The Bakken Shale covers an area of approximately 200,000 square miles in the Williston Basin. The Bakken Shale covers the northeastern portion of Montana.
Significant producers within the Bakken Shale are:
The Bakken shale is from the Devonian Mississippian age. The widespread Upper Devonian-Lower Mississippian Bakken formation consists of an upper and a lower shale member with a mixed siliciclastic carbonate middle member, that is usually referred to as a dolomitic sand (or a sandy dolomite). Both the upper and lower shales are organic-rich marine shale of relatively consistent lithology. These shales are both the petroleum source rocks (organic rich) and seal for the reservoir. The Bakken has also sourced the Three Forks Sanish formation, an underlying dolomite, in much of the Williston Basin. In 2008, the USGS estimated technically recoverable reserves from the Bakken could reach as high as 4.3 billion barrels of oil.
The Bakken Shale is located in the following Montana counties:
Additional Reading
Use of this site constitutes acceptance of our Terms & Conditions and Privacy Policy.
© COPYRIGHT 2009-2025 KED INTERESTS, LLC - ALL RIGHTS RESERVED