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274   Applied Petroleum Geomechanics
































          Figure 7.29 Pore pressure profile in ND and MT, USA based on analyzing 92 bot-
          tomhole pressure and DFIT data points, a number of hydrostatic points at eastern
          margin, six Sanish-Parshall points in the Middle Bakken and additional data of the
          Three Forks (Theloy, 2014).

          generation in both Upper and Lower Bakken shales correlates to formation
          overpressures.

          7.5.8.3 Haynesville and Bossier shale plays
          The Bossier and Haynesville shales are tight shale gas reservoirs with very
          low matrix permeability (0.00007e0.0007 mD). The lithology comprises
          the Tertiary-, Cretaceous-, and Jurassic-aged stratigraphic units character-
          ized primarily by claystones (shales) and sandstones. There are also lime-
          stone formations, such as the Knowles limestone in the Cotton Valley
          Group and the Smackover limestone at bottom of the Haynesville shale
          (Fig. 7.30). Regional correlation sections across northern Louisiana reveal a
          prominent mid-Cretaceous unconformity, suggesting a later uplift event
          affecting the area. It appears that the present-day Sabine High represents a
          Tertiary uplift event. The maximum missing section due to the Tertiary
          uplift is estimated in orders of several thousand feet. Timing of the uplift
          and erosion appears to be the Oligocene Epoch (Zhang and Wieseneck,
          2011).
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