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20220606
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FGDC
Bureau of Economic Geology
10100 Burnet Rd. Bldg. 130
Austin
TX
78729
US
8-5
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10100 Burnet Rd. Bldg 139
Austin
Texas
78758
US
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Top of Selma, Continuity of Top Seal for Tuscaloosa
<DIV STYLE="text-align:Left;"><P STYLE="font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>The Selma Chalk is thick and generally impermeable. However, Pashin and others (1998) demonstrated that fault-induced fracturing can greatly enhance fracturing in the Selma interval. Therefore, we used a map showing the configuration of the top of the Selma (Moffett and others, 1984a), which shows the location of major faults, to characterize the continuity of the top seal.</SPAN></SPAN></P><DIV><DIV><P><SPAN /></P></DIV></DIV></DIV>
Continuity of Top Seal for Tuscaloosa Group, Alabama Gulf Coastal Plain
Pashin, J. C., Raymond, D. E., Rindsberg, A. K., Alabi, G. G., Carroll, R. E., Groshong, R. H., and Jin, G., 1998, Area balance and strain in an extensional fault system: strategies for improved oil recovery in fractured chalk, Gilbertown Field, southwestern Alabama: U.S. Department of Energy Report DOE/PC/91008-20 (DE98000499), National Petroleum Technology Office, 221 p.
Alabama Gulf Costal Plain
Tuscaloosa Group
Tuscaloosa Group
Alabama Gulf Costal Plain
Access constraints: Restriction Code: other restrictions; Other Constraints: Access constraints: None
See access and use constraints information.
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