ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
皖南蛇绿岩套辉长岩锆石U-Pb定年以及元素和氧同位素研究
  
关键词:gabbro  zircon  O isotope  Neoproterozoic  hydrothermal alteration
基金项目:本文为国家自然科学基金项目(编号:40334036)和中国科学院知识创新工程项目(编号:KZCX3-SW-141)资助成果。
作者单位E-mail
吴荣新 中国科学院壳幔物质与环境重点实验室中国科学技术大学地球和空间科学学院安徽合肥230026 rxwu@mail.ustc.edu.cn 
郑永飞 中国科学院壳幔物质与环境重点实验室中国科学技术大学地球和空间科学学院安徽合肥230026  
吴元保 中国科学院壳幔物质与环境重点实验室中国科学技术大学地球和空间科学学院安徽合肥230026  
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摘要:
Zircon U-Pb Dating and Element and Oxygen Isotope Geochemistry of Gabbro from Ophiolites in South Anhui
      Zircon U-Pb dating, whole-rock major and trace elements, Sr-Nd isotopes, and mineral O isotopes were determined for samples from ophiolites in south Anhui. LA-ICPMS and SHRIMP zircon U-Pb analysis reveals three age phases of magmatic zircons formed at 891±13 Ma, 826±4 Ma and 764±10 Ma respectively. The features of elements and isotopes display apparent signatures of island-arc magmatic rocks, suggesting that they were derived from partial melting of mantle lithosphere of the supra-subduction zone (SSZ).O isotope analyses suggest that they experienced different degrees of subsolidus hydrothermal alt eration. Based on element and isotope analyses in combination with the records of Neoproterozoic magmatism in this area, the authors interpret 891±13 Ma and the age of ophiolite emplacement. It is also thought that at 826±4 Ma the rocks were rebuilt by pre-rift magmatic activities, and at 764±10 Ma they were affected by syn-rift magmatism and subsolidus hydrothermal alteration.
WU Rongxin,ZHENG Yongfei,WU Yuanbao.2005.Zircon U-Pb Dating and Element and Oxygen Isotope Geochemistry of Gabbro from Ophiolites in South Anhui[J].Acta Geoscientica Sinica,26(z1):70-73.
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