首页|於祖相石,Sr3Fe3+(Si2O6)2(OH)·3H2O:一种链状硅酸盐新矿物

於祖相石,Sr3Fe3+(Si2O6)2(OH)·3H2O:一种链状硅酸盐新矿物

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於祖相石发现于南非北开普省卡拉哈里锰矿田韦瑟尔锰矿,呈浅棕色微晶-纳米纤维状集合体产出,集合体粒度50~200 μm,共生矿物有硅镁锶钠石(meieranite)、羟钾锶鱼眼石[hydroxymcglassonite-(K)]、钠锂大隅石(sugilite)、针钠钙石(pectolite)、霓石等,呈玻璃光泽,具平行(10 0)及(0 0 1)的完全解理,估测莫氏硬度3-31/2,计算密度3.451 g·cm-3.在光学显微镜下,於祖相石为无色-浅黄色的针状、纤维状晶体,单晶体粒径<3 μm,二轴晶负光性,α=1.66(3),β=1.68(5),γ=1.72(3)(白光),2Vcal=72°.其拉曼光谱出现100~1500 cm-1范围里22个拉曼位移峰,归属Si—O,Fe—O,Sr—O振动模式,1500~4000 cm-1范围里出现5个拉曼位移峰,归属OH,H2O的振动模式.其经验化学式为(Sr2.94Pb0.04Ca0.02)∑3(Fe0.91Al0.09)∑1[(Si3.98 Al0.02)∑4O12](OH)·3H2O,理想式Sr3Fe(Si2O6)2(OH)·3H2O.X射线单晶衍射结构分析确定於祖相石为单斜晶系,空间群P21/m,晶胞参数a=11.1035(10)Å,b=7.8463(7)Å,c=7.8222(7)Å,β=101.406(8)°,V=668.02(11)Å3,Z=2.於祖相石与水硅钛锶石(ohmilite)等结构,由2条平行的SiO4四面体单链(2T4p)夹FeO4(OH)2八面体链形成平行b轴的复合链,链间空隙分布Sr2+和H2O分子.其X射线粉晶衍射最强线条为:d Å(I%,hkl):4.632(92,1 1 1),3.486(100,0 2 1),3.291(67,02 1),3.065(57,-2 2 1),2.841(48,3 1 1),2.118(49,3 3 0),1.956(46,0 4 0).於祖相石的命名以致敬和纪念矿物学家於祖相教授(1930-2019)的学术贡献.
Yuzuxiangite,Sr3Fe3+(Si2O6)2(OH)·3H2O:a new inosilicate mineral
Yuzuxiangite was discovered in the Wessels Mine,Kalahari Mangnese Field,North Cape Province of Africa.It occurs as agglomerates of acicular and fiberous crystals,50-200 μm in size of the aggregate,in association with meieranite,hydroxymcglassonite-(K),sugilite,pectolite and aegirine.It has light brown color,vitreous lustre,perfect cleavages parallel to(1 0 0)and(0 0 1),an estimated Mohs hardness of 3-31/2,and the calculated desity of 3.451 g·cm-3.Under microscope of transmittance light,yuzuxiangite is observed as colorless to light yellow acicular and fiberous crystals with single crystal size less than 3 μm in diameter.It is biaxial crystal(-),α=1.66(3),β=1.68(5),γ=1.72(3)(white),2Vcal=72°.Its Raman spectrum consists of 22 peaks in 100-1500 cm-1,belonging to the Si-O,Fe-O,and Sr-O vibration modes,and 5 peaks in 1500-4000 cm-1 belonging to OH and H2O vibration modes.Its ideal formula is Sr3Fe(Si2O6)2(OH)3H2O and its empirical formula(based on cation=8)is(Sr2.94Pb0.04Ca0.02)∑3(Fe0.91Al0.09)∑1[(Si3.98 Al0.02)∑4O12](OH)3H2O.The X-ray single crystal diffraction analysis confirms that uzuxiangite belongs to the monocliniccrystal system,with cell paramters of space group P21/m,a=11.1035(10)Å,b=7.8463(7)Å,c=7.8222(7)Å,β=101.406(8)°,V=668.02(11)Å3,Z=2.The crystal structure of yuzuxiangite is same with ohmiite,characterized by a composite chain parallel to the b-axis,composed of a chain of corner-shared FeO4(OH)2 octahedra flanked by 2 parallel chains(2T4p)of comer-shared SiO4 tetrahedra,leaving the surrounding space occupied by Sr and H2O.The strongest powder X-ray diffraction lines are of d Å(I%,hkl),including 4.632(92,111),3.486(100,0 2 1),3.291(67,0 2 1),3.065(57,-2 2 1),2.841(48,3 1 1),2.118(49,3 3 0),and 1.956(46,0 4 0).Yuzuxiangite is named in honor of Prof.YU Zuxiang(1930-2019),an eminent Chinese mineralogist with important contributions to studies of new minerals,especially to studies of platinum-group element minerals in China.

yuzuxiangiteohmiliteinosilicatenew mineralKalahari manganese fieldSouth Africa

谷湘平、杨和雄、谢先德、刘光华

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江西应用科技学院宝石与矿物资源学院,江西南昌 330100

中南大学 地球科学与信息物理学院,湖南长沙 410083

亚利桑那大学地球科学系,美国图森市第4街1040号,邮编AZ 85721-0077

中国科学院地球化学研究所矿物学与成矿学重点实验室/广东省矿物物理与材料重点实验室,广东 广州 510640

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於祖相石 水硅钛锶石 新矿物 链状硅酸盐 卡拉哈里锰矿田 南非

2024

矿物学报
中国矿物岩石地球化学学会 中国科学院地球化学研究所

矿物学报

CSTPCD北大核心
影响因子:1.2
ISSN:1000-4734
年,卷(期):2024.44(5)