Geothermal Gradient

The present work attempts to address the different positions taken by updating geophysical modeling evidence concerning heat flow in the Williston Basin in which paleogeothermal conditions are variable over geologic time.

After conducting the investigation, present research demonstrates that elevated heat flow may have existed in the Williston Basin in the geologic past but did not necessarily have to occur during or after the time period suggested.

The present work attempts to address the different positions taken by updating geophysical modeling evidence concerning heat flow in the Williston Basin in which paleogeothermal conditions are variable over geologic time.