A syn- to post-collisional tectonic transition in the Khondalite Belt, North China Craton: Constraints from 1.95 - 1.93 Ga adakitic granitoids in the Daqingshan Complex

Xiao Wang,Jian Zhang,Changqing Yin,Jiahui Qian,Peng Gao,Shuhui Zhang,Xiaoguang Liu,Ying Chen,Chen Zhao

Precambrian Research（2022）

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摘要

•Syn-collisional granitoids in the Daqingshan Complex were emplaced at 1.95–1.93 Ga.•Granitoids are adakitic-like rocks that were derived from the partial melting of the thickened mafic lower crust.•Syn- to post-collisional tectonic transition in the Khondalite Belt occurred at 1.95–1.93 Ga.

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关键词

Late Paleoproterozoic,Adakitic granitoids,Thickened lower crust,Khondalite Belt,North China Craton

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