ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鲁西孟家屯一种细粒斜长角闪岩的锆石SHRIMP年代学
  
关键词:western Shandong  Fine-grained amphbolite  chronology  North China platform
基金项目:原地质矿产部跨世纪人才基金项目;同位素开放实验室基金项目
作者单位E-mail
杜利林 中国科学院地质与地球物理研究所北京100029中国地质科学院地质研究所北京100037 dulilin7310@sina.com 
庄育勋 中国地质调查局北京100011  
杨崇辉 中国地质科学院地质研究所北京100037  
万渝生 中国地质科学院地质研究所北京100037
北京离子探针中心北京100037 
 
王新社 中国地质科学院地质研究所北京100037  
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摘要:
SHRIMP U-Pb Zircon Chronology of Fine-grained Amphibolite in the Mengjiatun Area, Western Shandong
      Based on studying mineral lithofaces, zircon characteristics and chronology, the authors obtained zircon SHRIMP metamorphic age of 2 604±11 Ma for fine-grained amphbolite from Mengjiatun area of western Shandong. According to metamorphic ages of Mengjiatun Formation and other magmatic ages of western Shandong, it is concluded that intense geological movement took place from 2 650 Ma to 2 600 Ma, which is quite different from other regions in the North China platform. Therefore western Shandong has its unique geological evolution history in Early Precambrian.
DU Li-lin,ZHUANG Yu-xun,YANG Chong-hui,WAN Yu-sheng,WANG Xin-she.2005.SHRIMP U-Pb Zircon Chronology of Fine-grained Amphibolite in the Mengjiatun Area, Western Shandong[J].Acta Geoscientica Sinica,26(5):429-434.
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