Fayetteville Shale Sandstone Stratigraphic range: Carboniferous: Mississippian (Serpukhovian) |
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Outcrop of the lower Fayetteville shale in northern Arkansas.
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Type | Geological formation |
Sub-units | Weddington Sandstone |
Underlies | Pitkin Limestone,Hale Sandstone (Morrow Group) |
Overlies | Rudell Shale, Batesville Sandstone Moorefield Shale |
Area | Arkansas and Oklahoma |
Thickness | 50 to 500 feet (15 to 152 m) |
Lithology | |
Primary | Shale |
Other | Sandstone, Limesone |
Location | |
Region | Arkansas |
Country | United States |
Extent | 50 miles (80 km) |
Type section | |
Named for | Fayetteville, Arkansas |
The Fayetteville formation runs widespread across Arkansas |
The Fayetteville Shale is a geologic formation of Mississippian age (354–323 million years ago) composed of tight shale within the Arkoma basin of Arkansas and Oklahoma. It is named for the city of Fayetteville, Arkansas, and requires hydraulic fracturing to release the natural gas contained within.
The formation holds natural gas in a fine-grained rock matrix which requires hydraulic fracturing to release the gas. This process became cost-effective in some shales such as the Fayetteville after years of experimentation in the Barnett Shale in North Texas, especially when combined with horizontal drilling.
The US Energy Information Administration estimated that the 5,853 square miles (15,160 km2) shale play held 13,240 billion cubic ft (375 billion cubic meters) of unproved, technically recoverable gas. The average well was estimated to produce 1.3 billion cubic feet of gas.