• 中文核心期刊
  • 中国科技核心期刊
  • 中国科学引文数据库核心期刊

柴北缘布赫特山一带达肯大坂岩群变质岩变形特征、地球化学特征及地质意义

王洪强, 邵铁全, 唐汉华, 姜开拓

王洪强, 邵铁全, 唐汉华, 姜开拓. 2016: 柴北缘布赫特山一带达肯大坂岩群变质岩变形特征、地球化学特征及地质意义. 地质通报, 35(9): 1488-1496.
引用本文: 王洪强, 邵铁全, 唐汉华, 姜开拓. 2016: 柴北缘布赫特山一带达肯大坂岩群变质岩变形特征、地球化学特征及地质意义. 地质通报, 35(9): 1488-1496.
WANG Hongqiang, SHAO Tiequan, TANG Hanhua, JIANG Kaituo. 2016: Metamorphic rock deformation characteristics, geochemical characteristics and geological significance of the Dakendaba Group in Buhete Mountain on the northern margin of Qaidam Mountain. Geological Bulletin of China, 35(9): 1488-1496.
Citation: WANG Hongqiang, SHAO Tiequan, TANG Hanhua, JIANG Kaituo. 2016: Metamorphic rock deformation characteristics, geochemical characteristics and geological significance of the Dakendaba Group in Buhete Mountain on the northern margin of Qaidam Mountain. Geological Bulletin of China, 35(9): 1488-1496.

柴北缘布赫特山一带达肯大坂岩群变质岩变形特征、地球化学特征及地质意义

基金项目: 

青海省国土资源厅项目 中铝基金200904

详细信息
    作者简介:

    王洪强(1986-), 男, 硕士, 助理工程师, 从事区域地质调查工作。E-mail:372223985@qq.com

  • 中图分类号: P534.3;P588.3

Metamorphic rock deformation characteristics, geochemical characteristics and geological significance of the Dakendaba Group in Buhete Mountain on the northern margin of Qaidam Mountain

  • 摘要:

    古元古代达肯大坂岩群为柴北缘构造带的变质结晶基底,是柴北缘造山带的重要组成部分。前人在德令哈以西的鱼卡河-锡铁山-沙柳河一带和大柴旦等地对达肯大坂岩群做了较深入的研究,但对于柴北缘东段的研究还相对薄弱,缺乏东西段的对比研究。通过对布赫特山一带达肯大坂岩群中片麻岩和斜长角闪片岩的岩石学、岩石地球化学、年代学研究和区域对比,认为研究区的岩性、矿物组合、变质程度与德令哈以西鱼卡河-锡铁山-沙柳河一带达肯大坂岩群具有较高的相似性。布赫特山一带达肯大坂岩群主要为一套碎屑岩夹火山岩的岩石组合,变形强烈,其形成环境为岛弧与活动性陆缘的过渡环境,且岩浆来源为壳幔混染。由采集的2件Sm-Nd同位素样品得到了2组等时线年龄分别为2085±14Ma和2027±19Ma。由此可知达肯大坂岩群为古元古代柴北缘地区的变质结晶基底,是柴北缘古元古代造山带的重要组成部分。

    Abstract:

    The Proterozoic Dakendaban Group is the metamorphic crystalline basement of the northern margin tectonic belt and is an important part of the orogenic belt on the northern margin of Qaidam Basin. Previous researchers have made in-depth studies of Dakendaban Group in the areas of Delingha to the west of the Yuka River-Xitieshan-Shaliu River and Da Qaidam, but the study of the east part of the northern Qaidam is relatively insufficient, with the lack of comparative study of the east part and the west part. The authors made meticulous researches on petrology, geochemistry and geochronology of gneiss and amphibolite hornblende schist in Dakendaban Group of Buhete Mountain. Regional correlation shows that the lithologies, mineral assemblage, and metamorphism in the study area are quite similar to things of Dakendaban Group in the west of Delingha Yuka River-Xitieshan-Shaliu River area. Dakendaban Group of Buhete Mountain is mainly a clastic rock intercalated with volcanic rock assemblage, with intense deformation. The environment was a transitional environment of island arc and active continental border, and the magma source experienced crust mantle contamination. Two Sm-Nd isotope samples yielded two groups of isochronal ages, i.e., 2085±14Ma and 2027±19Ma. It is thus concluded that the Dakendaban Group is Paleoproterozoic metamorphic crystalline basement on the northern margin of Qaidam Basin and is an important part of the Paleoproterozoic orogenic belt in northern Qaidam Basin.

