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首页> 外文期刊>Doklady Earth Sciences >New Pb-As-Bearing Eulytite from the Galechnoe Deposit, Eastern Yakutia
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New Pb-As-Bearing Eulytite from the Galechnoe Deposit, Eastern Yakutia

机译:雅库特东部加勒奇诺矿床中新的含铅辉绿岩

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摘要

Eulytite, Bi_4(SiO_4)_3, is a rare mineral. Since its discovery in Schneeberg and Johanngeorgenstadt (Saxony, Germany) by Breithaupt in 1827, this mineral has been reported from only a few other localities: Hechts-berg and the Clara Mine (Germany), Dognecea (Romania), Cornwall (England), Southwick Cliffs (Scotland), the Evans-Lou quarry (Canada), Pala pegmatites (United States), Smrkovec (Czech Republic), and Wombat Hill, Australia. In all the deposits, the eulytite associates with Bi-bearing minerals: bismuth-ite, bismuthinite, and native bismuth. Eulytite from the Uralian deposits was studied in cathode and UV rays. However, its exact locality, chemistry, physical properties, and relations with other minerals were not reported. Hence, the data reported below can be considered the description of the first reliable finding of eulytite in Russia.
机译:尤利特石Bi_4(SiO_4)_3是一种稀有矿物。自从Breithaupt于1827年在Schneeberg和Johanngeorgenstadt(德国萨克森州)发现该矿物以来,仅在其他几个地方报道过这种矿物:Hechts-berg和Clara矿山(德国),Dognecea(罗马尼亚),Cornwall(英格兰), Southwick Cliffs(苏格兰),Evans-Lou采石场(加拿大),Para伟晶岩(美国),Smrkovec(捷克共和国)和澳大利亚Wombat Hill。在所有矿床中,辉绿岩均与含铋矿物质相关联:铋矿,铋锰矿和原生铋。在阴极和紫外线下研究了来自乌拉尔矿床的尤利特沸石。但是,尚未报告其确切的位置,化学性质,物理性质以及与其他矿物的关系。因此,下面报告的数据可以被认为是对俄罗斯首次成功的发现的评价的描述。

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