花岗岩相关关键金属共生成矿的实验地球化学研究进展

Key Points

• This research investigates the mineralization mechanisms of key metals associated with granite, focusing on controlling factors.
• Conducted high-temperature and high-pressure experiments to simulate mineralization processes.
• Examined the effects of volatiles (F, Cl, S, H2O) on metal mobility and precipitation.
• Quantified partitioning behaviors of metals between melt and fluid phases.
• F and Cl mainly control the migration of rare metals (W, Sn, Be, Nb, Ta) and precious metals (Au, Ag, Cu, Pb, Zn).
• High fO2 conditions favor Cu and Au enrichment, while low fO2 promotes Sn, Pb, and Zn mineralization.
• Quantitative characterization of melt-fluid partition coefficients (D) provides key parameters for assessing mineralization potential.