  • 致谢: 参加本项研究工作的还有长安大学地球科学与资源学院许安东副教授、陕西区域地质矿产研究院王振东高级工程师,审稿人对本文的评阅和赐教使笔者受益匪浅,在此一并表示衷心的感谢。
  • 图  1   研究区构造位置[5]

    Figure  1.   Tectonic position of the study area

    图  2   研究区地质简图

    Figure  2.   Geological map of the study area

    图  3   片麻岩中的顺层掩卧褶皱

    Figure  3.   Bedding recumbent folds of gneiss

    图  4   掩卧褶皱(a)和勾状褶皱(b)

    Figure  4.   Bedding recumbent folds (a) and hook shaped fold(b)

    图版Ⅰ   a、b.旋转碎斑;c.波状消光;d.雁行状排列;e.顺层掩卧褶皱;f.无根勾状褶皱;g.糜棱岩;h.共轭X形剪节理

    图  5   球粒陨石标准化稀土元素配分曲线和原始地幔标准化元素蛛网图[13]

    Figure  5.   Seawater-normalized REE patterns and MORB-normalized trace element patterns

    图  6   Th-Hf-Nb图解[14]

    A—N-MORB;B—E-MORB和板内拉斑玄武岩;C—碱性板内玄武岩;D—岛弧拉斑玄武岩

    Figure  6.   Diagram of Th-Hf-Nb

    图  7   Sm-Nd样品等时线图

    L1等时线年龄T=2085±14Ma,Ii=0.510305,εNd(T)=7.2,MSWD=0.13;L2等时线年龄T=2027±19Ma,Ii=0.510246,εNd(T)=4.6,MSWD=0.89

    Figure  7.   Sm-Nd sample isochron chart

    表  1   达肯大坂岩群岩石化学分析结果

    Table  1   Analytical results of petrochemistry of Dakendaban Group

    样号 薄片定名 SiO2 Al2O3 Fe2O3 FeO CaO MgO K2O NazO TiO2 P2O5 MnO Total La Ce
    Ⅳ-31 角闪斜长变粒岩 59.9 13.08 1.08 4.28 13.23 2.97 3.72 0.79 0.54 0.1 0.32 100.01 43.93 89.73
    Ⅳ-42/1 黑云斜长片麻岩 52.16 14.52 1.25 10.5 10.95 7.17 0.56 1.6 0.98 0.08 0.21 99.98 10.51 25.37
    Ⅳ-58 黑云二长片麻岩 74.56 14.14 0.05 1.4 1.18 0.3 4.71 3.26 0.19 0.15 0.06 100 16.3 34.86
    Ⅳ-59 黑云斜长片麻岩 74.1 14.27 0.1 2.03 1.6 1.21 3.2 2.98 0.36 0.1 0.05 100 43.27 95.81
    Ⅳ-42 斜长角闪岩 48.07 14.18 2.5 12.95 9.99 7.17 0.55 2.17 1.97 0.18 0.25 99.98 10.12 23.07
    样号 Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Rb Sr Y
    Ⅳ-31 10.64 42.26 7.678 1.278 8.451 1.099 6.656 1.275 3.891 0.54 3.825 0.553 143.6 467.8 33.68
    Ⅳ-42/1 3.409 16.56 4.49 1.385 6.075 0.959 6.489 1.327 3.951 0.538 3.862 0.553 27.89 114.1 32.92
    Ⅳ-58 3.897 14.41 2.853 0.393 3.295 0.535 4.182 0.963 3.319 0.527 4.027 0.589 239.5 87.54 25.34
    Ⅳ-59 10.63 40.78 7.742 0.76 8.339 1.113 6.634 1.257 3.788 0.512 3.507 0.492 107.9 69.57 33.8
    Ⅳ-42 3.069 14.51 3.824 1.248 4.986 0.742 4.988 1.018 3.047 0.404 2.849 0.414 33.41 155.3 24.92
    样号 Zr Nb Cd In Cs Ba Hf Ta Pb Th U I REE δEu (La/Yb)N (La/Sm)N
    Ⅳ-31 202.4 13.82 0.37 0.09 10.81 391.6 5.56 0.98 22.25 15.28 3.05 221.81 0.48 7.76 3.6
    Ⅳ-42/1 107.5 7.33 0.28 0.1 2.41 88.91 3 0.41 4.21 2.02 0.56 85.48 0.81 1.84 1.47
    Ⅳ-58 67.21 8.05 0.09 0.06 1.57 244.1 2.02 0.53 26.25 4.2 3.87 90.15 0.39 2.74 3.6
    Ⅳ-59 151.3 21.32 0.23 0.05 1.83 341.1 4.24 2 23.84 26.35 6.53 224.63 0.29 8.34 3.52
    Ⅳ-42 94.52 7.47 0.33 0.09 2.37 107.9 2.57 0.4 6.76 1.82 0.59 74.29 0.87 2.4 1.67
    注:所有样品均由西安地质矿产研究所实验测试中心测试,主量元素含量单位为%,稀土及微量元素为10-6
    下载: 导出CSV

