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U.S. Department of Energy
Office of Scientific and Technical Information

Oil and gas data from Paleozoic rocks in the Appalachian basin: maps for assessing hydrocarbon potential and thermal maturity

Book ·
OSTI ID:6296338

Conodont color alteration index (CAI) isograd maps and overburden isopach maps are provided for 3 stratigraphic intervals in the Appalachian basin-Ordovician, Silurian through Middle Devonian, and Upper Devonian through Mississippian. Isograds follow isopach trends throughout the basin; both increase eastward. The CAI 2 isograd lies near the eastern limit (cutoff) of oil production for each stratigraphic interval. Gas production shows less relation to isograds because gas generation occurs over a very broad thermal range and its production depends mostly on primary and (or) secondary porosity and permeability. However, the CAI 4 isograd approximates the eastern limit of gas production over large areas of the basin because the temperature necessary to produce this high level of organic diagenesis concurrently produces mineral metamorphism that reduces porosity and permeability.

OSTI ID:
6296338
Country of Publication:
United States
Language:
English