In the crystal structures of the minerals edoylerite, deanesmithite, and wattersite and in the structures of the compounds HgCrO₄, Hg₃O₂CrO₄ (analog of the mineral schuetteite), and Pb₂HgO₂CrO₄, there are atomic groups or fragments linked by relatively strong (covalent) bonds. The anion fragments represented by CrO₄ tetrahedra are condensed into pairs and chains, in which adjacent tetrahedra are related by symmetry centers. The cation fragments form various patterns from zigzag ribbons of [Hg₄S₄] rings to ribbons and frameworks with [Hg₆O₂] r-octahedra, [Hg₂CrO] and [Pb₂HgO] triangles, and [Hg₆Cr₂O₄] (stella quadrangula) groups. The symmetry of the fragments and their assemblies is analyzed. Analysis of the reference crystal-forming planes has revealed cation sublattices (close to the F-cubic sublattice in two cases), determining the typical features of the structures.