    表  2   Sm-Nd样品测试结果

    Table  2   Sm-Nd sample test results

    编号 Sm/10-6 Nd/10-6 l47Sm/l44Nd 143Nd/144Nd
    09SG.Sm-Nd2-Ⅳ-38 2.8736 9.5154 0.1826 0.512682 ±2
    09SG.Sm-Nd2-Ⅳ-38/l 2.7092 8.3512 0.1961 0.512997 ±3
    09SG.Sm-Nd2-Ⅳ-42 2.5765 10.0349 0.1552 0.512316 ±6
    09SG.Sm-Nd2-Ⅳ-42/l 2.l4l7 8.0833 0.1602 0.512385 ±3
    09SG.Sm-Nd2-V-42/2 2.06l2 7.3676 0.1691 0.512502 ±3
    09SG.Sm-Nd2-V-42/3 4.7357 16.9831 0.1686 0.512620 ±3
    09SG.Sm-Nd2-V-42/4 2.9693 11.2004 0.1603 0.512505 ±3
    09SG.Sm-Nd2-V-60 12.6972 59.2546 0.1295 0.512083 ±5
    注:天津地质矿产研究所测试
    下载: 导出CSV
  • 青海省地质矿产局.青海省区域地质志[M].北京:地质出版社, 1991:1-662.
    张雪亭, 杨生德.青海省区域地质概论[M].北京:地质出版社, 2007.
    孙崇仁.青海省岩石地层[M].武汉:中国地质大学出版社, 1997.
    辛后田, 郝国杰, 王惠初, 等.柴北缘前震旦纪地层系统的新认识[J].前寒武纪研究进展, 2002, 6:113-118. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200202007.htm
    辛后田, 王惠初, 周世军.柴北缘的大地构造演化及其地质事件群[J].地质调查与研究, 2006, 12:311-320. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200604010.htm
    李怀坤, 陆松年, 赵风清, 等.柴达木北缘新元古代重大地质事件年代格架[J].现代地质, 1999, 2:224-225. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ902.036.htm
    李怀坤, 陆松年, 李惠民, 等.侵入下马岭组的基性岩床的锆石和斜锆石U-Pb精确定年——对华北中元古界地层划分方案的制约[J].地质通报, 2009, 28(10):1396-1404. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20091005&journal_id=gbc
    郝国杰, 陆松年, 王惠初, 等.柴达木盆地北缘前泥盆纪构造格架及欧龙布鲁克古陆块地质演化[J].地学前缘, 2004, 9:115-122. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403016.htm
    潘桂堂, 肖庆辉, 陆松年, 等.中国大地构造单元划分[J].中国地质, 2009, 2:1-28. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200901004.htm
    王惠初, 陆松年, 莫宣学, 等.柴达木盆地北缘早古生代碰撞造山系统[J].地质通报, 2005, 7:603-612. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=200507123&journal_id=gbc
    王惠初, 李怀坤, 陆松年, 等.柴北缘鱼卡地区达肯大坂岩群的地质特征与构造环境[J].地质调查与研究, 2006, 12:253-262. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200604003.htm
    田琪.柴达木盆地北缘东段阿尔茨托山一带达肯大坂岩群变形特征[J].青海地质, 1999, 2:39-46. http://www.cnki.com.cn/Article/CJFDTOTAL-GTJL199902007.htm
    Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[C]//Sauders A D, Norry M J. Magmatism in the Ocean Basins. Spec. Publ. Geol. Soc. Lond., 1989, 42:313-345.

    Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[C]//Sauders A D, Norry M J. Magmatism in the Ocean Basins. Spec. Publ. Geol. Soc. Lond., 1989, 42:313-345.

    Wood D A. The application of a Th-Hf-Ta diagram to problems of tectonic magmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province[J]. Earth Planet. Sci. Lett., 1980, 50:1130.

    Wood D A. The application of a Th-Hf-Ta diagram to problems of tectonic magmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province[J]. Earth Planet. Sci. Lett., 1980, 50:1130.

    杨学明, 杨晓勇, 陈双喜, 等.岩石地球化学[M].合肥:中国科学技术大学出版社, 2000.
    陆松年, 王惠初, 李怀坤, 等.柴达木盆地北缘"达肯大坂群"的再厘定[J].地质通报, 2002, 21(1):19-23. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20020106&journal_id=gbc
    李彦强, 雷爱全, 段建华.天峻县黑水河地区古元古代达肯大坂岩群区域变质岩的发现及其地质意义[J].学术前沿, 2009, 2:36-41. http://www.cnki.com.cn/Article/CJFDTOTAL-GTJL200902019.htm
    王勤燕, 陈能松, 李晓彦, 等.全吉地块基底达肯大坂岩群和热事件的LA-ICPMS锆石U-Pb定年[J], 科学通报2008, 7:1693-1701.
    黄婉, 张璐, 巴金, 等.柴达木地块北缘全吉地块钾长石浅粒岩碎屑锆石LA-ICP-MS U-Pb定年——对达肯大坂岩群时代的约束[J].地质通报, 2011, 30(9):1353-1359. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20110903&journal_id=gbc
图(8)  /  表(2)
计量
  • 文章访问数:  2376
  • HTML全文浏览量:  384
  • PDF下载量:  152
  • 被引次数: 0
出版历程
  • 收稿日期:  2016-04-30
  • 修回日期:  2016-06-26
  • 网络出版日期:  2023-08-16
  • 刊出日期:  2016-08-31

目录

    /

    返回文章
    返回