Dve nové lokality pyromorfitu v Slovenskej republike: Chvojnica a Hnilčík

Q3 Earth and Planetary Sciences Bulletin Mineralogie Petrologie Pub Date : 2022-01-01 DOI:10.46861/bmp.30.038
Martin Števko, Jiří Sejkora, František Kuraj, Matej Rybárik
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Abstract

Two new localities of pyromophite were recently discovered at the Chvojnica base metals occurrence in the Strážovské vrchy Mts. (Tatric Unit), and at the supergene zone of the Piata siderite-type hydrothermal vein near Hnilčík (Spišsko-gemerské rudohorie Mts., Gemeric Unit), Slovak Republic. At the Chvojnica occurrence pyromorphite occurs as bright green crystalline crusts and radial aggregates up to 3 mm developed in cavities and fractures in the porous quartz gangue with relicts of primary galena. It is associated with minor crystalline coatings of cerussite. The refined unit-cell parameters of pyromorphite from Chvojnica (for the hexagonal space group P63/m) are a 9.9750(2) Å, c 7.3569(2) Å and V 633.93(2) Å3. Except of dominant contents of Pb, P and Cl, only minor amounts of Ca (up to 0.10 apfu), Al (up to 0.05 apfu), Fe (up to 0.04 apfu), As (up to 0.05 apfu) and S (up to 0.02 apfu) were detected in studied pyromorphite. At the Hnilčík, pyromorphite occurs rarely in the cavities of the cavernous quartz-limonite gangue in the supergene zone of the Piata vein. It forms colourless to very light green prismatic crystals up to 2 mm in size, or crystalline aggregates associated with goethite, Mn oxides and malachite. The refined unit-cell parameters of pyromorphite from Hnilčík (for the hexagonal space group P63/m) are a 9.9484(15) Å, c 7.315(2) Å, V 627.0(2) Å3 (Ca-poor) and a 9.8983(6) Å, c 7.2589(8) Å, V 615.92(9) Å3 (Ca-rich). Pyromorphite from Hnilčík shows strong chemical zoning caused by variation of Pb and Ca contents, with outer parts of the crystals enriched in Ca. Contents of Ca are ranging between 0.09 to 0.96 apfu, with the atomic Pb/(Pb+Ca) ratio ranging from 0.98 to 0.81, which is close to the compositional boundary with phosphohedyphane. Interesting are also elevated concentrations of Cu reaching up to 0.07 apfu. Other minor elements detected in pyromorphite from Hnilčík are As (up to 0.12 apfu), Al, V and S (all up to 0.02 apfu).
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斯洛伐克共和国境内两处新的火山灰岩遗址:Chvojnica和Hnilčík
最近在斯洛伐克共和国Strážovské vrchy Mts. (Tatric单元)的Chvojnica贱金属矿床和Hnilčík (Spišsko-gemerské rudohorie Mts., generic单元)附近的Piata菱铁矿型热液脉的表生带发现了两个新的辉绿铁矿地点。在Chvojnica产状中,焦闪石以亮绿色结晶结壳的形式出现,在多孔石英脉石的孔洞和裂缝中发育着长达3毫米的放射状聚集体,伴有原生方铅矿的残余。它与少量的铜矿结晶涂层有关。Chvojnica焦闪石(六边形空间群P63/m)的精细化单位胞参数为:a 9.9750(2) Å, c 7.3569(2) Å和V 633.93(2) Å3。除Pb、P和Cl的主要含量外,还检出少量的Ca(可达0.10 apfu)、Al(可达0.05 apfu)、Fe(可达0.04 apfu)、As(可达0.05 apfu)和S(可达0.02 apfu)。在Hnilčík处,皮亚塔脉表生带海绵状石英-褐铁矿脉石的孔洞中很少出现焦闪石。它形成无色到非常浅绿色的棱柱状晶体,大小可达2毫米,或与针铁矿、锰氧化物和孔雀石相关的结晶聚落。从Hnilčík(对于六边形空间群P63/m)得到的焦闪石的精化单位胞参数为:9.9484(15)Å, c 7.315(2) Å, V 627.0(2) Å3(贫钙)和9.8983(6)Å, c 7.2589(8) Å, V 615.92(9) Å3(富钙)。Hnilčík焦闪石中Pb、Ca含量变化引起的化学分带性较强,晶体外部富集Ca, Ca含量在0.09 ~ 0.96 apfu之间,Pb/(Pb+Ca)原子比值在0.98 ~ 0.81之间,接近与磷磷脂的组成边界。有趣的是,铜的浓度也升高了,高达0.07 apfu。在Hnilčík的焦闪石中检测到的其他微量元素有As(高达0.12 apfu), Al, V和S(均高达0.02 apfu)。
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Bulletin Mineralogie Petrologie
Bulletin Mineralogie Petrologie Earth and Planetary Sciences-Economic Geology
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期刊介绍: Bulletin Mineralogie Petrologie is a peer-reviewed journal focused especially on: mineralogy, crystal chemistry and study of crystal structures of minerals study of mineral associations and processes of their origin meteoritics, research of tectites economic geology (of ore deposits) and study of history of mining of ore deposits topographic mineralogy petrology of igneous, metamorphic and sedimentary rocks instrumental analytical methods at mineralogy and petrology mineralogy and petrology as tools for archeology and similar disciplines
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