Supplemental Material: Within-plate granitoids in the Jiaobei Terrane were products of a possible tectonic switch from rifting to subduction collision at ca. 2.1 Ga in the North China Craton
Year: 2025
Type: supplementary-materials
Abstract: Supplemental Text S1: Analytical method. Table S1: Major- and trace-element concentrations of the Dongbaishishan and Gujiacun granitoids. Table S2: LA-ICP-MS U-Th-Pb zircon data of the Dongbaishishan and Gujiacun granitoids. Table S3: Lu-Hf isotopic data of the Dongbaishishan and Gujiacun granitoids. Table S4: Zircon oxygen isotopic data of the Dongbaishishan and Gujiacun granitoids. Table S5: The 2.2–2.1 Ga mafic-felsic magmatism in the North China Craton. Table S6: Summary of the spatiotemporal distribution, rock associations, and Hf-Nd isotope characters for G1 and G2 magmatism in the North China Craton.
Authors: Yali Zheng, et al.
Language: English
Subfield: Geophysics
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: gold
OpenAlex ID: W4414313209
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