“…However, the clearly lowest H-affinity of Fe corroborates the exceptional stability of this structure in the low-temperature region, as well as the preference for the high-pressure structure of phase I′-FeCp 2 dominated by hydrogen bonds CH···π . The dielectric response of ferrocene crystals, , as well as the conformational features recently revealed in the new modulated structure of phase I″ of ferrocene, suggests a contribution of dipole–dipole cohesion forces, which until recently were not considered. The weaker anagostic interactions and a stronger contribution of other types of cohesion forces can contribute to the presently known distinctly higher number of crystal phases (I, I′, I″, II, and III) of ferrocene compared to other simple metallocenes, e.g., only two phases are known for osmocene, ruthenocene, and nickelocene.…”