吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (6): 1740-1753.doi: 10.13278/j.cnki.jjuese.201606112

• 地质与资源 • 上一篇    下一篇

赤峰撰山子花岗岩年代学、地球化学特征及其成岩动力学背景

孙珍军1, 孙国胜2, 于赫楠1, 向柱1, 田毅3, 刘彤4, 陈旭4, 李杨4   

  1. 1. 防灾科技学院地震科学系, 北京 101601;
    2. 吉林大学地球科学学院, 长春 130061;
    3. 辽宁省地质矿产调查院, 沈阳 110031;
    4. 核工业二四三大队, 内蒙古 赤峰 024006
  • 收稿日期:2016-04-25 出版日期:2016-11-26 发布日期:2016-11-26
  • 通讯作者: 孙国胜(1964-),男,副教授,主要从事矿床地球化学研究,E-mail:sgsh8888@163.com E-mail:sgsh8888@163.com
  • 作者简介:孙珍军(1982-),男,讲师,主要从事矿床学研究,E-mail:306292193@qq.com
  • 基金资助:
    河北省高等学校科学技术研究重点项目（ZD2015203）；中央高校基本科研业务费资助项目（ZD2015203）

Chronology and Geochemical Characteristics of Zhuanshanzi Granite in Chifeng and Its Diagenetic Dynamics Background

Sun Zhenjun1, Sun Guosheng2, Yu Henan1, Xiang Zhu1, Tian Yi3, Liu Tong4, Chen Xu4, Li Yang4   

  1. 1. Department of Earthquake Science, Institute of Disaster Prevention Science and Technology, Beijing 101601, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. Liaoning Survey Academy of Geology and Mineral Resources, shenyang 110031, China;
    4. 243 Team of Nuclear Industry, Chifeng 024006, Inner Mongolia, China
  • Received:2016-04-25 Online:2016-11-26 Published:2016-11-26
  • Supported by:
    Supported by Higher School Science and Technology Research Key Project in Hebei Province(ZD2015203) and Central University Basic Scientific Research Business Expenses Funded Project(ZD2015203)

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摘要： 撰山子角闪二长花岗岩位于华北克拉通与兴蒙造山带结合部位的中生代构造岩浆活动带，对其开展了主量元素、稀土和微量元素分析以及LA-ICP-MS锆石U-Pb定年等工作，目的在于精确厘定岩体的形成时代和研究其形成的动力学背景。结果表明：花岗岩的LA-ICP-MS锆石U-Pb谐和年龄为（245.8±3.1）Ma（MSWD=3.7，n=17），属早三叠世。岩石地球化学成分特征显示为，其具有高硅（w（SiO2）=71.68%~72.85%）、富碱（w（Na2O+K2O）=8.98%~9.20%）、高铝（w（Al2O3）=13.45%~13.77%）、低钙（w（CaO）=0.81%~0.99%）及低TFeO/MgO值（平均值为6.55）的特征，属高钾钙碱性、高分异I型弱铝质花岗岩；稀土配分曲线呈现向右倾斜的配分模式，Eu具有明显的亏损（δEu=0.66~0.68），表明斜长石发生了明显的分离结晶作用；在微量元素原始地幔标准化图谱上呈现清晰的Th、U、La、P富集，Ba、Nb、Ti、Sr、Ta等相对亏损的特征。综合分析认为，撰山子角闪二长花岗岩主要形成于下地壳部分熔融作用，可能有少量的地幔组分加入，其形成于华北板块和西伯利亚板块最终拼合后的后碰撞/后造山伸展作用构造环境。

关键词: 花岗岩, 地球化学, LA-ICP-MS锆石U-Pb定年, 构造环境, 撰山子

Abstract: The Zhuanshanzi hornblende monzogranite is located in the the Mesozoic tectonic magmatic active belt which between the North China craton and the Xingmeng orogeny belt. Testing of major elements, rare-earth elements (REEs), trace elements and LA-ICP-MS zircon U-Pb dating of the hornblende monzogranite have be carried out to accurately determined the forming age and study the dynamics background of the granite,rock. Results show that the LA-ICP-MS zircon U-Pb age of the hornblende monzogranite is (245.8±3.1) Ma. (MSWD=3.7,n=17), and belongs to the Early Triassic. Geochemically, the granite is characterized by high concentrations of silica (w(SiO2)=71.68%-72.85%), alkali (w(Na2O+K2O)=8.98%-9.20%), and alumina (w (Al2O3)=13.45%-13.77%); low concentrations of calcium (w(CaO)=0.81%-0.99%); and with low values of TFeO/MgO (average is 6.55), indicating the hornblende monzogranite belongs to high-K, calc-alkaline high differentiation Ⅰ type, weak aluminum granite. The granite is enriched in LREE and relatively depleted in HREE(LaN/YbN=21.94-24.33), and obvious Eu anomaly (δEu=0.66-0.68), which indicates that a large number of the plagioclase fractionation occured during the magmatic processes. In addition, the granite is enriched in Th, U, La and P, and depleted in Ba, Nb, Ti, Sr and Ta, and so on. In summary, the Zhuanshanzi granite is mainly formed by partial melting of crust material, with a few new mantle source composition. It is formed under the extensional tectonic setting in post-collision or post-orogenic stage after the North China plate and Siberia plate's eventual collision.

Key words: granite, geochemistry, LA-ICP-MS zircon U-Pb dating, tectonic setting, Zhuanshanzi

中图分类号: 

  • P588.12
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