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首页> 外文期刊>Записки Российского минералогического общества >ALUMOFLUORIDES OF ZHARCHIKHINSKOYE MOLIBDENUM DEPOSIT (WESTERN TRANSBAIKALIA)
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ALUMOFLUORIDES OF ZHARCHIKHINSKOYE MOLIBDENUM DEPOSIT (WESTERN TRANSBAIKALIA)

机译:ZHARCHIKHINSKOE钼矿床(西跨界)的氟化物

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摘要

Infrequent alumofluorides have been found out in large quantity at the Zharchikhinskoye molibdenum deposit. The mineralization is located there within a tubular body of eruptive and explosive breccias. Alumofluoride association relates to the final stage of the ore forming process, where it made a paragenesis with quartz, galena, sphalerite, fluorite, siderite and dickite. The alumofluorides are presented by prosopite, ralstonite and gearksutite, the first two of them are considered as rare and even very rare mineral species.
机译:Zharchikhinskoye molibdenum矿床中发现了大量的氟化铝。矿化位于爆发性和爆发性角砾岩的管状体内。氟化铝缔合与矿石形成过程的最后阶段有关,在该过程中,它与石英,方铅矿,闪锌矿,萤石,菱铁矿和地开辉石共生。铝氟化物是由普苏普石,水钠钙石和硬硅钙石组成,其中前两种被认为是稀有甚至非常稀有的矿物。

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