Publications in Andrews

Title Publication Year Abstract Author Series Publisher
Bouguer gravity Atlas of Texas, Hobbs sheet Bouguer gravity Atlas of Texas, Hobbs sheet 1986

This folded transparent map is at the same scale as its corresponding Geologic Atlas of Texas (GAT) sheet and can be superimposed on it to compare gravity information with surface geology.

Keller, G.R., Aiken, C.L.V. Bouguer Gravity Atlas of Texas Bureau of Economic Geology
Geologic Atlas of Texas, Hobbs sheet Geologic Atlas of Texas, Hobbs sheet 1976

Geologic map that depicts the surface geology of Gaines and Andrews Counties and parts of Yoakum, Terry, Dawson, Martin, Winkler, Ector, and Midland Counties, Texas. The 5-page booklet indicates geologic formations, abbreviations, and ages.

Barnes, V.E., Eifler, G.K., Reeves, C.C., Kottlowski, F.E., Norman, D.M., Sherrod, C.H., Hansen, J.J. Geologic Atlas of Texas Bureau of Economic Geology
Electrical Imaging Catalog: Microresistivity Images and Core Photos from Fractured, Karsted, and Brecciated Carbonates Electrical Imaging Catalog: Microresistivity Images and Core Photos from Fractured, Karsted, and Brecciated Carbonates 1997

Electrical images in boreholes are becoming increasingly important in interpreting the rock record.

Hammes, Ursula Geological Circular Bureau of Economic Geology
Basin morphological controls on submarine-fan depositional trends:  Spraberry Sandstone, Permian Basin, Texas Basin morphological controls on submarine-fan depositional trends: Spraberry Sandstone, Permian Basin, Texas 1997

The Leonardian Spraberry Formation is a major oil-producing formation of the Permian Basin, accounting for more than 700 million barrels of oil produced from heterogeneous submarine-fan reservoirs.

Tyler, Noel, Gholston, J.C., Guevara, E.H. Geological Circular Bureau of Economic Geology
Subsurface Woodford black shale, West Texas and southeast New Mexico Subsurface Woodford black shale, West Texas and southeast New Mexico 1950

The geographic distribution, lithology, thickness, and paleontology of the subsurface Woodford in the Permian basin are described and illustrated.

Ellison Jr., S.P. Report of Investigations Bureau of Economic Geology
Depositional framework of the Lower Dockum Group (Triassic), Texas panhandle Depositional framework of the Lower Dockum Group (Triassic), Texas panhandle 1979

The Upper Triassic Dockum Group of Texas and New Mexico is composed of 200 to 2,000 feet of complexly interrelated terrigenous clastic facies ranging from mudstone to conglomerate.

McGowen, J.H., Granata, G.E., Seni, S.J. Report of Investigations Bureau of Economic Geology
Genesis and emplacement of oil in the San Andreas Formation, northern shelf of the Midland basin, Texas Genesis and emplacement of oil in the San Andreas Formation, northern shelf of the Midland basin, Texas 1982

San Andres oil constitutes more than 80 percent of the total production from the Northern Shelf of the Midland Basin, Texas.

Ramondetta, P.J. Report of Investigations Bureau of Economic Geology
Facies and stratigraphy of the San Andreas Formation, northern and northwestern shelves of the Midland basin, Texas and New Mexico Facies and stratigraphy of the San Andreas Formation, northern and northwestern shelves of the Midland basin, Texas and New Mexico 1982

The San Andres Formation on the Northern and Northwestern Shelves of the Midland Basin is a progradational stratigraphic unit consisting predominantly of carbonate facies. Lithofacies include dolomite, laminated anhydrite and dolomite, massive bedded anhydrite, limestone, salt, and red beds.

Ramondetta, P.J., Guetzow, D.D., Dauzat, Rick, Merritt, R.M., Garza, John, Holman, Lee, Roques, Dominick Report of Investigations Bureau of Economic Geology
Hydrogeology and hydrochemistry of the Ogallala aquifer, southern High Plains, Texas panhandle and eastern New Mexico Hydrogeology and hydrochemistry of the Ogallala aquifer, southern High Plains, Texas panhandle and eastern New Mexico 1988

The Ogallala aquifer, which underlies the Southern High Plains, consists of the saturated sediments of the Neogene Ogallala Formation. The aquifer is the main source of water for the High Plains of Texas and New Mexico and is being severely depleted by extensive pumpage for irrigation.

Nativ, Ronit Report of Investigations Bureau of Economic Geology
Effects of facies and diagenesis on reservoir heterogeneity:  Emma San Andres field, West Texas Effects of facies and diagenesis on reservoir heterogeneity: Emma San Andres field, West Texas 1988

Pervasively dolomitized, anhydritic carbonates of the upper San Andres Formation in the Emma field of West Texas constitute an upward-shallowing sequence of lithofacies representing four major depositional environments.

Ruppel, S.C., Cander, H.S. Report of Investigations Bureau of Economic Geology