Fluid inclusion microthermometry was conducted on late‐stage barren comb quartz and the latest stibnite at the Hishikari deposit to characterize the hydrothermal activity responsible for vein formation. Eight fluid inclusion assemblages (i.e. fluid inclusions trapped at the same time, ‘FIAs’) were studied to determine the formation fluid temperatures and salinities for the comb quartz in the Shosen No. 2 vein, Sanjin ore zone, and the stibnite in the Seisen No. 1–1 vein, Yamada ore zone.

中文翻译：

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日本Hishikari Au-Ag超热矿床中梳状石英和辉锑矿的流体包裹体研究

在后期贫瘠的梳状石英和Hishikari矿床上的最新辉辉石上进行了流体包裹体热分析，以表征导致静脉形成的水热活动。研究了八个流体包裹体组合（即，同时捕获的流体包裹体，称为“ FIA”），以确定Shosen 2号矿脉，三金矿带和梳状辉长岩中的梳状石英的地层流体温度和盐度。山田矿区1-1号矿脉。