首页> 外文期刊>Doklady Earth Sciences >Conditions of the Formation of Unique Mineralization with Yushkinite V_(1-x)S • n[(Mg,Al)(OH)_2] in Quartz-Calcite Veins,Pai-Khoi Ridge: Evidence from Study of Fluid Inclusions
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Conditions of the Formation of Unique Mineralization with Yushkinite V_(1-x)S • n[(Mg,Al)(OH)_2] in Quartz-Calcite Veins,Pai-Khoi Ridge: Evidence from Study of Fluid Inclusions

机译:在石英 - 方解石静脉中,玉石岩V_(1-X)的独特矿化的条件与玉石岩v_(1-x)S•n [(mg,al)(OH)_2],Pai-Khoi岭:来自液体夹杂物研究的证据

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摘要

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.
机译:据报道,石英中石英中液体夹杂物的研究结果报告了石英方解石静脉,具有独特的玉柳矿化。首次首次证明其形成在急剧还原条件下发生。矿物质形成培养基富含钙和氯化镁和硫化氢。矿物质形成的温度为〜120-150°С。

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