[P-PS06] Planetary interiors revealed by observations, experiments, and simulations

[PPS06-P03] Partitioning of P, Cr, Mn and Ti between metal and silicates melts in reduced Mercurian magmas

*Dilan Harsha Fernando Diyalanthonige¹, Takashi Yoshino¹, Tiffany L. Barry² (1. Institute for Planetary Materials, Okayama University, 2. Space Park Leicester, University of Leicester, Leicester)

Keywords:Mercury, metal–silicate partitioning, Fe-Si , enstatite chondrite