{ "culture": "en-US", "name": "", "guid": "", "catalogPath": "", "snippet": "Continuity of Top Seal for Tuscaloosa Group, Alabama Gulf Coastal Plain", "description": "

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>

<\/P><\/DIV><\/DIV><\/DIV>", "summary": "Continuity of Top Seal for Tuscaloosa Group, Alabama Gulf Coastal Plain", "title": "Top of Selma, Continuity of Top Seal for Tuscaloosa", "tags": [ "Tuscaloosa Group", "Alabama Gulf Costal Plain" ], "type": "", "typeKeywords": [], "thumbnail": "", "url": "", "minScale": "NaN", "maxScale": "NaN", "spatialReference": "", "accessInformation": "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.", "licenseInfo": "See access and use constraints information.", "portalUrl": "" }