摘要
Objective The North China Craton（NCC）is almost continuously widespread TTGs of 3.8–2.5 Ga,and the intrusive peak appears at^2.53 Ga,indicating that the Neoarchean is the most important period of continental growth in the NCC（Wan Yusheng et al.,2017）.Recently studies reveal that the TTGs were formed during-2.7 Ga and 2.6–2.5 Ga in southern Jilin Province,NE of the NCC（Wang Chaoyang et al.
Objective The North China Craton（NCC）is almost continuously widespread TTGs of 3.8–2.5 Ga,and the intrusive peak appears at^2.53 Ga,indicating that the Neoarchean is the most important period of continental growth in the NCC（Wan Yusheng et al.,2017）.Recently studies reveal that the TTGs were formed during-2.7 Ga and 2.6–2.5 Ga in southern Jilin Province,NE of the NCC（Wang Chaoyang et al.
基金
supported by the National Science Foundation of China(grant No.41272223)
China Geological Survey(grants No.12120114028001,121201004000150017-28 and 121201004000160901-7)
Graduate Innovation Fund of Jilin University
