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内蒙古苏尼特左旗白音乌拉北部白音高老组时代重新厘定——来自LA-ICP-MS锆石U-Pb年龄的证据
引用本文:肖中军,王振强,吴 煜,吕达鑫,田强国,王建统,徐建昌.内蒙古苏尼特左旗白音乌拉北部白音高老组时代重新厘定——来自LA-ICP-MS锆石U-Pb年龄的证据[J].地质通报,2015,34(9):1706-1714.
作者姓名:肖中军  王振强  吴 煜  吕达鑫  田强国  王建统  徐建昌
作者单位:河南省地质矿产勘查开发局第一地质矿产调查院,河南 洛阳 471023
基金项目:中国地质调查局项目(编号:1212011220452)
摘    要:内蒙古苏尼特左旗北部出露一套灰白色流纹质火山岩,前人根据岩性组合将其归入上侏罗统白音高老组。在这套火山岩中获得了4个LA-ICP-MS锆石U-Pb年龄,分别为305.1±1.1Ma、304.5±1.1Ma、305.7±1.9Ma、303.6±1.1Ma,将其划归为上石炭统宝力高庙组,这对研究区的地层划分及确定岩浆演化具有指导性意义。

关 键 词:白音高老组  火山岩  宝力高庙组  LA-ICP-MS锆石U-Pb年龄

Redetermination of the age of Baiyingaolao Formation in Sonid Left Banner, Inner-Mongolia: Evidence from LA-ICP-MS U-Pb dating of zircons
Institution:No. 1 Institute of Geological & Mineral Resources Survey of Henan, Luoyang 471023, He'nan, China
Abstract:There exists a suite of gray rhyolitic rocks in Sonid Left Banner of Inner-Mongolia. According to the petrological features, these volcanic rocks are considered to be a part of Upper Cretaceous Baiyingaolao Formation. With the LA-ICP-MS dating analysis, however, the authors obtained four U-Pb ages, i.e., 305.1±1.1Ma, 304.5±1.1Ma, 305.7±1.9Ma, and 303.6±1.1Ma, indicating that they belong to the Upper Carboniferous Baoligaomiao Formation. The result achieved by the authors has guiding significance for stratigraphic division and determination of magma evolution.
Keywords:Baiyingaolao Formation  rhyolitic rocks  Baoligaomiao Formation  LA-ICP-MS zircon U-Pb dating
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