在保加利亚首次发现osakaite矿物Zn4(OH)6(SO4)•5H2O

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
P. Petrov, T. Stanimirova, Svetla Stariradeva
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引用次数: 0

摘要

Osakaite是保加利亚的一种新矿物,是在南罗多彼南Petrovitsa矿床的Gyudyurska矿的钟乳石中发现的。化学成分决定了Cu2+的同构包合和(Zn3Cu)(OH)6(SO4)•5H2O的组成。该矿物是通过锌和铜硫化矿的矿井水相互作用的产物。在长时间的大气条件下储存,部分赤玉石晶体脱水形成矿物Zn3Cu(OH)6(SO4)•4H2O和lahnsteinite Zn3Cu(OH)6(SO4)•3H2O。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
First occurrence of the mineral osakaite Zn4(OH)6(SO4)•5H2O for Bulgaria
Osakaite, a new mineral for Bulgaria, was discovered in stalactites from the Gyudyurska mine, South Petrovitsa deposit, South Rhodope. The chemical composition determines isomorphous inclusion of Cu2+ and composition (Zn3Cu)(OH)6(SO4)•5H2O. The mineral is a product of the interaction of mine waters passing through Zn and Cu-sulfide ores. During prolonged storage in atmospheric conditions, part of the osakaite crystals were dehydrated to the formation of the minerals namuwite Zn3Cu(OH)6(SO4)•4H2O and lahnsteinite Zn3Cu(OH)6(SO4)•3H2O.
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