A plane plane crystallographic group is a discrete subgroup of the Euclidean isometry group with compact quotient. Its translations form a normal rank-two Euclidean lattice ; this is the standard translation-lattice structure of a plane crystallographic group. Its point group is the finite group of linear parts, equivalently the quotient by those translations. Conjugating a translation by an isometry sends its translation vector to its image under the linear part, so every point-group element preserves .
Choose a Euclidean lattice basis. A rotational linear part is then represented by an integer matrix , since it sends the basis to Euclidean lattice vectors. In an orthonormal basis the same map has eigenvalues , and its trace is independent of basis. ThusThese possibilities give rotation angles, modulo a full turn, , , , , and , respectively. Consequently the crystallographic restriction theorem isThe restriction comes from integrality of the Euclidean lattice action, not simply from finiteness of the point group.
Articles by others on the same topic
There are currently no matching articles.