“…1b–f ) including: the radius of gyration, R g 18 , to capture condensation from fluid to crystal states, average local hexagonal order, 〈 C 6 〉 25 , to capture the onset of crystallization, and global hexagonal order, ψ 6 26 , to capture the degree of polycrystallinity. R g and 〈 C 6 〉 are normalized by their N particle single crystal values (see Supplementary Methods ), so that 〈 C 6 〉 goes from 0–1 for fluids to complete locally ordered states, and R g decreases from arbitrarily high numbers to 1 for complete condensation 19 . ψ 6 is 0 for fluids and 1 for single-domain crystals like 〈 C 6 〉, but in contrast, depends strongly on relative domain size and misorientation ( e.g.…”