Decoupled magmatic and hydrothermal processes control Nb enrichment and mineralization in syenitic systems

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

《岩浆与热液过程解耦控制正长岩系铌富集与成矿作用》的补充表S1至S7
表S1：电子探针显微分析（EPMA）与激光剥蚀电感耦合等离子体质谱（LA-ICP-MS）分析所用标准物质；
表S2：百草侵入体与白马侵入体中辉石的主量元素组成及单位化学式原子数（Atoms per Formula Unit，apfu）；
表S3：百草侵入体与白马侵入体中各矿物的微量元素组成；
表S4：百草侵入体与白马侵入体中正长岩的全岩Sr-Nd同位素组成结果；
表S5：百草侵入体与白马侵入体中岩浆锆石的Hf-O同位素组成；
表S6：百草地区高钛玄武岩的主量元素与微量元素组成；
表S7：百草与白马地区的模拟实验结果