Publications by Giles, A.B.
Title | Publication Year | Abstract | Author | Series | Publisher | |
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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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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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Oakwood salt dome, east Texas: geologic framework, growth history, and hydrocarbon production | 1983 | The top of mushroom-shaped Oakwood salt dome is approximately 210 m (700 ft) beneath the boundary of Freestone and Leon Counties near the southwestern end of the East Texas Basin, The dome is surrounded by Jurassic, Cretaceous, and lower Tertiary marine and nonrnarine strata. |
Giles, A.B., Wood, D.H. | Geological Circular | Bureau of Economic Geology |