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南极横贯南极山脉休斯陡崖花岗质岩体的成因

崔迎春 马立杰 刘晨光 王庆超 LÄUFERAndreas

崔迎春, 马立杰, 刘晨光, 等, 2021. 南极横贯南极山脉休斯陡崖花岗质岩体的成因. 地质力学学报, 27 (5): 783-795. DOI: 10.12090/j.issn.1006-6616.2021.27.05.064
引用本文: 崔迎春, 马立杰, 刘晨光, 等, 2021. 南极横贯南极山脉休斯陡崖花岗质岩体的成因. 地质力学学报, 27 (5): 783-795. DOI: 10.12090/j.issn.1006-6616.2021.27.05.064
CUI Yingchun, MA Lijie, LIU Chenguang, et al., 2021. Petrogenesis of the Hughes Bluff granitic pluton in the Transantarctic Mountains, Antarctica. Journal of Geomechanics, 27 (5): 783-795. DOI: 10.12090/j.issn.1006-6616.2021.27.05.064
Citation: CUI Yingchun, MA Lijie, LIU Chenguang, et al., 2021. Petrogenesis of the Hughes Bluff granitic pluton in the Transantarctic Mountains, Antarctica. Journal of Geomechanics, 27 (5): 783-795. DOI: 10.12090/j.issn.1006-6616.2021.27.05.064

南极横贯南极山脉休斯陡崖花岗质岩体的成因

doi: 10.12090/j.issn.1006-6616.2021.27.05.064
基金项目: 

国家自然科学基金 91958216

国家自然科学基金 41876227

极地考察业务化与科研 JD0620010

极地考察业务化与科研 JD0620020

详细信息
    作者简介:

    崔迎春(1976-), 男, 博士, 高级工程师, 矿物学、岩石学、矿床学专业。E-mail: cuiyingchun@fio.org.cn

  • 中图分类号: P581

Petrogenesis of the Hughes Bluff granitic pluton in the Transantarctic Mountains, Antarctica

Funds: 

the National Natural Science Foundation of China 91958216

the National Natural Science Foundation of China 41876227

the projects of Polar Operation and Scientific Research JD0620010

the projects of Polar Operation and Scientific Research JD0620020

  • 摘要: 为了探讨横贯南极山脉休斯陡崖花岗质岩体的岩石成因,对其开展了岩相学和岩石化学分析。结果表明,休斯陡崖岩体主体岩石为二长花岗岩,后期被细粒二长花岗岩岩脉侵入。二者都具有高硅、富碱和高钾特征,里特曼指数小于3,岩石铝饱和指数(A/CNK)值小于1;微量元素原始地幔标准化分布型式具有Rb、Th、U和K元素富集,Nb、Ta、Nd和Ti等元素亏损特征;稀土元素总量偏低,轻稀土富集。主期二长花岗岩的稀土元素球粒陨石标准化分布型式具有轻微的负Eu异常,而岩脉具有正的Eu异常。休斯陡崖岩体的岩石类型为钙碱性准铝质I型花岗岩,源区为下陆壳,并伴有幔源物质的混入。在源区,岩浆发生了不同程度的斜长石、钛铁矿、金红石和磷灰石的分离结晶作用,其形成的构造环境为与俯冲作用有关的火山岛弧环境。

     

  • 图  1  休斯陡崖区域地质简图及地貌特征

    a-南极北维多利亚地地质构造图(底图据Ferraccioli and Bozzo, 1999; Läufer et al., 2005修改);b-休斯陡崖采样位置;c、d-采样点地貌特征

    Figure  1.  The generalized geologic map and geomorphic features of the Hughes Bluff region

    (a) Geological sketch map of Northern Victoria Land, Antarctica (modified after Ferraccioli & Bozzo, 1999; Läufer et al., 2005); (b) Sampling locations in the Hughes Bluff region; (c and d)Geomorphic features of the sampling locations

    图  2  休斯陡崖岩体二长花岗岩及二长花岗岩脉野外露头接触关系及显微照片

    Qtz-石英;Pl-斜长石;Bt-黑云母;Chl-绿泥石;Cb-碳酸盐矿物
    a-35LC108-2样品宏观照片;b-二长花岗岩(35LC108-2)显微照片(正交偏光);c-二长花岗岩与细粒二长花岗岩脉野外照;d-35LC108-3样品宏观照片;e-细粒二长花岗岩(35LC108-3)显微照片(正交偏光)

    Figure  2.  Outcrop and photomicrographs of the Hughes Bluff pluton

    (a)Photograph of the sample 35LC108-2; (b) Photomicrograph of the monzogranite sample 35LC108-2 (crossed-polarized light); (c)Photograph of the outcrop of monzogranite and dyke; (d) Photograph of the sample 35LC108-3; (e) Photomicrograph of the fine-grained monzogranite sample 35LC108-3 (crossed-polarized light)
    Qtz-quartz; Pl-plagioclase; Bt-biotite; Chl-chlorite; Cb-carbonate

    图  3  休斯陡崖岩体稀土元素球粒陨石标准化配分模式图与微量元素原始地幔标准化蛛网图(球粒陨石和原始地幔数据据Sun and McDonough, 1989)

    a-微量元素原始地幔标准化蛛网图;b-稀土元素球粒陨石标准化配分模式图

    Figure  3.  Primitive mantle (PM) normalized spider diagram (a) and chondrite-normalized REE pattern (b) for the Hughes Bluff pluton (Chondrite and PM values used for normalization are from Sun and McDonough, 1989)

