“…Since the 1950s, many investigations have indicated the possibility that terrestrial sediments (especially coal and bituminous shale) have a potential to generate oil or gas by thermal maturation of organic compounds when buried in a sedimentary basin (Hubbard, 1950). Organic-geochemical studies, such as Rock-Eval pyrolysis, show that humic coals have a chemical potential to generate hydrocarbons (Durand and Paratte, 1983;Espitalié et al, 1985;Mukhopadhyay et al, 1989;Littke et al, 1990;Powell et al, 1991;Boreham and Powell, 1993;Clayton, 1993;Littke and Leythaeuser, 1993;Powell and Boreham, 1994;Clayton, 1998;Kalkreuth et al, 1998).…”