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西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束

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徐盛林, 陈宣华, 李廷栋, 丁伟翠, 史建杰, 李冰, 马飞宙. 2019. 西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束[J]. 中国地质, 46(5): 1061-1078. doi: 10.12029/gc20190508
引用本文: 徐盛林, 陈宣华, 李廷栋, 丁伟翠, 史建杰, 李冰, 马飞宙. 2019. 西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束[J]. 中国地质, 46(5): 1061-1078. doi: 10.12029/gc20190508
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XU Shenglin, CHEN Xuanhua, LI Tingdong, DING Weicui, SHI Jianjie, LI Bing, MA Feizhou. 2019. Time of the ocean-continent transition in West Junggar: Constraints from zircon U-Pb dating and Lu-Hf isotopic composition[J]. Geology in China, 46(5): 1061-1078. doi: 10.12029/gc20190508
Citation: XU Shenglin, CHEN Xuanhua, LI Tingdong, DING Weicui, SHI Jianjie, LI Bing, MA Feizhou. 2019. Time of the ocean-continent transition in West Junggar: Constraints from zircon U-Pb dating and Lu-Hf isotopic composition[J]. Geology in China, 46(5): 1061-1078. doi: 10.12029/gc20190508
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西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束

  • 1.

    中国地质科学院, 北京 100037

  • 2.

    中国地质大学(北京)地球科学与资源学院, 北京 100083

  • 3.

    中国地质调查局, 北京 100037

  • 基金项目:
    中国地质调查局地质调查项目（DD20160083、DD20190011、DD20160344-05）、中央级公益性科研院所基本科研业务费项目（CAGS-YWF201706）和国家重点研发计划项目（2018YFC0603700）联合资助
详细信息
    作者简介: 徐盛林, 男, 1991年生, 博士, 构造地质学专业, 从事构造地质学、岩石地球化学研究工作; E-mail:xushenglindizhi@163.com
    通讯作者: 陈宣华, 男, 1967年生, 研究员, 博士生导师, 主要从事深地探测研究; E-mail:xhchen@cags.ac.cn

  • 中图分类号: P597;P542

Time of the ocean-continent transition in West Junggar: Constraints from zircon U-Pb dating and Lu-Hf isotopic composition

  • 1.

    Chinese Academy of Geological Sciences, Beijing 100037, China

  • 2.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 3.

    China Geological Survey, Beijing 100037, China

  • Fund Project: Supported by China Geological Survey Program(No. DD20160083, DD20160344-05 and DD20190011), Fundamental Research Funds for Central Public Welfare Research Institutes (No. CAGS-YWF201706) and National Key Research and Development Program of China (No. 2018YFC0603701)
More Information
    Author Bio: XU Shenglin, male, born in 1991, doctor, majors in structural geology, engages in research on tectonics and geochemistry; E-mail: xushenglindizhi@163.com .
    Corresponding author: CHEN Xuanhua, male, born in 1967, professor, supervisor of doctor candidates, engages in deep earth exploration; E-mail: xhchen@cags.ac.cn

    摘要

  • 中亚造山带西部的西准噶尔地区是古生代洋陆构造转换最显著的地区之一，但是关于该地区洋陆转换的具体时间和地壳演化至今仍存在诸多争议。本文以西准噶尔地区的庙尔沟岩体及其西北侧新发现的柱状节理流纹岩为研究对象，通过锆石U-Pb定年的方法，判断庙尔沟岩体的年龄为302.8~308.8 Ma，柱状节理流纹岩的年龄为303.6~294.5 Ma。锆石Lu-Hf同位素测试结果显示，庙尔沟岩体和柱状节理流纹岩都具有相似的高176Hf/177Hf值和高正εHf（t）值，具有亏损地幔的源区属性，可能来源于下地壳底部残余洋壳或火山岛弧等新生地壳发生部分熔融。结合区域地质资料和前人研究成果，将西准噶尔地区由大洋俯冲向陆内环境转变的时间限定为晚石炭-早二叠世，其基底可能是以新元古代晚期-晚古生代形成的年轻洋壳和岛弧为主，不存在古老的结晶基底。

    The West Junggar area of the western Central Asian Orogenic Belt is one of the most typical regions related to transition from the ocean to the continent in the late Paleozoic. It is still controversial about the specific time of ocean-continent transition and the continental growth of the West Junggar area at present. This paper reports zircon U-Pb age and zircon Lu-Hf isotope analytical results from the Miaoergou batholith and the newly discovered columnar jointed rhyolites on the northwest side of the Miaoergou batholith, West Junggar area. The zircon U-Pb ages indicate that the Miaoergou granitoids were formed at 302.8~308.8 Ma and the columnar jointed rhyolites were formed at 303.6~294.5 Ma, which indicates that the specific time of ocean-mainland transformation of the West Junggar area is limited to the Late Carboniferous-Early Permian. The zircon Lu-Hf isotope analytical results show that the Miaoergou granitoids and rhyolites have some similar characteristics in 176Hf/177Hf ratios and εHf(t) values. High 176Hf/177Hf ratios and εHf(t) values, similar to features of depleted mantle in nature, suggest that they resulted from partial melting of juvenile crust. Integrating regional geological data and previous research, the authors have reached the conclusion that the basement of West Junggar area was composed of juvenile oceanic crust and island arc which grew from late Neoproterozoic to late Paleozoic, with no old crystalline basement.

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  • 图 1  西准噶尔地区地质构造与采样位置图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  庙尔沟岩体与柱状节理流纹岩野外产出特征

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  庙尔沟花岗岩和流纹岩锆石CL图像

    Figure 3. 

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    图 4  庙尔沟花岗岩类和流纹岩U-Pb测年谐和图

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  庙尔沟花岗岩类与流纹岩锆石Hf同位素特征

    Figure 5. 

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    图 6  西准噶尔晚石炭—早二叠世构造背景模式图

    Figure 6. 

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    图 7  二阶模式年龄（Ma）分布图解

    Figure 7. 

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    表 1  庙尔沟花岗岩类与流纹岩LA-MC-ICP-MS U-Pb同位素分析结果

    Table 1.  LA-ICP-MS U-Pb isotopic data of Miaoergou granitoids and rhyolites

    下载: 导出CSV

    表 2  庙尔沟花岗岩类与流纹岩Lu-Hf同位素分析结果

    Table 2.  Lu-Hf isotopeic analytical results of Miaoergou granitoids and rhyolites

    下载: 导出CSV
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收稿日期:  2019-04-18
修回日期:  2019-08-26
刊出日期:  2019-10-25

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