Structures of (Ca22)(Si1P)4 crystals were examined as a function of x ranging from 0.03 to 0.40. All of the samples were heated at the stable temperature region of the -phase and then quenched in water. The phase constitution at ambient temperature was classified into three categories according to the fraction of the -to-H transition. When the transition was completed as in the crystals with x0.100, the and L phases were obtained, the relative amounts of which were determined by the start and finish temperatures of the L-to-martensitic transformation. With 0.125x0.150, the -totransition was incomplete. Dur ing further cooling, the product -phase was inverted to the L-phase, and the residual -phase was invert ed to the incommensurate phase successively. Because the start temperature of the L-to-transformation was lower than ambient temperature, the L-phase was stabilized. With x0.175, all of the crystals were free from the -totransition. The crystals with 0.175x0.225 were made up exclusively of the incom mensurate phase. A good correlation existed between the modulation wavelength (=N) and the P/(Si+P) ratio (=x) as N=4.134-1.56x(0.175x0.250). With 0.275x0.300, the crystals were isostructural with -Ca2Si4. The hexagonal phase with 0.350x0.400, probably a transition product from the -phase, showed two-dimensional modulations along the -axis with N=2 and along the c-axis with N=3.