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Publications in Hutchinson

Title Publication Year Abstract Author Series Publisher
Playas and recharge of the Ogallala aquifer on the southern High Plains of Texas -- an examination using numerical techniques Playas and recharge of the Ogallala aquifer on the southern High Plains of Texas -- an examination using numerical techniques 1997

This study used a numerical model to examine the playa-focused recharge theory by comparing it with the spatially uniform approach and with a zonal approach.

Mullican, W.F., Johns, N.D., Fryar, A.E. Report of Investigations Bureau of Economic Geology
Depositional, structural, and sequence framework of the gas-bearing Cleveland Formation (Upper Pennsylvanian), western Anadarko basin, Texas panhandle Depositional, structural, and sequence framework of the gas-bearing Cleveland Formation (Upper Pennsylvanian), western Anadarko basin, Texas panhandle 1994

ow-permeability ("tight") reservoir sandstones of the lower Missourian Cleveland formation produced more than 435 billion cubic feet (Bcf) of natural gas through December 1990, mostly from Ochiltree and Lipscomb Counties in the northeastern Texas Panhandle.

Hentz, T.F. Report of Investigations Bureau of Economic Geology
Geologic Significance of Remotely Sensed Physiographic Features of the Texas Panhandle and Adjacent Regions Geologic Significance of Remotely Sensed Physiographic Features of the Texas Panhandle and Adjacent Regions 1990

Remotely sensed features such as linear drainages, escarpments, ridges, and aligned playas have been identified on Landsat imagery (scale 1:250,000) of the Texas Panhandle and adjacent regions to allow comparison of these features with detailed regional and site-specific geologic data.

Collins, E.W. Geological Circular Bureau of Economic Geology
Tectonic structures of the Palo Duro basin, Texas panhandle Tectonic structures of the Palo Duro basin, Texas panhandle 1989

The Palo Duro Basin is a broad structural low in the southern Texas Panhandle that formed as a result of nearly continuous Pennsylvanian and Permian subsidence. True complexity of this basin is unknown because of the sparsity of structural information.

Budnik, R.T. 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
Structure-contour map on the Lower Permian Red Cave Formation, Panhandle Field and adjacent areas of the Texas Panhandle Structure-contour map on the Lower Permian Red Cave Formation, Panhandle Field and adjacent areas of the Texas Panhandle 1987 Budnik, R.T. Miscellaneous Map Bureau of Economic Geology
Bouguer gravity Atlas of Texas, Amarillo sheet Bouguer gravity Atlas of Texas, Amarillo 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
Bouguer gravity Atlas of Texas, Perryton sheet Bouguer gravity Atlas of Texas, Perryton 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
Styles of deformation in Permian strata, Texas panhandle Styles of deformation in Permian strata, Texas panhandle 1984

Permian strata in the Texas Panhandle exhibit a variety of deformation styles that are attributed to tectonic stresses as well as to collapse caused by evaporite dissolution. At Caprock Canyons State Park, deformation structures above salt dissolution zones include veins, faults, and folds.

Collins, E.W. Geological Circular Bureau of Economic Geology
Geology and geohydrology of the Palo Duro basin, Texas panhandle -- a report on the progress of nuclear waste isolation feasibility studies (1981), annual report for period October 1, 1980 - September 30, 1981 Geology and geohydrology of the Palo Duro basin, Texas panhandle -- a report on the progress of nuclear waste isolation feasibility studies (1981), annual report for period October 1, 1980 - September 30, 1981 1982

Integrated study of the basin structure, tectonic history, rock physics, physical stratigraphy, hydrogeology, geochemistry, natural resources, and geomorphology of the Palo Duro and Dalhart Basins in the Texas Panhandle is part of a national evaluation of ancient salt basins as potential sites fo

Gustavson, T.C., Bassett, R.L., Budnik, R.T., Finley, A.C., Goldstein, A.G., McGowen, J.H., Roedder, E., Ruppel, S.C. Geological Circular Bureau of Economic Geology