The behavior of the paramagnetic characteristics of low-metamorphized
coal and the same coal labeled with copper prophyrin during pyrolysis
is interpreted in terms of the microdomain model of the structure of c
oal. In this model, vitrainized maceral is regarded as a primarily ani
sotropic medium and as a natural high-molecular crystal. Anisotropic u
nits or microdomains 6.0 nm in length perform the function of recurren
t structural nuclei in different coals. Each microdomain has a complex
structure and contains about 15 close-packed crystallites, sequential
ly passing to the paramagnetic state during coal pyrolysis.