Observation shows that phase separation and fluid cooling drive gold precipitation in hydrothermal deposits, highlighting mineralization processes.
Table S1: LA-ICP-MS U-Pb zircon data of quartz diorite porphyry. Table S2: In situ LA-ICP-MS U-Pb data of hydrothermal monazite. Table S3: Trace element compositions of pyrite from different stages. Table S4: Trace element compositions of arsenopyrite from different stages. Table S5: Sulfur isotopic compositions of pyrite and arsenopyrite. Table S6: Summary of the microthermometric data for fluid inclusions from different mineralization stages.
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Zhang et al. (2025) studied this question.
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