Publications in Harrison
Title | Publication Year | Abstract | Author | Series | Publisher | |
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Geologic Atlas of Texas, Tyler sheet | 1964 | Geologic map that depicts the surface geology of Rains, Wood, Upshur, Marion, Harrison, Smith, and Gregg Counties and parts of Camp, Cass, Panola, Rusk, Cherokee, Anderson, Henderson, Van Zandt, Hunt, Morris, Franklin, and Hopkins Counties, Texas. |
Barnes, V.E., Shell Oil Co., Humble Oil and Refining Co., Mobil Oil Co., Pan American Petroleum Corp., Eaton, R.W., Wright, A.C., McCallum, H.D. | Geologic Atlas of Texas | Bureau of Economic Geology |
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Geology and geohydrology of the east Texas basin -- a report on the progress of nuclear waste isolation feasibility studies (1980) | 1981 | The third year of research was highlighted by the integration of regional basinal studies with growth histories for specific domes, studies of cap-rock diagenesis and salt deformation, preliminary studies of ground-water flow and geochemistry around Oakwood Dome, and preliminary studies of micros |
Kreitler, C.W., Collins, E.W., Davidson, E.D., Dix, O.R., Donaldson, G.A., Dutton, S.P., Fogg, G.E., Giles, A.B. | Geological Circular | Bureau of Economic Geology |
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Hydrocarbon accumulation patterns in the east Texas salt dome province | 1982 | Mobilization of the Louann Salt created the present structural configuration in the central part of the East Texas Basin and was the major control on hydrocarbon accumulation in the area. Salt-cored anticlines, turtle-structure anticlines, and salt diapirs were produced by flow of salt. |
Wood, D.H., Giles, A.B. | Geological Circular | Bureau of Economic Geology |
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Regional aquifer characterization for deep-basin lignite mining, Sabine uplift area, northeast Texas | 1983 | Lignite deeper than 200 ft (61 m) constitutes about 60 percent of the total lignite resources in Texas. Projections indicate that meeting future demand will require mining this deep-basin lignite. |
Fogg, G.E., Kaiser, W.R., Ambrose, M.L., Macpherson, G.L. | Geological Circular | Bureau of Economic Geology |
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The Wilcox Group (Paleocene - Eocene) in the Sabine uplift area, Texas: depositional systems and deep-basin lignite | 1990 | Kaiser, W.R., Jackson, M.L.W., Sutley, A.M., Fly, D.J., Dobson, R.E. | Geological Folios | Bureau of Economic Geology | |
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Lignites of the Texas Gulf coastal plain | 1963 | One of the basic mineral resources of Texas is abundant deposits of lignite in Eocene rocks of the Gulf Coastal Plain. |
Fisher, W.L. | Report of Investigations | Bureau of Economic Geology |
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Rock and mineral resources of east Texas | 1965 | In the past 100 years, more than 100 names have been used to designate parts or all of the outcropping Midway and Wilcox rocks in the Gulf Coastal Plain; less than half of these names are used currently by Coastal Plain geologists, and the validity of some of the remaining named rock units has be |
Fisher, W.L., Chelf, C.R., Shelby, C.A., Garner, L.E., Owen, D.E., Shofield, D.A. | Report of Investigations | Bureau of Economic Geology |
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Ground-water hydraulics and hydrochemical facies in Eocene aquifers of the east Texas basin | 1982 | Eocene stratigraphic units in the East Texas Basin are composed of a thick sedimentary sequence (approximately 2,000 ft [600 m]) of fresh-water aquifers and aquitards covering an area of approximately 15,000 mi2 (51,000 km2). |
Fogg, G.E., Kreitler, C.W. | Report of Investigations | Bureau of Economic Geology |
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Depositional systems in the Nacatoch Formation (Upper Cretaceous), northeast Texas and southwest Arkansas | 1983 | The Nacatoch Formation of the East Texas Basin is the middle formation of the Navarro Group and consists of marine sandstones and mudstones derived largely from source areas to the northwest, north, and northeast of the East Texas Embayment. |
McGowan, M.K., Lopez, C.M. | Report of Investigations | Bureau of Economic Geology |
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Diagenesis and burial history of the Lower Cretaceous Travis Peak Formation, east Texas | 1987 | Sandstone in the Travis Peak (Hosston) Formation has been extensively modified by burial diagenesis. Permeability in much of the formation has been reduced to less than 0.1 md as a result of compaction, extensive precipitation of authigenic minerals, and minor pressure solution. |
Dutton, S.P. | Report of Investigations | Bureau of Economic Geology |