Atoka Formation at Brooke Blain blog

Atoka Formation. This short course is an overview of the atoka formation in the arkoma basin, including tectonic evolution, sedimentology and. Atoka, hartshorne, mcalester, and savanna formations and a part of boggy shale are directly traceable into winslow formation as heretofore mapped in muskogee. One such formation, termed atoka shale, could prove to be a viable unconventional play within the permian basin. The atoka formation crops out along the backbone anticline, which is the expression of a thrust fault that ramps to the surface just north. Atokan strata of the arkoma basin record the transition from sedimentation on a passive, rifted margin to sedimentation in a foreland basin. The atoka formation along the southwestern margin of the arkoma basin in coal and pontotoc counties, oklahoma, is predominantly a.

Figure 1 from Diagenesis and Reservoir Characterization of the
from www.semanticscholar.org

Atokan strata of the arkoma basin record the transition from sedimentation on a passive, rifted margin to sedimentation in a foreland basin. The atoka formation along the southwestern margin of the arkoma basin in coal and pontotoc counties, oklahoma, is predominantly a. This short course is an overview of the atoka formation in the arkoma basin, including tectonic evolution, sedimentology and. One such formation, termed atoka shale, could prove to be a viable unconventional play within the permian basin. The atoka formation crops out along the backbone anticline, which is the expression of a thrust fault that ramps to the surface just north. Atoka, hartshorne, mcalester, and savanna formations and a part of boggy shale are directly traceable into winslow formation as heretofore mapped in muskogee.

Figure 1 from Diagenesis and Reservoir Characterization of the

Atoka Formation The atoka formation crops out along the backbone anticline, which is the expression of a thrust fault that ramps to the surface just north. The atoka formation along the southwestern margin of the arkoma basin in coal and pontotoc counties, oklahoma, is predominantly a. One such formation, termed atoka shale, could prove to be a viable unconventional play within the permian basin. Atokan strata of the arkoma basin record the transition from sedimentation on a passive, rifted margin to sedimentation in a foreland basin. The atoka formation crops out along the backbone anticline, which is the expression of a thrust fault that ramps to the surface just north. Atoka, hartshorne, mcalester, and savanna formations and a part of boggy shale are directly traceable into winslow formation as heretofore mapped in muskogee. This short course is an overview of the atoka formation in the arkoma basin, including tectonic evolution, sedimentology and.

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