ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
内蒙古西乌旗巴布盖诺尔地区早二叠世花岗斑岩U-Pb年龄、地球化学特征及其地质意义
  
关键词:Babugainuoer  granite porphyry  petrogeochemistry  LA-ICP-MS  zircon U-Pb age  Hf isotopes
基金项目:防灾科技学院中央高校基本科研业务费专题项目(编号: ZY20215134);国家自然科学基金青年科学基金项目(编号: 42002093)
作者单位E-mail
王承洋 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室防灾科技学院地球科学学院 598648597@qq.com 
陈伟 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室 nmgchenwei@163.com 
齐路晶 防灾科技学院地球科学学院  
俞嘉嘉 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
孙珍军 防灾科技学院地球科学学院  
黄静宜 防灾科技学院地球科学学院  
杨乐 内蒙古山金地质矿产勘查有限公司  
齐松 内蒙古山金地质矿产勘查有限公司  
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摘要:
Zircon U-Pb Age and Geochemical Characteristics of the Granite Porphyry in the Babugainuoer Area, West Ujimqin Banner, Inner Mongolia and Their Geological Implications
      The Babuganuoer area, West Ujimqin Banner, Inner Mongolia, is located at the western slope of southern Great Xing’an Range. For the purpose of revealing its formation age, petrogenesis and tectonic significance, we conducted a comprehensive study of zircon U-Pb chronology, Hf isotope and whole-rock geochemistry for granite porphyry exposed in this area. The 206Pb/238U ages of 12 spots of zircons from Sample SBLY-2 are between (269±3)–(279±3) Ma, with a weighted mean 206Pb/238U age of (274±3) Ma (MSWD=1.7). The 206Pb/238U ages of 12 spots of zircons from Sample SBLY-3 are between (269±3)–(282±4) Ma, with a weighted mean 206Pb/238U age of (275±3) Ma (MSWD=1.6). The above results reveal that they were magmatic products of the Late Early Permian, rather than the previously believed Cretaceous. These rocks show characteristics of high silicon, low aluminum, low magnesium, high alkali, rich potassium and low sodium. These samples are enriched in Rb, Th, U, K elements and depleted in Nb, Ta, Ti elements, indicating a genesis of aluminous A-type granites. Zircons of these rocks have εHf(t) values of 8.2–11.1, and the two-stage Hf model ages (TDM2) of 588–789 Ma, suggesting that the Early Permian granitic rocks in the Babugainuoer area mainly derived from the newly accreted lower crust during the Neoproterozoic period. We comprehensively conclude that the Early Permian granitic rocks in the Babugainuoer area were formed in a post-collisional extensional setting and the Paleo-Asian Ocean was closed no later than the Late Permian.
WANG Chengyang,CHEN Wei,QI Lujing,YU Jiajia,SUN Zhenjun,HUANG Jingyi,YANG Le,QI Song.2025.Zircon U-Pb Age and Geochemical Characteristics of the Granite Porphyry in the Babugainuoer Area, West Ujimqin Banner, Inner Mongolia and Their Geological Implications[J].Acta Geoscientica Sinica,46(2):283-297.
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