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Layer: tusc_006_sandbody_cont (33)

Name: tusc_006_sandbody_cont

Display Field: CONTINUITY

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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 CO2 sequestration in the area becomes a serious possibility.

Service Item Id: 72c05c4601f147b49131c6c12f6fe156

Copyright Text: Alverson, R. M., 1970, Deep well disposal study for Baldwin, Escambia and Mobile Counties, Alabama: Alabama Geological Survey, Circular 58, 49 p. * Mancini, 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. 1128–1142. * Tucker, W. E., and Kidd, R. E., 1973, Deep-well disposal in Alabama: Alabama Geological Survey, Bulletin 104, 229 p., 4 plates.

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Fields:
• objectid ( type: esriFieldTypeOID, alias: OBJECTID )
• edx_sp_csod.sde.tuscaloosa_006_sandbody_continuity.area ( type: esriFieldTypeDouble, alias: edx_sp_csod.sde.tuscaloosa_006_sandbody_continuity.area )
• perimeter ( type: esriFieldTypeDouble, alias: PERIMETER )
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• a_id ( type: esriFieldTypeDouble, alias: A_ID )
• continuity ( type: esriFieldTypeString, alias: CONTINUITY, length: 16 )
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• st_perimeter(shape) ( type: esriFieldTypeDouble, alias: st_perimeter(shape) )