The results of the study of fluid inclusions in quartz from quartz–calcite veins with unique yushkinite mineralization are reported. For the first time, it was proved that their formation occurred under sharply reducing conditions. The mineral formation medium was enriched in calcium and magnesium chlorides and hydrogen sulfide. The temperature of mineral formation was ~120–150°С.

中文翻译：

---

Yushkinite V1 – xS · n[(Mg,Al)(OH)2] 在 Pai-Khoi 山脊石英-方解石脉中形成独特矿化的条件：来自流体包裹体研究的证据

报告了对来自具有独特玉什金矿化作用的石英-方解石脉的石英中流体包裹体的研究结果。首次证明它们的形成是在急剧还原的条件下发生的。矿物形成介质富含氯化钙和氯化镁以及硫化氢。矿物形成的温度为~120-150°С。