{ "culture": "en-US", "name": "", "guid": "", "catalogPath": "", "snippet": "Continuity for Tuscaloosa Group, Alabama Gulf Coastal Plain", "description": "
Several authors have indicated that the sands in the lower Tuscaloosa Group are regionally continuous (Tucker and Kidd, 1973; Mancini and others, 1987). Alverson (1970) referred to lower Tuscaloosa Groups as a regionally continuous sand reservoir. The cross sections of Mancini and others (1987) provide direct evidence of the degree of sand-body continuity in the Lower Tuscaloosa Group. A large number of geophysical logs that penetrate the Tuscaloosa Group are available. From these logs, it would possible to determine sand-body continuity for the region, if CO<\/SPAN><\/SPAN>2<\/SPAN><\/SPAN> sequestration in the area becomes a serious possibility.<\/SPAN><\/SPAN><\/P> <\/P><\/DIV><\/DIV>",
"summary": "Continuity for Tuscaloosa Group, Alabama Gulf Coastal Plain",
"title": "Tuscaloosa Continuity",
"tags": [
"Tuscaloosa Group",
"Alabama Gulf Costal Plain"
],
"type": "",
"typeKeywords": [],
"thumbnail": "",
"url": "",
"minScale": 0,
"maxScale": 0,
"spatialReference": "",
"accessInformation": "Alverson, R. M., 1970, Deep well disposal study for Baldwin, Escambia and Mobile Counties, Alabama: Alabama Geological Survey, Circular 58, 49 p.\n*\nMancini, E. A., Mink, R. M., Payton, J. W., and Bearden, B. L., 1987, Environments of deposition and petroleum geology of the Tuscaloosa Group (Upper Cretaceous), South Carlton and Pollard Fields, southwestern Alabama: American Association of Petroleum Geologists Bulletin, v. 71, p. 1128\u20131142.\n*\nTucker, W. E., and Kidd, R. E., 1973, Deep-well disposal in Alabama: Alabama Geological Survey, Bulletin 104, 229 p., 4 plates.",
"licenseInfo": "See access and use constraints information."
}