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Title: Deep Tuscaloosa gas trend of S. Louisiana

Journal Article · · Oil Gas J.; (United States)
OSTI ID:6836103

Since the first gas discovery in 1975, proven plus potential reserves in the deep Tuscaloosa trend of south Louisiana have reached about 5 trillion CF. The trend covers a band approximately 30 miles wide and 200 miles in length from the Texas state line on the west and extending past Lake Pontchartrain on the east. The objective Tuscaloosa sands are of Upper Cretaceous age, overlain by Eagleford shale and the Austin-Taylor-Navarro chalk section. Underlying the Tuscaloosa sequence are lower Cretaceous carbonates and shales of Lower Cenomanian-Albian age. Seismic resolution of the deep structures below the chalk horizon is the key to successful Tuscaloosa exploration. In some areas along the trend, a major exploration problem is the inability to critically evaluate gas-show zones with electric logs because of the unknown and varying salinities of the formation water in the Tuscaloosa sands. Furthermore, the variable formation pressures encountered while drilling to and through the Tuscaloosa can often lead to lost circulation or blowout problems, pipe sticking, and hole collapse. These difficulties, along with the additional production problems inherent in ultradeep formations, are a major cause of excessively high well costs, which can run up to $15 million for a development well.

OSTI ID:
6836103
Journal Information:
Oil Gas J.; (United States), Vol. 78
Country of Publication:
United States
Language:
English