3 2 954.04 凝灰质岩屑石英含砾粗砂岩 45 22 0 2 5 4 7 1 13 1
      B2-4 2 954.19 岩屑石英含砾粗砂岩 25 27 0 6 8 4 18 0 9 3
      B2-5 2 955.02 岩屑石英含砾粗砂岩 32 41 0 2 9 2 5 1 7 3
      B2-7 2 955.62 凝灰质岩屑石英含砾粗砂岩 19 43 1 6 11 6 5 2 5 4
      B2-8 2 955.98 岩屑石英中砂岩 11 58 2 0 8 3 3 2 9 4
      B2-9 2 957.28 岩屑石英中砂岩 14 58 0 1 10 3 2 2 9 2
      B3 B3-6 3 091.43 含钙岩屑石英粗砂岩 20 45 0 3 9 0 14 0 0 9
      B3-3 3 093.54 岩屑石英含砾粗砂岩 28 50 0 1 5 0 9 0 3 5
      B3-2 3 094.32 岩屑石英含砾中粗砂岩 36 45 0 1 5 3 8 0 3 0
      注:Qp.多晶石英;Qm.单晶石英;P.斜长石;K.正长石;R.流纹岩屑;T.凝灰岩屑;G.花岗岩屑;Ls.沉积岩屑;Tu.凝灰质基质;Ca.钙质.
      下载: 导出CSV

      表  2  北黄海盆地东部坳陷中-下侏罗统泥岩样品的主量(%)、微量及稀土元素含量(10-6)(B3井)

      Table  2.   The contents of major elements, trace elements and rare-earth elements of the middle-upper Jurassic mudstones of Eastern sag in the North Yellow Sea basin (Well B3)

      样号 上侏罗统 中侏罗统
      B3-4 B3-5 B3-7 B3-8 B3-9 B3-10 B3-11 B3-12 B3-13
      SiO2 48.78 57.36 55.58 54.10 52.40 53.52 58.82 49.20 51.20
      Al2O3 21.95 15.23 18.44 16.90 15.50 16.43 17.70 15.91 16.29
      Fe2O3 1.51 0.37 1.65 1.47 2.31 2.23 1.92 2.52 1.52
      FeO 6.87 0.41 5.60 3.52 5.64 3.68 1.72 6.87 3.89
      TiO2 1.10 0.76 0.84 0.70 0.66 0.80 0.72 0.66 0.70
      P2O5 0.15 0.15 0.20 0.15 0.25 0.25 0.20 0.40 0.45
      MnO 0.08 0.02 0.06 0.10 0.18 0.12 0.03 0.22 0.14
      CaO 0.49 0.35 0.51 3.11 2.75 3.46 1.65 2.97 4.26
      MgO 2.66 0.33 2.12 2.99 3.00 2.96 1.62 2.88 3.36
      K2O 2.610 2.310 1.890 4.570 4.500 4.680 5.100 4.420 4.820
      Na2O 0.10 0.06 0.08 1.28 0.95 0.92 0.86 1.39 0.74
      LOI 13.37 22.46 12.46 10.70 11.48 10.71 9.26 12.42 12.45
      Total 92.8 99.4 93.83 96.07 93.98 96.08 97.88 92.99 95.93
      Fe2O3T 8.38 0.78 7.25 4.99 7.95 5.91 3.64 9.39 5.41
      SiO2/Al2O3 2.22 3.77 3.01 3.20 3.38 3.26 3.32 3.09 3.14
      K2O/Na2O 26.10 38.50 23.63 3.57 4.74 5.09 5.93 3.18 6.51
      Al2O3/TiO2 19.95 20.04 21.95 24.14 23.48 20.54 24.58 24.11 23.27
      Fe2O3+MgO 4.17 0.70 3.77 4.46 5.31 5.19 3.54 5.40 4.88
      Al2O3/SiO2 0.45 0.27 0.33 0.31 0.30 0.31 0.30 0.32 0.32
      Al2O3/(CaO+NaO) 37.20 37.15 31.25 3.85 4.19 3.75 7.05 3.65 3.26
      K2O+Na2O 2.71 2.37 1.97 5.85 5.45 5.60 5.96 5.81 5.56
      Ni 135.90 63.46 88.24 36.54 25.28 23.69 51.10 29.82 28.70
      Hf 4.560 7.198 7.215 8.035 7.732 8.342 9.029 7.799 7.955
      La 207.80 63.46 117.40 84.33 83.00 83.59 94.69 76.50 77.02
      Th 24.8 16.3 19.1 25.3 23.6 26 26.6 23.4 24.4
      Cr 141.8 80.18 140.6 79.18 71.85 76.16 87.30 70.80 74.00
      Zr 160.6 281.8 270.3 310.0 305.9 332.7 342.4 309.5 315.8
      Cr/Zr 0.88 0.28 0.52 0.26 0.23 0.23 0.25 0.23 0.23
      La/Th 8.39 3.90 6.14 3.33 3.52 3.22 3.55 3.27 3.16
      下载: 导出CSV

