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    华北西部贺兰山中段黄旗口花岗岩成因及地质意义

    余淳梅 杨华本 曾佐勋 吴林波

    余淳梅, 杨华本, 曾佐勋, 吴林波, 2019. 华北西部贺兰山中段黄旗口花岗岩成因及地质意义. 地球科学, 44(4): 1266-1277. doi: 10.3799/dqkx.2018.295
    引用本文: 余淳梅, 杨华本, 曾佐勋, 吴林波, 2019. 华北西部贺兰山中段黄旗口花岗岩成因及地质意义. 地球科学, 44(4): 1266-1277. doi: 10.3799/dqkx.2018.295
    Yu Chunmei, Yang Huaben, Zeng Zuoxun, Wu Linbo, 2019. Geochemistry and Significance of Paleoproterozoic Granitoids from Huangqikou, Central Helanshan Area. Earth Science, 44(4): 1266-1277. doi: 10.3799/dqkx.2018.295
    Citation: Yu Chunmei, Yang Huaben, Zeng Zuoxun, Wu Linbo, 2019. Geochemistry and Significance of Paleoproterozoic Granitoids from Huangqikou, Central Helanshan Area. Earth Science, 44(4): 1266-1277. doi: 10.3799/dqkx.2018.295

    华北西部贺兰山中段黄旗口花岗岩成因及地质意义

    doi: 10.3799/dqkx.2018.295
    基金项目: 

    中国地质大学(武汉)中央高校基本科研业务费专项资金 CUG090101

    宁夏1:5万黄旗口幅区调项目 J48E009016

    国家自然科学青年基金项目 40602009

    详细信息
      作者简介:

      余淳梅(1977-), 博士, 副教授, 从事岩石学和矿物学的教学与研究工作

    • 中图分类号: P581

    Geochemistry and Significance of Paleoproterozoic Granitoids from Huangqikou, Central Helanshan Area

    • 摘要: 华北克拉通孔兹岩带内发育类型复杂的各类岩石,是记录和反演华北西部早期块体拼合以及岩浆作用、变质演化的重要对象,而其中段发育的出露面积广阔、岩性复杂的黄旗口花岗岩体的研究还较为薄弱.在野外地质和岩相学研究基础上,主要报道了贺兰山中段黄旗口花岗岩的主、微量元素和Sr-Nd同位素组成,对岩体的源区特征、成因及地质意义进行了探讨.黄旗口复式花岗岩体主要由早期正长花岗岩、二长花岗岩和晚期英云闪长岩组成.两期岩体具有高K2O(2.97%~6.71%)含量,A/CNK均大于1.1,但晚期侵入单元较早期岩石更贫硅、富铝.两期岩体都表现为轻稀土富集、Eu负异常的特点,且强烈富集K、Rb、Th等大离子亲石元素,亏损Nb、Ta、P、Ti等高场强元素.岩石87Sr/86Sr初始比值变化范围较大,可能是后期改造的结果;εNdt)变化在+1.81~+4.90,对应的Nd同位素模式年龄TDM1为2.10~2.37 Ga,TDM2为2.10~2.35 Ga.这些特征表明黄旗口岩体为S型花岗岩,可能来自该区归属于孔兹岩的赵池沟组岩系的部分熔融,并可能有地幔岩浆的参与.结合区域变质、岩浆事件的综合研究成果,认为黄旗口不同期次的花岗岩具有造山带花岗岩的特征,分别形成于阴山地块和鄂尔多斯地块碰撞拼合以及造山后伸展的不同阶段.

       

    • 图  1  贺兰山中段黄旗口地区地质构造简图

      修改自宁夏国土资源调查监测院(2013,贺兰山中段1:5万区域地质调查成果报告);图a为华北克拉通构造单元划分简图,修改自Zhao et al.(2005),其中白框所示为工作区(东经105°45′~106°00′,北纬38°30′~38°40′)

      Fig.  1.  Geological sketch map of Huangqikou in central Helanshan area

      图  2  贺兰山中段黄旗口花岗岩野外特征

      a.野外早晚两期岩体接触界线;b.黄旗口岩体中的捕掳体;c.岩体中穿插的辉绿岩脉;d.大口子沟出露的石榴石花岗岩

      Fig.  2.  Field characteristics of the Huangqikou granites in central Helanshan

      图  3  贺兰山中段黄旗口花岗岩体岩相学特征

      a.石榴石花岗岩的镜下显微特征,1966-1;b.二长花岗岩中矿物组合:Q(石英)+Mi(微斜长石)+Pl(斜长石)+Bi(黑云母),401-13-2;c.英云闪长岩中矿物组合:Q(石英)+Pl(斜长石)+Bi(黑云母)+Ms(白云母),401-6-1

