Given its high symmetry, this is likely the quasi-nucleus that loses its orbiting electrons, acquire a layer of g+ particles that bonds by sharing g− particles and forms into a crystal lattice.
Does it stop here? The likely release of T− particle when the crystal collapse suggests another T+ layer is attracted to the quasi-nucleus and that the crystal are held together by T−--T+ bonds instead of g−--g+ bonds proposed previously. T−--T+ will be seen as magnetic in nature.
Bonding with T− particles complement the charge on the quasi-nucleus and prevents the next p+ layer.
Maybe, but Good Morning!
