A continental magmatic arc existed during the global “tectono‑magmatic lull”:Evidence from ca. 2.3 Ga intrusive rocks of the Taihua Complex in the North ChinaCraton
收藏NIAID Data Ecosystem2026-05-10 收录
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https://figshare.com/articles/dataset/A_continental_magmatic_arc_existed_during_the_global_tectono_magmatic_lull_Evidence_from_ca_2_3_Ga_intrusive_rocks_of_the_Taihua_Complex_in_the_North_ChinaCraton/31073683
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The supporting information Text S1 presents the analytical methods. Figures S1 and S2 consist of the element correlation diagrams and the LOI vs. major element variation diagram, respectively, for the quartz diorite, diorite, gabbro-diorite, and hornblendite samples from the southern margin of the North China Craton.
创建时间:
2026-01-15



