Zircon U-Pb ages and Hf isotopes from the Yishui Complex:implications for the crustal evolution of the Shandong Complex in the Eastern Block, North China Craton
The Neoarchean Yishui Complex locates in the eastern margin of the Western Shandong Complex,which is an important component of the Precambrian basement of the Eastern Block of the North China Craton.High-grade metamorphic supracrustal rocks and granitoids comprise the majority of the Yishui Complex.LA-ICP-MS zircon U-Pb dating and Hf isotopic analyses on various lithological units of the Yishui Complex have been carried out in this study and the results therefore provided new insights into the Neoarchean crustal evolution history of the Western Shandong Complex in the Eastern Block of the North China Craton.
Zircon U-Pb Hf isotope Yishui Complex North China Croton Precambrian crustal evolution
Meiling Wu Guochun Zhao Min Sun Sanzhong Li Zhian Bao
Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong College of Marine Geosciences, Ocean University of China, Qingdao, 266003, China, State Key Laboratory of Continental Dynamics, Northwest University, Xi”an, 710068, China
国内会议
兰州
英文
546-546
2012-09-21(万方平台首次上网日期,不代表论文的发表时间)