Abstract
The crystal structure of neighborite (NaMgF3) is determined at high pressure using monochromatic synchrotron X-ray powder diffraction data with Rietveld structural refinement methods. The previously assumed regularity of the MgF6 octahedra at high pressure in the perovskite structure is demonstrated to be valid. The pressure-induced dimensional changes are expressed empirically as a combination of compression of the Mg-F bond length and tilting of the MgF6 octahedral framework. We demonstrate that the dominant compression mechanism involves shortening of the octahedral Mg-F bond, which contributes about 80% to the overall compression, with the remaining 20% due to an increase in octahedral tilting. Linear compressibilities are consistent with single-crystal elasticity data, with the significant anisotropy observed being directly related to the tilting freedom of the octahedra along each axis of the unit cell.