,Phase Transition and EOS of Marmatite (Zn0.76Fe0.23S) up to 623 K and 17 Gpa

• 作 者: JIANG Xi ZHOU Wen-Ge XIE Hong-Sen LIU Yong-Gang FAN Da-Wei LIU Jing LI Yan-Chun LUO Chong-Ju MA Mai-Ning
• 机 构: Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002“,”Graduate School of Chinese
• 出 处: 中国物理快报（英文版）
• 发表日期: 2007年1期

In situ energy dispersive x-ray diffraction for natural marmatite (Zn0.76Fe0.23S) is performed up to 17.7 GPa and 623K. It is fitted by the Birch-Muaghan equation of state (EOS) that K0 and α0 for marmatite are 85(3)GPa and 0. 79(16)× 10-4 K-1, respectively.