      表  3  碎屑岩源区性质判别函数的变量组成及其系数

      Table  3.   Provenance discriminant function coefficients used to calculate discriminant scores for clastic rocks

      变量 TiO2 Al2O3 Fe2O3T MgO CaO Na2O K2O 常量C
      F1系数 -1.773 0.607 0.760 -1.500 0.616 0.509 -1.224 -9.090
      F2系数 0.445 0.070 -0.250 -1.142 0.438 1.475 1.426 -6.681
      注:判别公式为F=a1x1+a2x2+…+anxn+C,其中,x1~xnn个判别变量,a1~an为其相应系数;据Roser and Korsch(1988).
      下载: 导出CSV

      表  4  Dickinson图解各组分含量(%)

      Table  4.   The contents of components used in Dickinson diagram

      井号 样品号 顶深(m) 底深(m) 定名 Q F L Qm F Lt Qp Lv Ls Qm P K
      B2 B2-1 2 730.29 2 730.31 细砂岩 74.58 7.76 17.66 71.37 7.76 20.88 15.40 84.60 0 90.20 0.78 9.02
      B2-2 2 952.61 2 952.64 粗砂岩 67.86 1.54 30.6 40.36 1.54 58.10 47.33 50.05 2.62 96.33 0 3.67
      B2-3 2 954.04 2 954.05 粗砂岩 71.86 1.61 26.54 23.86 1.61 74.53 64.40 34.16 1.44 93.68 0 6.32
      B2-4 2 954.19 2 954.20 粗砂岩 41.08 4.65 54.27 21.64 4.65 73.71 26.38 70.82 2.81 82.31 0 17.69
      B2-5 2 955.02 2 955.05 粗砂岩 79.46 2.09 18.45 44.71 2.09 53.20 65.32 30.48 4.21 95.54 1.01 3.45
      B2-7 2 955.62 2 955.64 粗砂岩 75.61 7.02 17.37 52.31 7.02 40.66 57.28 39.13 3.59 88.16 1.14 10.70
      B2-8 2 955.98 2 956.00 中砂岩 80.53 1.72 17.75 67.28 1.72 31.00 42.76 55.74 1.50 97.51 2.49 0
      B2-9 2 957.28 2 957.33 中砂岩 80.01 1.38 18.61 64.38 1.38 34.25 45.65 48.50 5.84 97.91 0 2.09
      B3 B3-2 3 094.32 3 094.38 粗砂岩 84.81 0.70 14.50 46.46 0.70 52.85 72.57 21.35 6.08 98.52 0.00 1.48
      B3-3 3 093.54 3 093.60 粗砂岩 82.05 0.00 17.95 53.50 0.00 46.50 61.40 29.17 9.43 100.00 0.00 0.00
      B3-6 3 091.43 3 091.47 粗砂岩 80.53 3.05 16.42 55.19 3.05 41.76 60.67 29.94 9.39 94.76 0.00 5.24
      注:Q.稳定石英颗粒,其中包括Qm和Qp;Qm.单晶石英颗粒;Qp.复晶石英颗粒,主要为燧石质颗粒;F.单晶长石颗粒,其中包括P和K;P.斜长石单晶颗粒;K.钾长石单晶颗粒;L.不稳定复晶岩屑,其中包括Lv和Ls;Lv.火山岩屑和变质火山岩屑;Ls.沉积岩屑和变质沉积岩屑;Lt.岩屑总含量,即相当于L与Qp之和.
      下载: 导出CSV
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