Scheelite and gold-bearing mineralization in the ptasznik roof pendant, sudetes, poland

机译：波兰萨兹特山脉的ptasznik屋顶吊坠中的白钨矿和含金矿化

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Scheelite and gold-bearing mineralization in quartz veins and stockworks is a result of metasomatic and hydrothermal processes in metamorphic rocks of the Ptasznik roof pendant of the Klodzko-Zloty Stock intrusion. Scheelite-titanite mineralization preceding Au and/or sulphide-bearing quartz mineralization originated in zones of a strong silicification and K-feldspar metasomatism at the temperature of about 460 deg. Chemical analyses determined 0.3 wt.

机译：石英脉和储层中的白钨矿和含金矿化是Klodzko-Zloty储层侵入的Ptasznik屋顶悬垂变质岩中交代和热液作用的结果。含金和/或含硫化物的石英矿化之前的白钨矿-钛铁矿矿化起源于温度约为460度的强烈硅化和钾长石交代作用的区域。化学分析确定为0.3重量％。

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《Biennial SGA meeting;Quadrennial IAGOD symposium》|1999年|p.393-396|共4页
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S.Z.Mikulski;
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Scheelite and gold-bearing mineralization in the ptasznik roof pendant, sudetes, poland

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