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兴安石的晶体结构
CRYSTAL STRUCTURE OF XINGANITE
【摘要】 兴安石是我国新发现的一种富含稀土、铍的硅酸盐新矿物,其理想的化学式为(Y,Ce)BeSiO4(OH)。该矿物属于单斜晶系,利用四圆单晶衍射仪收集强度数据,测得α=4.7681±0.00263,b=7.6757±0.00686,c=9.9301±0.00639;α=90°,β=90.17°±0.053°,γ=90°;空间群为P21/c;Z=4。利用直接法及电子密度函数法测定了晶体结构,经最小二乘修正,最后的偏离因子R=0.086。 结构测定结果证实兴安石具有硅硼钙石的结构类型,与羟磷铍钙石,硅铍钇矿等均属同构似型矿物。
【Abstract】 Xinganite, a new mineral discovered in China, is a REE-Be-rich silicate. The ideal formula is: (Y, Ce) BeSiO4(OH). The mineral is monoclinic. The intensity data were collected with a single-crystal four-circle diffractometer. The cell parameters are: a=4.7681(±0.00263), b=7.6757(±0.00686), c=9.9301(±0.00639), α=90°,β=90.17°(±0.0053°),γ=90°, Space group P21/c. Z=4. The crystal structure has been determined by direct methods and electron-density synthesis methods. The least squares refinement gave a final discrepancy index R=0.086.The crystal structural analysis shows that xinganite is of datolite-type structure.
- 【文献出处】 矿物学报 ,Acta Mineralogica Sinica , 编辑部邮箱 ,1985年04期
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