New Minerals from the Redmond Mine, North Carolina, USA: V. Finescreekite and Hayelasdiite, Two New Thiosulfate Minerals Containing Cubane-Like Pb4O4 Structural Units

A. R. Kampf, Jason B. Smith, John M. Hughes, Chiu‐Shun Ma, Christopher R. Emproto
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Abstract

The new minerals finescreekite, [Pb4(OH)4](S2O3)2 (IMA2022–030), and hayelasdiite, [Pb4O1.5(OH)2.5]2[Cu+5(S2O3)4(S2O2OH)2(H2O)]·4H2O (IMA2022–021), were found in the Redmond mine, Haywood County, North Carolina, USA, where they occur in a highly unusual secondary assemblage that comprises a variety of rare Pb-Zn-Cu sulfates, thiosulfates, and carbonates. Finescreekite was found in close association with anglesite, cubothioplumbite, redmondite, and steverustite. Hayelasdiite was found in close association with anglesite and steverustite. Finescreekite properties: colorless tablets to about 1.5 mm across; white streak; resinous to adamantine luster; brittle; Mohs hardness ∼ 2½; curved, stepped fracture; excellent cleavage on {001}, fair on {100}, {010}, and {110}; 5.675 g/cm3 calculated density; biaxial (−) with α = 2.00(1), β = 2.04(calc), γ = 2.065(calc), 2V = 75.9(5)°. Hayelasdiite properties: colorless prisms and blades to about 0.5 mm in length; white streak; vitreous to subadamantine luster; brittle; Mohs hardness ∼ 2½; curved fracture; perfect cleavage on {010}; 4.909 g/cm3 calculated density; biaxial (−) with α = 1.89(1), β = 1.95(calc), γ = 1.97(calc), 2V = 58(5)°. Electron probe microanalyses provided the empirical formulae [Pb4(OH)4](S2O3)1.76(SO4)0.24 and [Pb4.00O1.5(OH)2.5]2[Cu+5.00(S2O3)3.24(SO4)0.76(S2O2OH)2(H2O)]·4H2O for finescreekite and hayelasdiite, respectively. Finescreekite is Orthorhombic, P212121, a = 8.2330(9), b = 10.7128(13), c = 14.8256(13) Å, V = 1307.6(2) Å3, and Z = 4. Hayelasdiite is triclinic, P1̄, a = 7.52089(15), b =14.9345(3), c = 17.9895(13) Å, α = 106.727(8), β = 90.966(6), γ = 90.031(6)°, V = 1934.79(16) Å3, and Z = 2. The structures of finescreekite (R1 = 0.061 for 1440 I > 2σI) and hayelasdiite (R1 = 0.055 for 5636 I > 2σI) both contain cubane-like Pb4O4 clusters, [Pb4(OH)4]4+ in finescreekite and [Pb4O1.5(OH)2.5]2.5+ in hayelasdiite. The structure of hayelasdiite also contains a decorated double chain with the formula [Cu+5(S2O3)4(S2O2OH)2(H2O)]5−.
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美国北卡罗来纳州雷德蒙德矿区的新矿物:V. Finescreekite 和 Hayelasdiite,两种含有类似古巴 Pb4O4 结构单元的新硫酸盐矿物
在海伍德县雷德蒙德矿区发现了新矿物细溪石[Pb4(OH)4](S2O3)2 (IMA2022-030)和霞石[Pb4O1.5(OH)2.5]2[Cu+5(S2O3)4(S2O2OH)2(H2O)]-4H2O(IMA2022-021)发现于美国北卡罗来纳州海伍德县的雷德蒙德矿,它们出现在一个非常不寻常的次生集合体中,该集合体由各种稀有的铅锌铜硫酸盐、硫代硫酸盐和碳酸盐组成。细长溪石与角闪石、立方硫锑矾土、红芒硝和石英岩密切相关。海拉斯迪石与角闪石和石榴石密切相关。细闪长岩的性质:无色片状,直径约 1.5 毫米;白色条纹;树脂光泽至金刚光泽;脆性;莫氏硬度 ∼ 2½;弯曲的阶梯状断口;{001}上的裂隙极佳,{100}、{010}和{110}上的裂隙一般;5.计算密度为 675 g/cm3;双轴(-),α = 2.00(1),β = 2.04(calc),γ = 2.065(calc),2V = 75.9(5)°。Hayelasdiite 的性质:无色棱柱和叶片,长约 0.5 毫米;白色条纹;玻璃光泽至亚金刚光泽;脆性;莫氏硬度 ∼ 2½;弯曲断口;{010}上有完美的劈理;计算密度为 4.909 克/立方厘米;双轴(-),α = 1.89(1),β = 1.95(calc),γ = 1.97(calc),2V = 58(5)°。电子探针显微分析提供了细长溪石和黑云母的经验公式:[Pb4(OH)4](S2O3)1.76(SO4)0.24 和 [Pb4.00O1.5(OH)2.5]2[Cu+5.00(S2O3)3.24(SO4)0.76(S2O2OH)2(H2O)]-4H2O。细长石为正长方晶,P212121,a = 8.2330(9),b = 10.7128(13),c = 14.8256(13)埃,V = 1307.6(2)埃3,Z = 4。Hayelasdiite 为三棱体,P1̄,a = 7.52089(15),b = 14.9345(3),c = 17.9895(13)埃,α = 106.727(8),β = 90.966(6),γ = 90.031(6)°,V = 1934.79(16)埃3,Z = 2。细溪石(R1 = 0.061,1440 I > 2σI)和干腊石(R1 = 0.055,5636 I > 2σI)的结构都含有类似立方体的 Pb4O4 团簇,细溪石中为 [Pb4(OH)4]4+,干腊石中为 [Pb4O1.5(OH)2.5]2.5+。霞石的结构中还含有一条装饰双链,其结构式为[Cu+5(S2O3)4(S2O2OH)2(H2O)]5-。
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