Pressure can induce significant changes in atomic and electronic structures and can in some cases even induce compound formation between elements that do not bond under ambient conditions. Here, we have extensively explored the Li−Fe system at high pressure using the effective CALYPSO algorithm in combination with first-principles calculations. Strikingly, our results show that the stoichiometries of LiFe, Li 3 Fe and Li 3 Fe 2 have stability regimes on the phase diagram. It is found that both LiFe and Li 3 Fe 2 adopted fully developed three-dimensional framework. With Li content increasing, Li bonding pattern evolves from occupying diamond sublattice to