Seatonville Syncline (Discarded)

Location

Bureau and southernmost Lee Counties

References

Willman and Payne 1942

Description

A north-trending depression, which could be considered a lobe of the Granville Basin, was defined on the basis of very sparse well data on Ordovician horizons. The Seatonville feature has not been confirmed by newer structural mapping; therefore, using the name Seatonville Syncline should be discontinued.