ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
阿尔泰造山带西段同造山铁列克花岗岩体锆石U-Pb年龄及其构造意义
  
关键词:arc granite  La-ICPMS  Central Asia  Orogenic belt  Eopaleozoic ozoic
基金项目:本文由国家重大基础研究规划项目(编号:2001CB409802)、国际合作基金项目(编号:40210647)、国家自然科学基金项目(编号:40472101、49772105)、西北大学大陆动力学实验室资助。
作者单位E-mail
童英 中国地质科学院地质研究所北京100037 yingtong@pku.edu.cn 
王涛 中国地质科学院地质研究所北京100037  
洪大卫 中国地质科学院地质研究所北京100037  
柳晓明 西北大学地质学系大陆动力学教育部重点实验室陕西西安710069  
韩宝福 北京大学地球与空间科学学院北京,100871  
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摘要:
Zircon U-Pb Age of Syn-orogenic Tielieke Pluton in the Western Part of Altay Orogenic Belt and Its Structural Lnplications
      Being an important pluton in the western part of Altay orogen, Tielieke pluton shows arc granitoid characteristics. Its emplacement time, however, remains undetermined. This paper presents a zircon La-ICPMS 206Pb/238U age of 409±5 Ma (MSWD=10),which is interpreted as its emplacement age. This provides an evidence for discrimination and epoch of syn-orogenic granitoid, and also serves as a new chronological restriction for the subduction-orogeny of Altay orogen in Eopaleozoic (Ordovician-Devonian).
TONG Ying,WANG Tao,HONG Dawei,LIU Xiaoming,HAN Baofu.2005.Zircon U-Pb Age of Syn-orogenic Tielieke Pluton in the Western Part of Altay Orogenic Belt and Its Structural Lnplications[J].Acta Geoscientica Sinica,26(z1):74-77.
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