Comparative study of Fe2B3O7 and Mn4(B6O13(OH)): a new structure linking melilite and johachidolite

Leonard C. Pasqualini, H. Huppertz
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引用次数: 0

Abstract

Abstract The two compounds Fe2B3O7 (a = 663.61(4), c = 438.39(3) pm, space group: P 4 ‾ $\overline{4}$ 21 m) and Mn4(B6O13(OH)) (a = 445.14(1), b = 683.56(2), c = 1330.34(3) pm, β = 90.42(1)°, space group: P21/c) were synthesized under high-pressure/high-temperature conditions of 9 GPa and 800 °C. Their crystal structures have been determined via single-crystal X-ray diffraction and the occurring side-phases have been identified. Fe2B3O7 crystallizes in the melilite structure type, whereas the novel structure of Mn4(B6O13(OH)) can be derived from the structures of the minerals melilite or johachidolite.
Fe2B3O7和Mn4(B6O13(OH))的比较研究:一种连接千英石和约绢石的新结构
摘要在9 GPa和800 ℃的高压/高温条件下合成了两个化合物Fe2B3O7 (a = 663.61(4), c = 438.39(3) pm,空间群:p4 $\overline{4}$ 21 m)和Mn4(B6O13(OH)) (a = 445.14(1), b = 683.56(2), c = 1330.34(3) pm, β = 90.42(1)°,空间群:P21/c)。通过单晶x射线衍射测定了它们的晶体结构,并确定了发生的侧相。Fe2B3O7结晶为千英石结构型,而Mn4(B6O13(OH))的新结构可来源于矿物千英石或约千英石的结构。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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