Publication Search
Publications by Collins, E.W.
Title | Publication Year | Abstract | Author | Series | Publisher | |
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Geomorphology and Quaternary stratigraphy of the Rolling Plains, Texas Panhandle | 1986 | Gustavson, T.C., Baumgardner, R.W., Jr., Caran, S.C., Collins, E.W., Dalquest, W.W., Goldstein, A.G., Harrison, B.R., Machenberg, M.D. | Guidebook | Bureau of Economic Geology | |
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Canyon Dam Spillway Gorge and Natural Bridge Caverns: Geologic Excursions in the Balcones Fault Zone, Central Texas | 2017 | Woodruff, C.M., Jr., Collins, E.W., Potter, E.C., Loucks, R.G. | Guidebook | Bureau of Economic Geology | |
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Quaternary faulting in East Texas | 1980 | Three closely spaced oblique-slip faults displace a Quaternary gravel and sand unit overlying Eocene Claiborne strata in the Trinity River Valley, Leon County. |
Collins, E.W., Hobday, D.K., Kreitler, C.W. | Geological Circular | Bureau of Economic Geology |
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The Queen City Formation in the East Texas embayment: a developmental record of riverine, tidal and wave interaction | 1980 | Five distinct facies are recognized in the Eocene Queen City exposures between the Trinity River valley and the Louisiana state boundary. These facies (fluvial, deltaic, tidal flat, barrier, and tidal delta) display diagnostic suites of physical and biogenic structures. |
Hobday, D.K., Morton, R.A., Collins, E.W. | Geological Circular | 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 (1979) | 1980 | Analysis during the second year was highlighted by a historical characterization of East Texas Basin infilling, the development of a model to explain the growth history of the domes, the continued studies of the Quaternary in East Texas, and a better understanding of the near-dome and regional hy |
Kreitler, C.W., Agagu, O.K., Basciano, J.M., Collins, E.W., Dix, O.R., Dutton, S.P., Fogg, G.E., Giles, A.B. | Geological Circular | Bureau of Economic Geology |
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Oakwood salt dome, east Texas: surface geology and drainage analysis | 1981 | Oakwood Salt Dome in Leon and Freestone Counties, East Texas, is under consideration as a nuclear waste repository. |
Collins, E.W., Dix, O.R., Hobday, D.K. | Geological Circular | 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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Surficial evidence of tectonic activity and erosion rates, Palestine, Keechi, and Oakwood salt domes, east Texas | 1982 | Surficial geologic investigations at Palestine, Keechi, and Oakwood salt domes have provided information necessary for evaluating these domes as nuclear waste repositories. Diapir growth uplifted sediments to form domes and created complex radial faulting. |
Collins, E.W. | Geological Circular | Bureau of Economic Geology |
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Geology and geohydrology of the Palo Duro basin, Texas panhandle -- a report on the progress of nuclear waste isolation feasibility studies (1982) | 1983 | Since early 1977, the Bureau of Economic Geology has been evaluating several salt-bearing basins within the State of Texas as part of the national nuclear waste repository program, The Bureau, a research unit of The University of Texas at Austin, is conducting a long-term program to gather and in |
Gustavson, T.C., Kreitler, C.W., Bassett, R.L., Budnik, R.T., Ruppel, S.C., Baumgardner, R.W., Jr., Caran, S.C., Collins, E.W. | Geological Circular | Bureau of Economic Geology |
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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 |