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

Figure 8

Burial history model for wells B-2, D-1, and J-1. There are two main breaks in depositional rate in all three wells, the first occurred from 99.6 My to 89.3 My (during Cenomanian-Turonian), and the more important second one occurred from 15.97 My to the present day.