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
Abstract
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.
Fields of Study & Subjects
Geological and Geochemical Analysis
Geochemistry and Geochronology of Asian Mineral Deposits
Geological and Geophysical Studies
Publication details
- Journal / source
- Figshare
- Publication date
- 1 January 2026
- Document type
- Dataset