摘要

The partial isothermal section of the Fe-Sn-Zr system at 900 degrees C reported in Ref [7] was completed. As compared with this section, three new ternary compounds were evidenced (Y, 06 and Fe(6)Sn(6)Zr), one compound previously reported with a homogeneity domain (X) was shown to consist in fact of two separate compounds with close compositions (X' and X '') The crystal structure of the previously reported N phase was determined ab initio from powder diffraction data.

  • 出版日期2010-11
  • 单位中国地震局