吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 766-780.doi: 10.13278/j.cnki.jjuese.201603113

• 地质与资源 • 上一篇    下一篇

伊勒呼里山中生代火山岩:锆石U-Pb年代学及其对岩浆事件的制约

尹志刚1, 王文材1, 张跃龙2, 王阳1, 韩宇1, 曹忠强1, 郑贝1   

  1. 1. 辽宁工程技术大学矿业学院, 辽宁 阜新 123000;
    2. 黑龙江省地质调查研究总院齐齐哈尔分院, 黑龙江 齐齐哈尔 161005
  • 收稿日期:2015-11-13 出版日期:2016-05-26 发布日期:2016-05-26
  • 作者简介:尹志刚(1962-),男,教授,博士生导师,主要从事区域地质矿产调查研究,E-mail:yzg63@163.com
  • 基金资助:

    中国地质调查局项目(1212011120659)

Mesozoic Volcanic Rocks in Yilehuli Area: Zircon U-Pb Ages and Their Constraints on the Magmatic Events

Yin Zhigang1, Wang Wencai1, Zhang Yuelong2, Wang Yang1, Han Yu1, Cao Zhongqiang1, Zheng Bei1   

  1. 1. College of Mining Engineering, Liaoning Technical University, Fuxin 123000, Liaoning, China;
    2. Qiqihar Branch, Heilongjiang Institute of Geological Survey, Qiqihar 161005, Heilongjiang, China
  • Received:2015-11-13 Online:2016-05-26 Published:2016-05-26
  • Supported by:

    Supported by Geological Survey Project of China Geological Survey(1212011120659)

摘要:

伊勒呼里山地区中生代火山岩由安山岩、粗面英安岩、流纹岩、流纹质凝灰岩和流纹质玻屑凝灰岩等组成。中生代火山岩中的锆石多呈半自形-自形晶,振荡环带发育,Th/U值略高(0.30~2.56),为岩浆成因。锆石U-Pb同位素年代学研究表明:塔木兰沟组安山岩年龄为(161.0±1.0)Ma(n=22),形成于中侏罗世;满克头鄂博组流纹岩年龄为(157.8±2.3)Ma(n=24),形成时代属于晚侏罗世;玛尼吐组火山岩2个样品的年龄分别为(154.0±2.0)Ma(n=23)和(151.7±1.4)Ma(n=25),形成时代属于晚侏罗世;白音高老组火山岩2个样品的年龄分别为(124.1±1.1)Ma(n=25)和(125.1±0.7)Ma(n=23),形成时代为早白垩世。捕获锆石的定年结果显示,本区存在前寒武纪岩浆事件(774 Ma)、加里东期岩浆事件(472 Ma)、印支期岩浆事件(214、210 Ma),这与周边基底岩石中锆石U-Pb的定年结果相吻合。

关键词: 中生代, 火山岩, 锆石U-Pb定年, 伊勒呼里山

Abstract:

The Mesozoic volcanic rocks in Yilehuli area consist of andesites, trachy-dacite, rhyolites, fine ash tuff rhyolitic volcanos and rhyolitic vitric tuffs.Zircons from these Mesozoic volcanic rocks has obvious oscillatory zoning, are of euhedral-subhedral shapes and high Th/U ratios (0.30-2.56), implying their magmatic origin.The mean U-Pb age of zircons in volcanic rock from the Tamulangou Formation is (161.0±1.0)Ma(n=22), suggesting the volcanic rock was formed in the Middle Jurassic; mean U-Pb ages of zircon from the volcanic rock in the Manketouebo Formation is (157.8±2.3)Ma(n=24), suggesting these volcanic rock in the Manketouebo Formation was formed in the Late Jurassic; U-Pb age of zircon grains from two volcanic rock samples in the Manitu Formation are (154.0±2.0)Ma(n=23) and (151.7±1.4)Ma(n=25) respectively, suggesting the volcanic rock in Manitu Formation was also formed in the Late Jurassic;mean U-Pb ages of zircon grains from volcanic rocks in the Baiyingaolao Formation are (124.1±1.1)Ma(n=25) and (125.1±0.7)Ma(n=23) respectively, suggesting those volcanic rocks in the Baiyingaolao Formation formed in the Early Carboniferou. The dating results of captured zircons show that the Precambrian (D4554.10:774 Ma), Caledonian (PM008TC42.17:472 Ma), Indosinian (D0350.15:214 Ma, D0350.16:210 Ma) magmatic events had taken place in the area, which is consistent with the zircon U-Pb dating results from the surrounding rocks in basement.

Key words: Mesozoic, volcanic rocks, zircon U-Pb dating, Yilehuli area

中图分类号: 

  • P588.14

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