    图  4  休斯陡崖花岗岩成因类型判别图解

    a-休斯陡崖花岗质样品的(K2O+Na2O)/CaO-(Zr+Nb+Ce+Y)图解(底图据Whalen et al., 1987);b-休斯陡崖花岗质样品的TiO2-Zr图解(底图据刘洪等, 2016)

    Figure  4.  Petrogenesis discrimination diagrams for the Hughes Bluff granitic pluton

    (a) (K2O+Na2O)/CaO-(Zr+Nb+Ce+Y) diagram (modified after Whalen et al., 1987); (b) TiO2-Zr diagram (modified after Liu et al., 2016)

    图  5  休斯陡崖岩体微量元素构造环境判别图

    ORG-大洋中脊花岗岩;WPG-板内花岗岩;VAG-火山弧花岗岩;Syn-CLOG-同碰撞花岗岩;Post-CLOG-后碰撞花岗岩
    a-Y-Nb构造环境判别图(底图据Pearce et al., 1984);b-(Y+Nb)-Rb构造环境判别图(底图据Pearce, 1996)

    Figure  5.  Diagrams showing the tectonic setting of Y-Nb(a) and (Y+Nb)-Rb(b) for the Hughes bluff pluton (a after Pearce et al., 1984; b after Pearce, 1996)

    ORG-oceanic ridge granites; WPG-within-plate granites; VAG-volcanic arc granites; Syn-CLOG-syncollisional granites; Post-CLOG-postcollisional granites

    表  1  休斯陡崖岩体主量元素分析结果

    Table  1.   Major element results of the Hughes Bluff pluton

    主量元素含量/% SiO2 TiO2 Al2O3 Fe2O3 MnO MgO CaO Na2O K2O P2O5 LOI 总和 Mg# 石英 斜长石 正长石 刚玉 透辉石 紫苏辉石 钛铁矿 磁铁矿 磷灰石
    35LC108-2 70.5 0.35 14.00 2.43 0.04 0.87 2.01 3.86 4.42 0.48 0.84 99.8 41.55 25.55 40.22 26.71 0.64 0.00 3.95 0.53 0.29 0.83
    35LC108-3 74.47 0.12 13.36 1.53 0.02 0.22 1.63 4.06 4.17 0.11 0.64 100.33 22.28 30.92 40.45 24.76 0.00 1.28 1.88 0.23 0.22 0.25
    35LC108-4 71.20 0.28 14.00 1.94 0.04 0.62 1.49 4.07 4.44 0.35 0.61 99.04 38.92 25.87 40.00 26.48 0.36 0.00 5.14 0.66 0.36 1.14
    注:矿物含量来自于CIPW标准矿物的计算结果;Mg#=100×Mg2+/(Mg2++Fe2+)
    下载: 导出CSV

    表  2  休斯陡崖岩体微量元素分析结果

    Table  2.   Trace element results of the Hughes Bluff pluton

    微量元素含量/×10-6 Ba Sr Zn Zr Li Be Sc V Cr Co Ni Cu Ga Ge Rb Y Nb Mo Cd Cs Hf Ta W Tl Pb Bi Th U
    35LC108-2 1231.89 625.32 48.06 179.72 36.12 2.91 2.48 9.45 1.06 2.54 0.8 4.19 19.17 0.84 133.03 10.14 11.64 0.78 - 2.07 4.76 1.24 0.27 0.84 23.67 0.03 14.55 2.14
    35LC108-3 1124.32 369.72 28.62 112.33 26.15 2.15 1.21 2.17 0.44 0.96 0.27 0.65 13.29 0.92 138.87 8.42 6.19 4.60 0.02 1.85 3.16 0.71 0.33 0.71 37.77 0.03 10.32 2.00
    35LC108-4 1172.63 521.56 52.35 178.86 27.12 2.52 1.59 8.29 1.36 2.37 0.55 0.41 17.16 0.99 149.48 8.98 9.99 0.11 0.02 4.20 4.90 0.79 0.28 0.69 30.40 0.03 17.46 2.61
    注:-低于检测限
    下载: 导出CSV

    表  3  休斯陡崖岩体稀土元素分析结果

    Table  3.   Rare earth element results of the Hughes Bluff pluton

    稀土元素含量/×10-6 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu ΣREE LaN/YbN EuN
    35LC108-2 32.89 58.20 6.27 20.49 3.24 0.79 2.39 0.30 1.51 0.32 0.90 0.16 1.15 0.17 128.76 19.36 0.83
    35LC108-3 25.04 41.73 4.47 14.76 2.27 0.75 1.80 0.25 1.41 0.30 0.89 0.15 1.08 0.17 95.05 15.71 1.10
    35LC108-4 29.47 54.01 5.81 19.97 3.30 0.70 2.50 0.33 1.68 0.32 0.88 0.13 0.84 0.13 120.06 23.70 0.72
    下载: 导出CSV
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  • 收稿日期:  2021-05-30
  • 修回日期:  2021-08-30
  • 预出版日期:  2021-12-31
  • 刊出日期:  2021-10-28

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