Abstract
The Upper Jurassic Cotton Valley Sandstone is a thick siliciclastic unit in the East Texas Basin. Sandstones and shales of this unit were deposited in shallow marine and fluvial-deltaic environments and exhibit progradational successions of facies. Along the eastern flank of the basin, natural gas is produced from Cotton Valley reservoirs characterized by low porosity and permeability, which have been stimulated by massive hydraulic fracturing.
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