Decoupled magmatic and hydrothermal processes control Nb enrichment and mineralization in syenitic systems
Published: 11 March 2026| Version 1 | DOI: 10.17632/gxnmzypfbj.1
Contributor:
Yan LiuDescription
Supplementary Table S1 to S7 for “Decoupled magmatic and hydrothermal processes control Nb enrichment and mineralization in syenitic systems” Table S1 Standards used for EPMA and LA-ICP-MS analyses; Table S2 Major Element Compositions and Atoms per Formula Unit (apfu) of Pyroxene from the Baicao and Baima Intrusions; Table S3 Trace Element Compositions of minerals from the Baicao and Baima Intrusions; Table S4 The whole-rock Sr-Nd isotopic results of syenite from Baicao and Baima Intrusions; Table S5 Magmatic Zircon Hf–O Isotope Compositions from Baicao and Baima Intrusions; Table S6 Major element and trace element of high-Ti basalt from Baicao region; Table S7 Simulation results for Baicao and Baima
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Institutions
- Chinese Academy of Geological SciencesBeijing, Beijing
Categories
Geology