U-Pb Isotopic Age and a Further Understanding of the Ore-Forming Mechanism in Granite from the Southern Jiangxi Province
详细信息   
摘要

    

Magmatic rocks in the Southern Jiangxi Province are widely distributed. The diagenetic ages of some rocks are clear, but are still in dispute for others. The U-Pb ages of the Tianxin, Lujing, Shuitou, Baie, Gaoshanjiao, Hanfang, Yangcun, Hunandong, Zhulanbu, Linyang, Dafuzu, Youshan, Huangsha,Yangbu,Wantian and other granites were obtained by using Laser Ablation-Multicollector Inductively Coupled Plasma-Mass Spectrometry (LA-MC-ICPMS). All the research results indicate that granites in the Southern Jiangxi Province experienced a long term evolution and many of them were formed in multiple stages. Although Caledonian rocks were ignored previously since they had no relationship with W deposits, they can be primary rocks for ion-adsorption type rare earth element deposits.

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