Research Article

Formation Pore Pressure Variation of the Neocomian Sedimentary Succession (the Fahliyan Formation) in the Abadan Plain Basin, SW of Iran

Figure 1

The location of studied wells on the map of the Abadan Plain Basin and contiguous area. The arbitrary line between wells A-6, B-2, D-1, I-1, and J-1 corresponds to the stratigraphic correlation in Figure 6.