来自卢萨蒂亚山脉Cvikov附近Křížovývrch的Zephylite、tobermolite、氟叶沸石-(K)和伴随的沸石矿化作用(捷克共和国)

Q3 Earth and Planetary Sciences Bulletin Mineralogie Petrologie Pub Date : 2023-01-01 DOI:10.46861/bmp.31.065
P. Pauliš, Libor Hrůzek, J. Sejkora, Oldřich Janeček, Ondřej Pour, Bohuslav Bureš, Blanka Šreinová
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引用次数: 0

摘要

在捷克共和国位于Cvikov东北1.5 km, Česká Lípa、Lužické hory山脉东北13 km的Křížový vrch山西坡(a.s.l 443 m)小废弃采石场的新生代玄武岩岩洞中发现了沸石、钙辉石、钙辉石、氟辉石-(K)及其伴生沸石。沸石形成无色球形聚集体,具有珍珠般的光泽,通常大小为3 - 4毫米,很少观察到直径达1厘米的聚集体。它是三角形的,空间群R-3,其单位胞参数由PXRD细化:a 9.362(2), c 36.470(12) Å和V = 2768.3(1.2) Å3。分子式为(Ca12.84Na0.07)Σ12.91(Si9.83Al0.26)Σ10.09 O28(OH)1.43 F8.42·6H2O。托贝莫里石以白色的半球形或球形聚集体出现,大小可达1厘米,它取代了早期的沸石。它是单斜的,空间群Bm,其单位胞参数由PXRD改进:a 6.714(4), b 17.375(4), c 22.670(8) Å, γ 123.31(3)°和V 938.2(1.3) Å3。化学分析表明,经验式为(Ca4.55Na0.03K0.02)Σ4.60(Si5.40Al0.60)Σ6.00O15.56(OH)1.44·5H2O的托伯莫里石与经验式为(Ca3.99Na0.04)Σ4.03(Si5.60Al0.40)Σ6.00O14.62(OH)2.38·5H2O的贫钙基诺托伯莫里石相结合。氟磷灰石-(K)形成丰富的棱柱状晶体,大小可达0.5 - 2厘米。无色至白色,具有玻璃状至油腻状光泽。它是四边形的,空间群为P4/mnc,其单胞参数由PXRD得到:a为9.0157(13),c为15.7889(19)Å, V = 1283.4(3) Å3。氟泡石-(K)的化学分析对应于实验式(K0.81Na0.24)Σ1.05Ca4.06(Si7.25Al0.47)Σ8.00O20F1.05·8H2O。伴生沸石有钙方石、钙方石、钙方石和钾方石;文中给出了它们的PXRD数据、单胞参数和化学成分。
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Zeofylit, tobermorit, fluorapofylit-(K) a doprovodná zeolitová mineralizace z Křížového vrchu u Cvikova v Lužických horách (Česká republika)
Zeophyllite, tobermorite, kenotobermorite, fluorapophylite-(K) and associated zeolites were found in cavities of Cenozoic basaltic rocks of small abandoned quarry at western slope of the Křížový vrch hill (443 m a.s.l.), 1.5 km NE from Cvikov, 13 km NNE from Česká Lípa, Lužické hory Mountains, Czech Republic. Zeophyllite forms colorless spherical aggregates with pearly lustre usually 3 - 4 mm in size, aggregates with diameter up to 1 cm were observed only rarely. It is trigonal, space group R-3, with unit-cell parameters refined from PXRD: a 9.362(2), c 36.470(12) Å and V = 2768.3(1.2) Å3. Chemical analyses of zeophyllite correspond to the empirical formula (Ca12.84Na0.07)Σ12.91(Si9.83Al0.26)Σ10.09 O28(OH)1.43 F8.42· 6H2O. Tobermorite occurs as snow-white hemispherical to spherical aggregates up to 1 cm in size, it replaces earlier zeophyllite. It is monoclinic, space group Bm, with unit-cell parameters refined from PXRD: a 6.714(4), b 17.375(4), c 22.670(8) Å, γ 123.31(3)° and V 938.2(1.3) Å3. On the base of chemical analyses, tobermorite with empirical formula (Ca4.55Na0.03K0.02)Σ4.60(Si5.40Al0.60)Σ6.00O15.56(OH)1.44·5H2O is accompanied by more rare Ca-poor kenotobermorite with empirical formula (Ca3.99Na0.04)Σ4.03(Si5.60Al0.40)Σ6.00O14.62(OH)2.38·5H2O. Fluorapophyllite-(K) forms abundant prismatic crystals up to 0.5 - 2 cm in size. It is colorless to white with vitreous to greasy lustre. It is tetragonal, space group P4/mnc, with unit-cell parameters refined from PXRD: a 9.0157(13), c 15.7889(19) Å and V = 1283.4(3) Å3. Chemical analyses of fluorapophyllite-(K) correspond to the empirical formula (K0.81Na0.24)Σ1.05Ca4.06(Si7.25Al0.47)Σ8.00O20F1.05· 8H2O. Other zeolites, thomsonite-Ca, chabazite-Ca, phillipsite-Ca and -K, were found in association; their PXRD data, unit-cell parameters and chemical compositions are given in the paper.
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来源期刊
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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