State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
Institute of Earth and Environmental Sciences, Albert-Ludwig University Freiburg, 79104 Freiburg, Germany
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
Wolfgang Siebel
Institute of Earth and Environmental Sciences, Albert-Ludwig University Freiburg, 79104 Freiburg, Germany
Shuhao Tang
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
Yiru Ji
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
Jianfeng He
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
Fukun Chen
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
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Our study investigates ca. 1.78 Ga Jiguanshan diorite in the North China Craton. We found that Paleoproterozoic diorites across the craton share similar compositions and formed from melted deep crust, differing from volcanic and mafic rocks of the same age. Geochemical analysis reveals these diorites formed during crustal stretching, marking a tectonic shift from orogenic-related to within-plate settings. This provides key evidence for understanding how tectonic setting evolved after collisions.
Our study investigates ca. 1.78 Ga Jiguanshan diorite in the North China Craton. We found that...