North-Central Section - 42nd Annual Meeting (24–25 April 2008)

Paper No. 4
Presentation Time: 1:00 PM-5:00 PM


REPETSKI, John E.1, RYDER, Robert T.2, EAST, Joseph A.2, NORBY, Rodney D.3, REXROAD, Carl B.4, ROWAN, Elisabeth L.5, SHAW, Thomas H.6, BERGSTRÖM, Stig M.7, TRIPPI, Michael H.2 and WEARY, David J.8, (1)U.S. Geological Survey, 926A National Center, Reston, VA 20192, (2)Eastern Energy Resources, United States Geol Survey, 12201 Sunrise Valley Drive, MS 956, Reston, VA 20192, (3)University of Illinois, 615 E. Peabody Dr, Champaign, IL 61820-6964, (4)Indiana Geological Survey, 611 N. Walnut Grove, Bloomington, IN 47405, (5)United States Geol Survey, 12201 Sunrise Valley Drive, MS 956, Reston, VA 20192, (6)LK Energy, Houston, TX 77098, (7)Ohio State Univ - Columbus, 155 S Oval Mall, Columbus, OH 43210-1308, (8)U.S. Geological Survey, MS 926A, Reston, VA 20192, JREPETSKI@USGS.GOV

New thermal maturity maps have been constructed for Paleozoic rocks of the central part of the Appalachian basin (New York to central Kentucky) and for the Michigan and Illinois basins, using conodont color alteration index (CAI). New CAI values were derived from drill cuttings from several hundred wells throughout the region and from several dozen outcrops along the edges of the Illinois basin. Ordovician, Devonian, and Carboniferous carbonate intervals were chosen for CAI because they are within or near probable hydrocarbon source beds and oil and gas reservoir zones in these basins. These maps show thermal patterns that are aligned with, and probably causally related to, structural and geophysical features, such as the Rome trough and selected basement-fault systems. Also, the CAI isograds show differing levels of compatibility with known hydrocarbon accumulations, suggesting that accumulations originating from local migration may be distinguished from ones originating from longer-distance migration.

The CAI isograds indicate higher paleotemperatures than can be explained by present burial depths over the region, as do other paleothermal investigations, e.g., vitrinite reflectance (%Ro). Possible sources of additional heating vary from region to region but include burial and insulation of lower Paleozoic rocks by Devonian black shale and Pennsylvanian coal, migration of hot geothermal fluids, local emplacement of mantle-derived rocks along reactivated extensional structures during post-Paleozoic time, and crustal thinning. These data and maps will aid in resource assessments and the development of burial/thermal history, hydrocarbon generation, and fluid flow models for these basins.