      Fig.  3.  Petrographic characteristics of the Huangqikou granites in central Helanshan

      图  4  贺兰山中段黄旗口和白杨沟岩体TAS图解

      底图据Middlemost(1994)

      Fig.  4.  Plot of SiO2 vs. Na2O+K2O of the Huangqikou and Baiyanggou granitic plutons in central Helanshan

      图  5  贺兰山中段黄旗口和白杨沟岩体的A/NK-A/CNK(a)和K2O-SiO2(b)关系

      图a据Maniar and Piccoli(1989), 图b据Rickwood(1989)

      Fig.  5.  Plots of A/CNK vs. A/NK (a) and SiO2 vs. K2O (b) of the Huangqikou and Baiyanggou granitic plutons in central Helanshan

      图  6  贺兰山中段黄旗口和白杨沟岩体主量元素哈克图解

      Fig.  6.  Harker diagrams of major elements of the Huangqikou and Baiyanggou granitic plutons in central Helanshan

      图  7  贺兰山中段黄旗口及白杨沟岩体稀土元素配分图(a,c)和微量元素蛛网图(b,d)

      球粒陨石、原始地幔数据引自Sun and McDonough(1989)

      Fig.  7.  Chondrite-normalized REE patterns (a, c) and primitive mantle-normalized spidergrams (b, d) for the Huangqikou and Baiyanggou granitic plutons in central Helanshan

      图  8  贺兰山中段黄旗口和白杨沟花岗岩的Rb/Ba-Rb/Sr图解

      其他样品数据来自Sylvester (1998)

      Fig.  8.  Plot of Rb/Ba vs. Rb/Sr of the granitic rocks from the Huangqikou and Baiyanggou area in central Helanshan

      表  1  贺兰山中段黄旗口和白杨沟岩体Sr-Nd同位素组成

      Table  1.   Sr and Nd isotopic compositions of the Huangqikou and Baiyanggou granitic plutons in central Helanshan

      样品编号 87Rb/86Sr 87Sr/86Sr (87Sr/86Sr)i 147Sm/144Nd 143Nd/144Nd εNd(t) TDM1(Ma) TDM2(Ma)
      D0509-1 早期岩体 4.700 0.831 67 6 0.692 84 0.131 7 0.511 982 7 4.35 2 162 2 146
      101-3-1 4.492 0.839 92 4 0.707 24 0.125 2 0.511 766 8 1.81 2 374 2 349
      401-2-1 4.458 0.814 90 5 0.683 22 0.125 8 0.511 879 5 3.89 2 194 2 183
      401-8-1 3.448 0.804 52 4 0.702 68 0.128 1 0.511 853 9 2.77 2 299 2 272
      401-10-1 3.246 0.785 58 4 0.689 71 0.107 6 0.511 685 7 4.90 2 097 2 102
      401-12-3 1.437 0.744 73 5 0.702 28 0.102 7 0.511 576 4 4.06 2 153 2 169
      101-7-2 晚期岩体 1.361 0.754 52 4 0.717 28 0.116 4 0.511 744 4 2.16 2 193 2 198
      101-4-1 5.906 0.842 90 6 0.681 40 0.129 3 0.511 933 8 2.69 2 190 2 156
      401-7-1 2.157 0.759 79 5 0.700 79 0.106 8 0.511 629 4 2.24 2 161 2 192
      D1514-4 白杨沟 1.028 0.761 76 6 0.731 39 0.1161 0.511 810 13 5.10 2 085 2 086
      D1514-13 3.381 0.771 21 5 0.671 35 0.1174 0.511 703 5 2.64 2 281 2 283
      注:(87Sr/86Sr)i=(87Sr/86Sr)S-(87Rb/86Sr)S× (eλt-1), λ=1.42×10-11 a-1; εNd(t)=[(143Nd/144Nd)S/(143Nd/144Nd)CHUR(t)-1]×104, TDM1=1/λ×ln{1+[((143Nd/144Nd)S-(143Nd/144Nd)DM)/((147Sm/144Nd)S-(147Sm/144Nd)DM)]}; TDM2=1/λ×ln{1+[(143Nd/144Nd)S-(143Nd/144Nd)DM-((147Sm/144Nd)S-(147Sm/144Nd)C)×(eλt-1)]/[(147Sm/144Nd)C-(147Sm/144Nd)DM]},公式中的下标S、CHUR、DM、C分别表示样品测量值、球粒陨石值、亏损地幔值、大陆地壳平均值,(143Nd/144Nd)DM=0.513 15,(147Sm/144Nd)DM=0.213 7,(147Sm/144Nd)C=0.118,λ=6.54×10-12 a-1t为岩浆结晶年龄,早期岩体为2.05 Ga,晚期岩体为1.90 Ga.
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    • 收稿日期:  2018-04-20
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