吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1599-1614.doi: 10.13278/j.cnki.jjuese.20200011

• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇    

内蒙古西乌旗迪彦庙蛇绿岩带内辉长岩地球化学及年代学

熊光强1,2, 刘敏3, 张达1, 王忠4   

  1. 1. 江西省地质矿产勘查开发局物化探大队, 南昌 330025;
    2. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
    3. 西北大学地质学系, 西安 710069;
    4. 内蒙古自治区地质调查院, 呼和浩特 010020
  • 收稿日期:2020-01-13 出版日期:2020-09-26 发布日期:2020-09-29
  • 通讯作者: 张达(1967-),教授,主要从事构造地质学及区域成矿规律研究,E-mail:zhangda@cugb.edu.cn E-mail:zhangda@cugb.edu.cn
  • 作者简介:熊光强(1988-),男,工程师,硕士,主要从事构造地质学研究,E-mail:xgq_1201@163.com
  • 基金资助:
    中国地质调查局项目（1212011085490，1212011120700）

Geochemistry and Geochronology of Gabbro in Diyanmiao Ophiolite Belt, West Ujimqin Banner, Inner Mongolia

Xiong Guangqiang1,2, Liu Min3, Zhang Da1, Wang Zhong4   

  1. 1. Geophysical and Geochemical Exploration Party, Jiangxi Bureau of Geology and Mineral Resources, Nanchang 330025, China;
    2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    3. Department of Geology, Northwest University, Xi'an 710069, China;
    4. Institute of Geological Survey of Inner Mongolia, Hohhot 010020, China
  • Received:2020-01-13 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by Project of China Geological Survey (1212011085490, 1212011120700)

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摘要： 内蒙古西乌旗迪彦庙蛇绿岩位于二连浩特—贺根山蛇绿岩带与交其尔—锡林浩特蛇绿岩带一线之间，大地构造位于中亚造山带中段的锡林浩特晚古生代褶皱带。本文主要对其内的辉长岩进行了地球化学及年代学研究。研究结果表明：辉长岩w（SiO2）为45.49%~50.48%，w（Al2O3）为13.31%~17.05%，w（K2O）为0.01%~0.65%，w（Na2O）为0.30%~4.15%，w（CaO）为8.00%~19.54%，w（MgO）为5.22%~10.92%，w（P2O5）为0.03%~0.23%，显示西乌旗迪彦庙蛇绿岩中的辉长岩属于高铝、低钾、低钠的拉斑系列；辉长岩的稀土元素总量低，重稀土元素比轻稀土元素富集，微量元素Nb、Zr、Hf、Ti相对亏损，K、Ta、Sr相对富集；La-ICP-MS锆石U-Pb测年获得辉长岩的年龄为（345.3±2.3）Ma，为早石炭世。综合分析，辉长岩可能为受到俯冲作用产生的流体交代而成，而并非结晶分异作用所致；迪彦庙蛇绿岩形成环境为弧前环境。

关键词: 迪彦庙, 地球化学, 锆石U-Pb定年, 蛇绿岩, 辉长岩

Abstract: The Diyanmiao ophiolite in the west Ujimqin Banner, Inner Mongolia, which tectonically belongs to the Xilinhaote Late Paleozoic fold belt in the southeastern Central Asian orogenic belt, is located between the Erlianhot-Hegenshan ophiolite belt and the Jiaoqier-Xilinhaote ophiolite belt. This study focuses on the geochemical and geochronological characteristics of the gabbros from the Diyanmiao ophiolite. Whole-rock geochemical data show that the gabbros are high Al, lower K, lower Na, and tholeiitic in nature, with w(SiO2) of 45.49%~50.48%, w(Al2O3) of 13.31%~17.05%, w(K2O) of 0.01%~0.65%, w(Na2O) of 0.30%~4.15%, w(CaO) of 8.00%~19.54%, w(MgO) of 5.22%~10.92%, and w(P2O5) of 0.03%~0.23%. These rocks have low total REE contents and relatively enriched HREE. They also show enrichments in K, Ta, and Sr, and depletions in Nb, Zr, Hf, and Ti. La-ICP-MS zircon U-Pb dating results suggest that the gabbros were formed at Early Carboniferous ((345.3±2.3) Ma). In combination with previously works and regional geology, the authors propose that the gabbros in the Diyanmiao ophiolite were possibly formed by fluids metasomatism in an island arc setting during oceanic subduction, rather than crystallization and differentiation processes.

Key words: Diyanmiao, geochemistry, zircon U-Pb dating, ophiolite, gabbro

中图分类号: 

  • P588.12
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