Changes

::<math>= 0.34 \text{or } 34% \text{ reactive organic carbon}</math>

::<math>= 0.34 \text{or } 34% \text{ reactive organic carbon}</math>

An important example of variable organofacies is provided by analog data for the Bossier and Haynesville shales in the area between the east Texas and north Louisiana salt basins. As only gas window maturity Bossier and Haynesville shale data are available, analog data are used, that is, immature Tithonian and Kimmeridgian source rocks from the deep-water Gulf of Mexico (Table 3).

An important example of variable organofacies is provided by analog data for the Bossier and Haynesville shales in the area between the east Texas and north Louisiana salt basins. As only gas window maturity Bossier and Haynesville shale data are available, analog data are used, that is, immature Tithonian and Kimmeridgian source rocks from the deep-water [[Gulf of Mexico]] (Table 3).

{| class=wikitable

{| class=wikitable