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Bureau of Economic Geology
10100 Burnet Rd. Bldg. 130
Austin
TX
78729
US
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20230328
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Austin
Texas
78758
US
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Arbuckle Formation Top Seal Thickness 2
Isopach (thickness) maps of confining zone
Publication Date: 2012
Geographic Extent: Oklahoma, Kansas, Texas, Arkansas, Louisiana
Top-seal thickness. We combined the isopach maps of Hester and Schmoker (1993) and Amsden (1975) to derive a thickness map for the Woodford Shale. The unit that we identify as the best potential seal for the Arbuckle and gridded it 51 (s7arbuckle). Johnson (1991b) mentioned that by the early 1990’s all ten of the hazardous waste-disposal wells then operating in Oklahoma were using the Arbuckle or Arbuckle-Simpson as the recipient reservoir. Significantly, either the Woodford Shale (in the Tulsa area) or truncating Pennsylvanian-age shales (in the Oklahoma City area) acted as the confining units. This fact suggests that, at least in the cases where hazardous waste is involved, the intervening Silurian- and Devonian-age rocks may not be sufficiently low in permeability to act as seals for either the Arbuckle or the Simpson.
Havorka, S., Romero, M., Warne, A., Ambrose, W., Tremblay, T., Trevino, R., and Sasson, D. "Sequestration of Greenhouse Gassesin Brine Formations: CO2 Brine Database. Bureau of Economic Geology Gulf Coast Carbon Center. 2012. https://www.beg.utexas.edu/gccc/research/brine-main
Arbuckle
Oklahoma
United States
Oklahoma
Kansas
Texas
Arkansas
Louisiana
Arbuckle Formation Top Seal Isopach
Cap Rock Isopach
Top Seal Thickness
Cap Rock Thickness
Arbuckle Formation
Top Seal Isopach
Arbuckle
Formation
Top Seal
Cap Rock
Isopach
Thickness
Reservoir
Polyline
Access constraints: None
Use constraints: research purposes only
Public access
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