عنوان مقاله [English]
In this study, a thermal modeling was carried out in surface outcropped-formations in Kuh-e Khami and Kuh-e Mish, Iran. The formations were studied by two sets of experiments obtained from three different locations. Lithology, thickness, dip and azimuth of strata were measured. Also the eroded parts of these formations were reconstructed. A cross section of Kuh-e Khami and Kuh-e Mish were prepared from NE-SW direction and was used for the simulation software. Finally maturity model and history of Kazhdumi were established based on the results. It was included that erosion had a significant impact on maturation rate of organic materials. Initiation of erosion from burial depth resulted in lower temperatures and oil production rates.
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