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Level of thermal maturation of organic matter from the Upper Na 1 sub-member shows early mature stage of main oil generation zone, and maturity of organic matter in the Eocene Na 2 member mudstones reached the middle stage of oil generation zone.
Biomarker and non-biomarker parameters have been used to evaluate the origin, paleodepositional conditions, lithology and thermal maturation of organic matter.
Despite the maturation of organic chemistry and the efforts of medicinal and combinatorial chemistry, natural products play a preeminent role in drug discovery.
Boundary conditions define the basic energetic conditions for temperature and burial history of the source rock and, consequently, for the maturation of organic matter through time (Ben-Awuah et al. 2013).
The results indicate that the thermal maturation of organic matter in the shale can be divided into four stages: oil generation (<0.6 1.0% EasyRo), condensate generation (1.0 1.5% EasyRo), wet gas generation (1.5 2.2% EasyRo), and dry gas generation (2.2 4.5% EasyRo).
According to van Krevelen (1993) particular organic matters present in coal beds are classified based on H/C and O/C atomic ratio (Table 2) The H/C and O/C atomic ratios decrease with increased thermal maturation of organic matter, which indicates the types of kerogen and maceral types present in the coal.
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In order to determine the total history of basin burial, we executed one-dimensional modeling of maturation levels of organic matter contained in the Cretaceous Yezo Group.
Hence, we examined maturation profiles of organic matter derived from sedimentary rocks and attempted to reconstruct the burial history based on kinetic models.
Twenty eight mudstone (28) samples were tested by using standard organic geochemistry methods (Rock-Eval VI-TOC, bitumen extraction and fractionation), as well as GC-MS analysis of the hydrocarbons fraction to define the origin, type and maturation level of organic material, and the environment conditions during deposition.
Color, in particular, is a highly variable characteristic as it is mainly controlled by the thermal maturation of the organic matter.
Optical reflectance of the vitrinite increases with its thermal maturation due to irreversible decompression of organic material.
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