吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 690-708.doi: 10.13278/j.cnki.jjuese.20180240

• 地质与资源 • 上一篇    下一篇

东天山觉罗塔格带东段早志留世中酸性侵入岩的年代学、地球化学及构造意义

于介禄1, 于介江1, 杨万志2, 张元厚1, 郭秀玮1   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 新疆维吾尔自治区地质调查院, 乌鲁木齐 830000
  • 收稿日期:2018-09-14 出版日期:2019-06-03 发布日期:2019-06-03
  • 通讯作者: 于介江(1961-),男,教授,博士,主要从事岩石学方面的研究,E-mail:yujiejiang@jlu.edu.cn E-mail:yujiejiang@jlu.edu.cn
  • 作者简介:于介禄(1992-),男,硕士研究生,主要从事岩石学方面的研究,E-mail:626951312@qq.com
  • 基金资助:
    国家自然科学基金项目（41672050）；新疆维吾尔自治区地质勘查基金管理中心项目（Y14-5-LQ05）

Geochronology, Geochemistry and Tectonic Implications of Early Silurian Intermediate-Acid Intrusive Rocks in East of Jueluotage Belt, Eastern Tianshan

Yu Jielu1, Yu Jiejiang1, Yang Wanzhi2, Zhang Yuanhou1, Guo Xiuwei1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Xinjiang Institute of Geological Survey, Urumqi 830000, China
  • Received:2018-09-14 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by National Natural Science Foundation of China (41672050) and Project of the Xinjiang Uygur Autonomous Region Geological Survey Fund Management Center (Y14-5-LQ05)

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摘要： 为了确定东天山觉罗塔格带东段玉海地区中酸性侵入岩的形成时代、源区性质及其构造属性，本文对该区中酸性侵入岩进行了系统的LA-ICP-MS锆石U-Pb定年、全岩地球化学以及Sr-Nd同位素分析。2个样品中的锆石在CL图像上具明显振荡环带，Th/U值为0.28~0.59，指示其岩浆成因。对岩浆锆石定年结果表明，它们主要形成于早志留世（433.2~431.2 Ma），代表了寄主岩石的形成时代。样品w（SiO2）=57.88%~69.01%，w（Na2O）=3.46%~5.07%，w（K2O）=0.50%~1.65%，Na2O/K2O=4.26~6.79，Mg#=45.1~52.3，A/CNK=0.89~1.00；稀土配分模式呈右倾型，LREE/HREE=5.55~11.47，（La/Yb）N=4.18~13.54，δEu=0.82~1.25；在微量元素蛛网图上表现为大离子亲石元素（Ba、U、K、Sr等）相对富集和高场强元素（Th、Ti、Nb、Ta）相对亏损；全岩εNd（t）值介于6.1~7.0之间。研究表明，早志留世中酸性侵入岩的岩浆源区主要为年轻地壳物质，结合火成岩的组合特征、岩浆作用性质以及区域构造演化历史，认为早志留世中酸性侵入岩形成于康古尔洋板片向北（吐-哈地块）俯冲的活动大陆边缘环境，从而将康古尔大洋板片北向俯冲的时限追溯至早志留世。

关键词: 东天山觉罗塔格带东段, 早志留世, 中酸性侵入岩, 年代学, 地球化学, 构造意义

Abstract: In order to ascertain the formation age, source and tectonic properties of the intermediate-acid intrusive rocks in the Yuhai area of the eastern Jueluotage belt in the eastern Tianshan, this paper systematically presents LA-ICP-MS zircon U-Pb geochronology, whole rock geochemistry and Sr-Nd isotopes data of the rocks in this area. The selected zircons of two samples show obvious oscillation zoning in cathodoluminescence (CL) images, and have Th/U value of 0.28-0.59, indicating a magmatic origin. The zircon U-Pb dates indicate that they formed in the Early Silurian of (433.2-431.2) Ma, representing the emplacement age of these host rocks. These samples have w(SiO2)=57.88%-69.01%,w(Na2O)=3.46%-5.07%,w(K2O)=0.50%-1.65%,Na2O/K2O=4.26-6.79,Mg#=45.1-52.3,and A/CNK=0.89-1.00; the rare earth element distribution patterns are right-slipped, LREE/HREE=5.55-11.47,(La/Yb)N=4.18-13.54,and δEu=0.82-1.25;the trace element spider diagrams show that they are enriched in LILE (Ba, U, K and Sr), moderately depleted of HFSE (Th, Ti, Nb and Ta); the value of εNd(t) of the whole rock is between 6.1 and 7.0. The study shows that the magma source of the intermediate-acid intrusive rocks in the Early Silurian is mainly young crustal material. Combining with the characteristics of igneous rock association, magmatism and regional tectonic evolution history, it is considered that the intermediate-acid intrusive rocks of the Early Silurian were formed in the active continental margin environment under the northward subduction of the Kanggur Ocean plate (Turpan-Hami block). Thus, the time of the Kanggur plate subduction can be traced back to the Early Silurian.

Key words: eastern part of Jueluotage belt, Eastern Tianshan, Early Silurian, intermediate-acid intrusive rocks, geochronology, geochemistry, tectonic implications

中图分类号: 

  • P588.12
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