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东昆仑东段阿拉思木辉长岩锆石U-Pb年代学、地球化学特征及洋盆闭合时限界定

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张玉, 裴先治, 李瑞保, 刘成军, 陈有炘, 李佐臣, 王兴, 胡晨光, 颜全治, 彭思钟. 2017. 东昆仑东段阿拉思木辉长岩锆石U-Pb年代学、地球化学特征及洋盆闭合时限界定[J]. 中国地质, 44(3): 526-540. doi: 10.12029/gc20170310
引用本文: 张玉, 裴先治, 李瑞保, 刘成军, 陈有炘, 李佐臣, 王兴, 胡晨光, 颜全治, 彭思钟. 2017. 东昆仑东段阿拉思木辉长岩锆石U-Pb年代学、地球化学特征及洋盆闭合时限界定[J]. 中国地质, 44(3): 526-540. doi: 10.12029/gc20170310
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ZHANG Yu, PEI Xianzhi, LI Ruibao, LIU Chenjun, CHEN Youxin, LI Zuochen, WANG Xin, HU Chenguang, YAN Quanzhi, PENG Sizhong. 2017. Zircon U-Pb geochronology, geochemistry of the Alasimu gabbro in eastern section of East Kunlun Mountains and the closing time of Paleo-ocean basin[J]. Geology in China, 44(3): 526-540. doi: 10.12029/gc20170310
Citation: ZHANG Yu, PEI Xianzhi, LI Ruibao, LIU Chenjun, CHEN Youxin, LI Zuochen, WANG Xin, HU Chenguang, YAN Quanzhi, PENG Sizhong. 2017. Zircon U-Pb geochronology, geochemistry of the Alasimu gabbro in eastern section of East Kunlun Mountains and the closing time of Paleo-ocean basin[J]. Geology in China, 44(3): 526-540. doi: 10.12029/gc20170310
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东昆仑东段阿拉思木辉长岩锆石U-Pb年代学、地球化学特征及洋盆闭合时限界定

  • 1.

    长安大学 地球科学与资源学院, 陕西 西安 710054

  • 2.

    长安大学 西部矿产资源与地质工程教育部重点实验室, 陕西 西安 710054

  • 基金项目: 国家自然科学基金项目（41472191、41502191、41172186、310827161006）、中央高校基本科研业务费专项资金项目（CHD2011TD020、2013G1271091、2013G1271092）和青海省国土资源厅-中国铝业公司公益性区域地质矿产调查基金项目（中铝基金200801）联合资助
详细信息
    作者简介: 张玉, 男, 1991年生, 硕士生, 构造地质学专业, E-mail:2211461032@qq.com
    通讯作者: 裴先治, 男, 1963年生, 教授, 博士生导师, 从事构造地质学和区域地质学研究, E-mail:peixzh@263.net

  • 中图分类号: P597+.3;P595

Zircon U-Pb geochronology, geochemistry of the Alasimu gabbro in eastern section of East Kunlun Mountains and the closing time of Paleo-ocean basin

  • 1.

    School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China

  • 2.

    Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China

  • Fund Project: Supported by the National Science Foundation of China (No. 41472191, 41502191, 41172186); the Special Fund for Basic Scientific Research of Central Colleges, Chang`an University (Nos. CHD2011TD020, 2013G1271091, 2013G1271092); the Commonweal Geological Survey, the Aluminum Corporation of Chian and the Land-Resources Department of Qinghai Province (No. 200801)
More Information
    Author Bio: ZHANG Yu, male, born in 1991, master candidate, majors in structural geology; E-mail: 2211461032@qq.com .
    Corresponding author: PEI Xianzhi, male, born in 1963, doctor, supervisor of doctor candidates, mainly engages in the study of structural geology and regional geology; E-mail: peixzh@263.net

