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Xitieshanite——A New Ferric Sulphate Mineral
【摘要】 <正> Xitieshanite is a new ferric sulfate mineral discovered in the oxidation zone of a Pb-Zndeposit at Xitieshan,Qinghai Province,China.The typical crystal of xitieshanite is a rhom-bic rectangle.It is bright green in colour with a light yellow tint.Luster vitrous Translu-cent to almost transparent.Streak yellow.Cleavage imperfect.Fracture uneven or conchoi-dal.H.(Vickers)=62.6kg/mm2.Specific gravity=1.99obs.(2.02calc,).Pleochroism strong,andaxial colours:X=colourless to pale yellow,Y=pale yellow,Z=light yellow with greenishtint..It is optically positive,biaxial,2V=77°,r v.Refractive indices:Nx=1.536,Ny=1.570,Nz=1.628.Extinction parallel and inclined.Elongation positive and negative.X-raysingle-crystal study shows it is monoclinic.Space group P21/a.Unit cell parameters:a=14.102,b=6.908,c=10.673(?),β=111.266°,V=968.9,(?)3,Z=4.The powder pattern of xitie-shanite gave the strongest lines:6.67(6)(201),6.09(5)(110),5.69(5)(011),4.96(10)(002),4.81(10)(211),4.21(5)(112),and 3.90(9)(211).Chemical analysis gave Al2O3 0.01,Fe2O326.15,FeO 0.18,MgO 0.03,CaO 0.09,K2O 0.03,Na2O 0.07,SO3 27.69,H2O 45.02,total 99.27%,corresponding to the chemical formula:Fe3+ (SO4)(OH)·7H2O.The DTAcurve shows respectively three strong endothermic peaks at 85°,170°,and 735℃,anda weak peak at 460℃.The TGA curve shows a loss of weight in three different steps.The infrared spectral curve of xitieshanite demonstrates that it has two principal absorptionbands at 3,350 and 1,225—1,003 cm-1 and two subordinate bands at 1,620 and 603 cm-1.
【Abstract】 Xitieshanite is a new ferric sulfate mineral discovered in the oxidation zone of a Pb-Zn deposit at Xitieshan,Qinghai Province,China.The typical crystal of xitieshanite is a rhom- bic rectangle.It is bright green in colour with a light yellow tint.Luster vitrous Translu- cent to almost transparent.Streak yellow.Cleavage imperfect.Fracture uneven or conchoi- dal.H.(Vickers)=62.6kg/mm2.Specific gravity=1.99obs.(2.02calc,).Pleochroism strong,and axial colours:X=colourless to pale yellow,Y=pale yellow,Z=light yellow with greenish tint..It is optically positive,biaxial,2V=77°,r v.Refractive indices:Nx=1.536,Ny= 1.570,Nz=1.628.Extinction parallel and inclined.Elongation positive and negative.X-ray single-crystal study shows it is monoclinic.Space group P21/a.Unit cell parameters:a= 14.102,b=6.908,c=10.673(?),β=111.266°,V=968.9,(?)3,Z=4.The powder pattern of xitie- shanite gave the strongest lines:6.67(6)(201),6.09(5)(110),5.69(5)(011),4.96(10)(002), 4.81(10)(211),4.21(5)(112),and 3.90(9)(211).Chemical analysis gave Al2O3 0.01,Fe2O3 26.15,FeO 0.18,MgO 0.03,CaO 0.09,K2O 0.03,Na2O 0.07,SO3 27.69,H2O 45.02, total 99.27%,corresponding to the chemical formula:Fe3+ (SO4)(OH)·7H2O.The DTA curve shows respectively three strong endothermic peaks at 85°,170°,and 735℃,and a weak peak at 460℃.The TGA curve shows a loss of weight in three different steps. The infrared spectral curve of xitieshanite demonstrates that it has two principal absorption bands at 3,350 and 1,225—1,003 cm-1 and two subordinate bands at 1,620 and 603 cm-1.
- 【文献出处】 Geochemistry(English Language Edition) ,地球化学(英文版) , 编辑部邮箱 ,1983年03期
- 【被引频次】1
- 【下载频次】13