意大利蒙特拉马佐矿山罗萨斯石-孔雀石组的新成员 Perchiazziite、Co2(CO3)(OH)2

Anna Barbaro, F. Nestola, A. Kasatkin, Matteo Ardit, Nicola Rotiroti, R. Škoda, A. Agakhanov, M. C. Dalconi, Fabrizio Castellaro
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The main bands in the Raman spectrum are at 154, 511, 707, 1085, 1526, 3304, aXnd 3479 cm−1. The chemical composition (by electron microprobe; CO2 and H2O by stoichiometry) of perchiazziite is (in wt.%): MgO 1.81, CaO 0.41, MnO 0.32, FeO 0.12, CoO 32.45, NiO 4.02, CuO 5.40, ZnO 25.60, CO2 20.63, H2O 8.42, total 99.18. The empirical formula calculated on the basis of 5 O apfu is: (Co0.93Zn0.67Cu0.15Ni0.12Mg0.10Ca0.02Mn0.01)Σ2.00(CO3)(OH)2. The crystal structure was refined by the Rietveld method. Perchiazziite is monoclinic, space group P21/a, a = 12.1832(16) Å, b = 9.3187(16) Å, c = 3.1570(3) Å, β = 97.165(15)°, V = 355.62(8) Å3, and Z = 4. The strongest lines of the X-ray powder diffraction pattern [d, Å (I, %) (hkl)] are 6.040 (22) (200), 5.073 (38) (210), 3.694 (53) (220), 2.599 (100) (021), 2.535 (26) (420), 2.480 (27) (221̄), 2.140 (26) (231̄), 1.561 (25) (202̄). 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引用次数: 0

摘要

Perchiazziite(理想状态下为 Co2(CO3)(OH)2)是在意大利利古里亚热那亚省 Monte Ramazzo 矿发现的一种新矿物。它呈球状聚集,直径可达 0.1 毫米,由非常细的纤维组成。它们形成于主要由鹅卵石和磁铁矿组成的基质上,并与方解石和共生孔雀石伴生。蛭石聚集体的外表面呈淡橙粉色,但在薄片上呈白色。它呈半透明状,带有白色条纹,具有丝绸般的光泽,韧性较脆,断口不均匀。未观察到劈裂和分离现象。莫氏硬度为 4。Dcalc. = 3.970 g/cm3。用 Gladstone-Dale 公式计算得出的平均折射率为 1.77。拉曼光谱的主要波段在 154、511、707、1085、1526、3304 和 3479 cm-1 处。橄榄石的化学成分(通过电子显微探针;通过化学计量法测定 CO2 和 H2O)为(单位:重量百分比):MgO 1.81,CaO 1.81,CrO 1.81:氧化镁 1.81,氧化钙 0.41,氧化锰 0.32,氧化铁 0.12,氧化钴 32.45,氧化镍 4.02,氧化铜 5.40,氧化锌 25.60,二氧化碳 20.63,水 8.42,总计 99.18。根据 5 O apfu 计算得出的经验公式为:(Co0.93Zn0.67Cu0.15Ni0.12Mg0.10Ca0.02Mn0.01)Σ2.00(CO3)(OH)2。晶体结构是通过里特维尔德法精制而成的。Perchiazziite 为单斜晶体,空间群为 P21/a,a = 12.1832(16) Å,b = 9.3187(16) Å,c = 3.1570(3) Å,β = 97.165(15) °,V = 355.62(8) Å3,Z = 4。X 射线粉末衍射图样的最强线[d, Å (I, %) (hkl)] 为 6.040 (22) (200)、5.073 (38) (210)、3.694 (53) (220), 2.599 (100) (021), 2.535 (26) (420), 2.480 (27) (221̄), 2.140 (26) (231̄), 1.561 (25) (202̄).Perchiazziite 是玫瑰石-孔雀石组的一个新成员。
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Perchiazziite, Co2(CO3)(OH)2, a New Member of the Rosasite–Malachite Group from the Monte Ramazzo Mine, Italy
Perchiazziite, ideally Co2(CO3)(OH)2, is a new mineral discovered at the Monte Ramazzo Mine, Genova Province, Liguria, Italy. It occurs as globular aggregates up to 0.1 mm in diameter, composed of very thin fibers. These develop on a matrix composed mostly of goethite and magnetite, in association with calcite and Co-bearing malachite. Aggregates of perchiazziite are pale orange-pink on their outer surfaces but white in thin section. It is translucent with white streak, silky luster, brittle tenacity, and uneven fracture. No cleavage and parting are observed. The Mohs hardness is ∼4. Dcalc. = 3.970 g/cm3. The mean refractive index calculated using the Gladstone-Dale equation is 1.77. The main bands in the Raman spectrum are at 154, 511, 707, 1085, 1526, 3304, aXnd 3479 cm−1. The chemical composition (by electron microprobe; CO2 and H2O by stoichiometry) of perchiazziite is (in wt.%): MgO 1.81, CaO 0.41, MnO 0.32, FeO 0.12, CoO 32.45, NiO 4.02, CuO 5.40, ZnO 25.60, CO2 20.63, H2O 8.42, total 99.18. The empirical formula calculated on the basis of 5 O apfu is: (Co0.93Zn0.67Cu0.15Ni0.12Mg0.10Ca0.02Mn0.01)Σ2.00(CO3)(OH)2. The crystal structure was refined by the Rietveld method. Perchiazziite is monoclinic, space group P21/a, a = 12.1832(16) Å, b = 9.3187(16) Å, c = 3.1570(3) Å, β = 97.165(15)°, V = 355.62(8) Å3, and Z = 4. The strongest lines of the X-ray powder diffraction pattern [d, Å (I, %) (hkl)] are 6.040 (22) (200), 5.073 (38) (210), 3.694 (53) (220), 2.599 (100) (021), 2.535 (26) (420), 2.480 (27) (221̄), 2.140 (26) (231̄), 1.561 (25) (202̄). Perchiazziite is a new member of the rosasite–malachite group.
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