The Pabdeh and Kazhdumi formations have fair-very good generation potential.
A homogenous kerogen is mainly Type II.
The Pabdeh source rock was in early mature stage since Early Pliocene.
The Kazhdumi source rock reached the main stage of oil generation at Late Miocene.
Based on modeling, the heat flow values are in the range of 37–41 mW/m2.