首页 | 本学科首页   官方微博 | 高级检索  
     检索      


SHRIMP U-Pb zircon age,geochemistry and Nd isotope of the Guandaoshan pluton in SW Sichuan: Petrogenesis and tectonic significance
Authors:Li Xianhua  Li Zhengxiang  Zhou Hanwen  Liu Ying  Liang Xirong  Li Wuxian
Institution:1.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou,China;2.Tectonics Special Research Centre, School of Earth and Geographical Sciences,The University of Western Australia,Crawley,Australia;3.Faculty of Earth Sciences,China University of Geosciences,Wuhan,China
Abstract:SHRIMP U-Pb zircon age, geochemical and Nd isotopic data are reported for the Neo-proterozoic Guandaoshan pluton in the Yanbian region, SW Sichuan. This pluton is of typical I-type granite and emplaced at (857 ± 13) Ma. Geochemical and Nd isotopic characters suggest that the pluton was generated by partial melting of pre-existing, young (late Mesoproterozoic to early Neo-proterozoic) low-K tholeiitic protolith within an intraplate anorogenic setting. The Guandaoshan pluton probably records the earliest magmatism induced by the proposed ca. 860–750 Ma mantle superplume beneath the supercontinent Rodinia.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号