BITUMEN FILLED FRACTURES IN THE BAKKEN FORMATION AND IMPLICATIONS FOR GAS SHALE SYSTEMS
The Bakken shale contains sub-horizontal to vertical bitumen filled fractures and pores interpreted to have formed during petroleum generation. The fractures and pores are visible in both the upper and lower shale, and provide insight into migration of petroleum out of Bakken shale, suggesting fracture formation may have been an essential step in the migration process. The presence of large pores within the shale facies demonstrates development of significant pore systems is possible within the shale facies. Observations from the Bakken oil system may also provide insight into the development of gas shale systems. The cracking of retained petroleum to gas in shales is a significant source of gas for gas shales, and appears to be the primary reason marine shales that contain Type II, oil-prone kerogen can become gas charged systems at higher levels of thermal maturity. Assuming that bitumen filled fracture systems that developed in the upper and lower Bakken during petroleum generation and migration are the rule rather than the exception, this observation may help explain why marine, oil prone source rocks have the potential to deliver gas as gas shale systems.