The densest and hardest polymorph of silica found in nature so far, with a structure similar to that of alpha-PbO
2. Found first in the Shergotty meteorite, and since then in several other Martian meteorites. Stable only above pressures of 780 kilobars, so it could theoretically also form in the Earth's mantle at depths over 1,700 km, if any free silica is present. Suggested as a minor phase near the core-mantle boundary by Zhang et al. (2016), who synthesized seifertite; in the experiment it was associated with (Mg,Fe)SiO
3 post-
perovskite.