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内蒙古克什克腾旗广兴源复式岩体SHRIMP U-Pb定年及地质意义讨论
引用本文:江小均,柳永清,彭楠,石玉若,许欢,魏文通,刘增校,赵华平,姚宝钢. 内蒙古克什克腾旗广兴源复式岩体SHRIMP U-Pb定年及地质意义讨论[J]. 地质学报, 2011, 85(1): 114-128
作者姓名:江小均  柳永清  彭楠  石玉若  许欢  魏文通  刘增校  赵华平  姚宝钢
作者单位:1.国地质科学院地质研究所,北京,100037;2.国地质大学地球科学与资源学院,北京,100083;3.京离子探针中心,北京,100037;4.北省区域地质矿产调查研究所,河北廊坊,065000
摘    要:广兴源复式岩体位于内蒙古东部西拉木伦河上游地区,岩体主体由二长岩、二长花岗岩、花岗岩和花岗闪长岩构成,边部有少量二长辉长岩和闪长岩出露.岩体地球化学特征表明其属于火山弧环境;对岩体早期的二长岩和侵位于二长岩的花岗闪长岩进行锆石SHRIMP U-Pb定年,分别得到206Pb/238U加权平均年龄为 263.8±2.1Ma...

关 键 词:广兴源复式岩体  地球化学  锆石SHRIMP U-Pb定年  内蒙古
收稿时间:2010-04-29
修稿时间:2010-04-29

Constraints on the closing time of Paleo-Asian Ocean: evidence of Geochemistry and SHRIMP U-Pb dating from the Guangxingyuan composite granites in Hexiqten Qi , Inner Mongolia, China
JIANG Xiaojun,LIU Yongqing,PENG Nan,SHI Yuruo,XU Huan,WEI Wentong,LIU Zengxiao,ZHAO Huaping,YAO Baogang. Constraints on the closing time of Paleo-Asian Ocean: evidence of Geochemistry and SHRIMP U-Pb dating from the Guangxingyuan composite granites in Hexiqten Qi , Inner Mongolia, China[J]. Acta Geologica Sinica, 2011, 85(1): 114-128
Authors:JIANG Xiaojun  LIU Yongqing  PENG Nan  SHI Yuruo  XU Huan  WEI Wentong  LIU Zengxiao  ZHAO Huaping  YAO Baogang
Affiliation:1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing,100037; 2. School of Geosciences and Resources,Chinese University of Geosciences, Beijing,100083;3. Beijing SHRIMP Center, Beijing,100037; 4. Institute of Regional Geology and Mineral Resources Survey of Hebei Province, Langfang,065000
Abstract:
Keywords:zircon SHRIMP U-Pb dating   Guangxingyuan composite granites   Hexiqten Qi   Inner Mongolia
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