A large number of coal samples from the Palaeogene coal deposits of Northea
st India were subjected to detailed chemical (proximate, ultimate and Rock-
Eval pyrolysis) and petrographic (maceral, microlithotype and vitrinite ref
lectance) analyses to examine their source rock characteristics and to expl
ore their participation in hydrocarbon generation. The results show that th
ese coals are sub-bituminous 'C' to high Volatile bituminous 'C' in rank an
d have requisite petrographic characteristics to act as a potential source
for the generation of significant amount of normal hydrocarbons. The values
of vitrinite reflectance, particularly of the coals of Meghalaya and Assam
, suggest a maturation close to the 'top oil window' (birth line). This ind
icates the possibility of expulsion of oil and condensates in the basin. Ho
wever, this contention needs to be supported by organic geochemical data, m
aturation modelling and time of hydrocarbon generation.