ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
云南马头湾透辉石花岗斑岩锆石SHRIMPU-Pb年龄研究
  
关键词:zircon  SHRIMP  diopside granite porphyry  Matouwan  western Yunnan Province
基金项目:中国科学院知识创新工程重要方向性项目(KZCX2SW117、KZCX2101)
作者单位E-mail
刘红英 中国科学院广州地球化学研究所边缘海地质重点实验室广东广州510640 liuhy@gig.ac.cn 
夏斌 中国科学院广州地球化学研究所边缘海地质重点实验室广东广州510640  
张玉泉 中国科学院广州地球化学研究所边缘海地质重点实验室广东广州510640  
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摘要:
The SHRIMP U-Pb Age of Matouwan Diopside Granite Porphyry in Yunnan Province
      The SHRIMP technique was applied to determining U-Pb age of the Matouwan diopside granite porphyry in western Yunnan Province. The results show that the Matouwan diopside granite porphyry was intruded at 34 Ma,which should be Oligocene in time and belong to Himalayan period. The age indicates that the Ailaoshan-Jinshajiang deep fracture zone is controlled by the collision of the Indian plate with the Eurasian continental plate at about 40 Ma.The formation of Matouwan diopside granite porphyry must have had inherent connection with the collision of the two plates.
LIU Hong-ying,XIA Bin,ZHANG Yu-quan.2003.The SHRIMP U-Pb Age of Matouwan Diopside Granite Porphyry in Yunnan Province[J].Acta Geoscientica Sinica,24(6):552-554.
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