Rock-Eval pyrolysis and Py-GC experiments on naturally and artificially mat
ured coal samples were carried out. The results suggest that both depolymer
ization and defunctionalization exist during the maturation and evolution o
f coal. The patterns of hydrocarbon regeneration are diverse at different s
tages of the maturation and evolution. When the vitrinite reflectance (R-0)
is 0.7%-0.9%, bitumen is the richest in coal while activation energy is th
e minimum, and the temperature of peak yield is lower than that of primary
hydrocarbon generation. However, if reflectance is greater than 0.9%, defun
ctionalization predominates and the temperature of peak regeneration is sho
wn in lagging compared with the primary hydrocarbon generation. When reflec
tance is out of the "oil window", the peak temperature of hydrocarbon regen
eration and that of the primary hydrocarbon generation seems to be continuo
us.