Transmission electron microscopy (TEM) investigation of natural kalsilite, (K,77Doo9Na,4b(Si209Alu9Feo12bOg, from San Venanzo, Italy, shows that it contains a pervasive domain structure related to a superstructure. The probable space group for the superstructure is P21. The relationship between the unit -cell parameters of the P6, subcell and those of the P21 supercell is a,upec ~ b,upec ~ v'3a,ub; c,upec = Cmb,and the a,upec axis is rotated 30° about the C axis with respect to the a,ubaxis. Nonperiodic distribution of elongated twin domains causes streaking of superstructure reflections normal to the c* axis. The average structure of this kalsilite sample has P6, symmetry. On the basis of previous structure refinements, this average structure has three 01 positions slightly displaced from the threefold axis, and each 01 position has a site occupancy of V3.High-temperature annealing studies indicated that there is a displacive phase transition from the P21 superstructure to the P63 substructure. The twin domains are related by threefold twin operations. The phase-transition temperature for kalsilite may range from 500 to 600°C and is dependent on the crystal composition (e.g., the proportions of Na, Ca, and vacancies). Kalsilite crystals prepared from nepheline by Na-K exchange are structurally complex. Domain structures in Na-bearing kalsilite crystals with more than 2.5 mol% NaSiAI04 are similar to those in the natural kalsilite sample but exhibit additional twin boundaries parallel to the c axis. Na-poor and Na-free kalsilite crystals are composed of (0001) domains with P63 and P31c symmetries, respectively, and merohedral twins between the neighboring P63 or P31c domains. The merohedral twins in the synthetic crystals formed during transformation of the nepheline structure to the kalsilite structure. The intergrown domains with P31c symmetry formed during the phase transition on cooling of the Na-poor kalsilite. There is no simple symmetry hierarchy among the known structures in the proposed phase diagram.