A parallelotope is a polytope that admits a facet-to-facet tiling of space by translation copies of along a lattice. The Voronoi cell of a lattice is an example of a parallelotope. A parallelotope can be uniquely decomposed as the Minkowski sum of a zone closed parallelotope and a zonotope , where is the set of vectors used to generate the zonotope. In this paper we consider the related question: When is the Minkowski sum of a general parallelotope and a zonotope a parallelotope? Two necessary conditions are that the vectors of have to be free and form a unimodular set. Given a unimodular set of free vectors, we give several methods for checking if is a parallelotope. Using this we classify such zonotopes for some highly symmetric lattices.
In the case of the root lattice , it is possible to give a more geometric description of the admissible sets of vectors . We found that the set of admissible vectors, called free vectors, is described by the well-known configuration of 27 lines in a cubic surface. Based on a detailed study of the geometry of , we give a simple characterization of the configurations of vectors such that is a parallelotope. The enumeration yields 10 maximal families of vectors, which are presented by their description as regular matroids.