UNCONVENTIONAL RESOURCE POTENTIAL OF ORGANIC-RICH DEVONIAN SHALE FORMATIONS, EASTERN OHIO, USA
Geophysical well log interpretation, source rock analysis, and thermal maturity data characterize the nature of these units. Two organic-rich shales of significant thickness occur in the area of interest: the Huron Member of the Ohio Shale and the Rhinestreet Member of the West Falls Formation. Gross isopach maps suggest relatively uniform deposition across the basin throughout the Rhinestreet Member interval and a shift in depocenter from north to south during deposition of the Huron Member. Net reservoir maps suggest organic constituents were deposited and preserved in the deepest part of the basin throughout deposition of the Rhinestreet Member. However, net reservoir maps of the Huron Member suggest that organic constituents were either not deposited or not preserved in the deepest parts of the basin. The relationship between net and gross isopach maps of the Huron Member suggests organic matter was deposited and preserved on a distal ‘shelf’ beyond the prograding Catskill Delta Complex. Coupled with source rock analyses and thermal maturity maps, these data indicate significant hydrocarbon and CO2-sequestration potential in the Rhinestreet and Huron Members of eastern Ohio.