The number of recorded events decreases with increasing magnitude (Table 4).
The upper bound magnitude, by contrast, fits well the seismic slip required (Earthquake rupture model 1934_H1, maximum magnitude, Table 1).
Generally, the saturation remanence of olivine was stronger than that of plagioclase by ~1 order of magnitude (Table 4).
The affinity of CFT for DAT and NET is of the same order of magnitude (Table 1).
Starting from 2014, a number of emulsion-based protocols including that by 10× Genomics increased this number by another one to two orders of magnitude (Table 1).
Using its lower bound magnitude, 172 % of afterslip would be required to fully release the seismic moment deficit since 1255 (Earthquake rupture model 1934_H1, minimum magnitude, Table 1).
Depolymerisation rate constants for the samples with iron gall inks were higher almost by two orders of magnitude (Table 2, bold data).
Over the years, the numbers of collaborators, collaboration relationships and co-artifacts vary, but have the same order of magnitude (Table 9).
The theoretically expected diffusion coefficients covered three orders of magnitude ( Table 2).
For example, published values for LC-0 error span an entire order of magnitude (Table 4).
However, the values of Δπmax were of low magnitude (Table 2), which indicated a moderate affinity of the peptide for these gangliosides compared with GalCer-HFA.