    摘要

  • 东昆仑东段广泛分布晚古生代的中酸性花岗岩，基性岩浆岩记录较少。本文选择位于东昆仑北弧岩浆岩带南缘的阿拉思木基性岩进行研究，为东昆仑东段晚古生代岩浆演化研究提供新的依据。通过LA-ICP-MS锆石U-Pb定年方法获得阿拉思木基性岩形成年龄为（241±1）Ma，为中三叠世岩浆活动的产物。岩石地球化学特征显示岩石具有低TiO2（0.17%~0.37%，平均值0.25%）和较高的Mg#值（72.94~77.32，平均值为74.95）及Al2O3值（13.08~23.20%，平均值18.9%），富集大离子亲石元素（LILE：Sr、Rb、Ba），明显亏损高场强元素（HFSE：Nb、Ta、Zr、Hf）。Harker图解表明，MgO与Fe2O3T、TiO2、Ni、Co呈明显的正相关，暗示阿拉思木基性岩浆在形成过程中有一定程度的橄榄石、钛铁氧化物的分离结晶。阿拉思木辉长岩具有岛弧玄武岩的地球化学特征，并且其结晶年龄明显早于东昆仑碰撞及后碰撞构造岩浆时限。综合区域地质资料认为，阿拉思木辉长岩可能代表了东昆仑地区中三叠世洋壳俯冲的最晚期岩浆记录，进而确定东昆仑古特提斯洋俯冲结束碰撞开始的时间可能为中三叠世。

    Late Paleozoic intermediate-acid granitoids are widely distributed in the East Section of East Kunlun, but the records of basic magmatism are very insufficient. Alasimu mafic rocks on the southern margin of the arc magmatic rock belt in northern East Kunlun Mountains was selected as the study objective so as to provide a new basis for the research on the Late Paleozoic magmatic evolution of the east section of East Kunlun Mountains. LA-ICP-MS zircon U-Pb analysis yielded the crystallization age of 241±1Ma, suggesting that Alasimu Mafic rocks were formed in the Middle Triassic. All the rock samples are characterized by relatively low TiO2 (0.17%-0.37%, averagely 0.25%) and high Mg# (72.94%-77.32%, averagely 74.95%) and high Al2O3 (13.08%-23.20%, averagely 18.9%), enrichment of large ion lithophile elements (LILE:Sr, Rb, Ba), apparent depletion of high field strength elements (HFSE, Nb, Ta, Zr and Hf). MgO shows some correlation with Fe2O3T, TiO2, Ni and Co in the diagram of Harker, which reveals some degree of fractional crystallization of olivine and Ti-Fe oxide. Alasimu mafic rocks have similar chemical composition to island arc basalts, and they formed earlier than the collision and post-collision time of tectonic-magmatic activity. Combined with regional studies, the authors hold that Alasimu gabbro rocks ought to be the latest magmatism records in the East Kunlun region related to Middle Triassic Paleo Tethys oceanic crust subduction, which indicated that the tectonic transition from ocean subduction to collisional orogeny might have commenced in Middle Triassic.

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  • 图 1  东昆仑东段巴隆地区地质简图

    Figure 1. 

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    图 2  阿拉思木辉长岩手标本及镜下显微照片

    Figure 2. 

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    图 3  阿拉思木辉长岩典型锆石CL图像与表面年龄

    Figure 3. 

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    图 4  阿拉思木辉长岩锆石U-Pb谐和年龄和加权平均年龄图

    Figure 4. 

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    图 5  阿拉思木辉长岩岩石分类图

    Figure 5. 

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    图 6  阿拉思木辉长岩的Harker图解

    Figure 6. 

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    图 7  阿拉思木辉长岩球粒陨石标准化稀土元素配分曲线(a）和原始地幔标准化微量元素蛛网图(b）

    Figure 7. 

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    图 8  阿拉思木辉长岩Th/Nb-Ba/Th图解(a，据Hanyu et al.，2006）、Th/Yb-Ba/La图解(b，据Woodhead et al.，2001）和Th/Yb-Nb/ Yb图解(c，据Pearce et al.，2008）

    Figure 8. 

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    图 9  阿拉思木辉长岩La/Nb-La图解(a，据李曙光等，1993）和Ti-V图解(b，据Shervais.，1982）

    Figure 9. 

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    图 10  东昆仑地区晚古生代—早中生代沉积-构造-岩浆演化简图(据李瑞保等，2012修改）

    Figure 10. 

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    表 1  阿拉思木辉长岩(XRD165/4）中锆石LA-ICP-MS U-Pb同位素年龄分析数据

    Table 1.  U-Pb isotopic composition of zircons in Alasimu gabbro (XRD164/4) measured by using LA-ICP-MS technique

    下载: 导出CSV

    表 2  阿拉思木辉长岩主量(%）、微量和稀土元素(10-6）分析结果

    Table 2.  Major (%) and trace (10-6) elements analyses of Alasimu gabbro

    下载: 导出CSV
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收稿日期:  2016-04-22
修回日期:  2016-06-02
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