“…Inorganic overlayers possess a rigidity that inhibits deformation required for achieving commensurism (when a commensurate configuration with the native overlayer is not available), leaving only azimuthal rotation as a route to achieving a minimum interfacial energy. Examples of coincidence in inorganic overlayers include transition metal dichalcogenides (TX 2 ) on mica, [44] metal dihalides on TX 2 , [45] a-alumina nanocrystals on mica, [46] CdSe on Au, [47] Bi 2 O 3 on Au, [48] AgBr on Au, [49] Ag on highly oriented pyrolytic graphite (HOPG), [50] PtCl 6 on Au, [51] simple face-centered cubic (fcc) and body-centered cubic (bcc) systems, [52,53] and others. [54,55] The concept of coincidence actually has its roots in the description of grain boundaries.…”