1987
DOI: 10.2172/6466037
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Subsurface-controlled geological maps for the Y-12 plant and adjacent areas of Bear Creek Valley

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Cited by 22 publications
(30 citation statements)
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“…During this investigation, core holes were drilled at four locations in the vicinity of Y-12 to characterize subsurface geological and hydrological conditions to depths of 1200 ft below ground surface Haase 1987 and.…”
Section: -1985mentioning
confidence: 99%
“…During this investigation, core holes were drilled at four locations in the vicinity of Y-12 to characterize subsurface geological and hydrological conditions to depths of 1200 ft below ground surface Haase 1987 and.…”
Section: -1985mentioning
confidence: 99%
“…From oldest to youngest, these units are the Rome Formation, Conasauga Group, Knox Group, and Chickamauga Group. The formations located in and around Bear Creek Valley generally strike N47"E to N67"E. Regional dips range from 30" to 50" to the southeast (King and Haase 1987). Figures 2.1 and 2.2 represent a generalized geologic cross section and map, respectively, that illustrate the locations and stratigraphic relationships of the major stratigraphic groups and formations that occur in the Bear Creek Valley area.…”
Section: Stratigraphymentioning
confidence: 99%
“…The six formations, from oldest to youngest, are the Pumpkin Valley Shale, Rutledge Limestone, Rogersville Shale, Maryville Limestone, Nolichucky Shale, and Maynardville Limestone. Detailed lithologic descriptions of these formations are given in King and Haase (1987). Chestnut Ridge, to the south of Bear Creek Valley, is underlain by siliceous dolostones of the Knox Group.…”
Section: Stratigraphymentioning
confidence: 99%
“…The unit is generally described as massive to thinly bedded, light gray to tan, thrombolitic, oolitic, and peloidal limestone; algal laminated and stromatolitic dolostorie increases in abundance upward within the formation (Goldstrand, 1995). The Maynardville Limestone is thought to have been deposited in shallow-marine subtidal to intertidal environments and, to a smaller extent, in supratidal environments (Weber, 1988;Goldstrand, 1995 Dorsch, 1995 (King and Haase, 1987;Hatcher et al, 1992b). The depositional environments are interpreted as shallow subtidal to supratidal (Lee and Ketelle, 1987;Weber, 1988 (Shevenell et al, 1993;Goldstrand, 1995).…”
Section: 52% (Immersion-saturation Technique) the Vast Majority Of mentioning
confidence: 99%