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The origin and growth of Oolites and a study of three types of Oolites from Northern Australia /Williams, A.F. January 1968 (has links) (PDF)
Thesis (B.Sc.(Hons)) --University of Adelaide, Department of Economic Geology, 1968.
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Natural gas exploration associated with fracture systems in Alleghenian thrust faults in the Greenbrier Formation, southern West VirginiaEdmonds, Craig A. January 1900 (has links)
Thesis (M.S.)--West Virginia University, 2004. / Title from document title page. Document formatted into pages; contains xi, 94 p. : ill. (some col.), maps (some col.). Includes abstract. Includes bibliographical references (p. 78-79).
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Analyzing Tidal Fluctuations in the Big Pine Key Freshwater Lens with Time-Lapse ResistivityTucker, Nicole M. 20 May 2013 (has links)
The tidal influence on the Big Pine Key saltwater/freshwater interface was analyzed using time-lapse electrical resistivity imaging and shallow well measurements. The transition zone at the saltwater/freshwater interface was measured over part of a tidal cycle along three profiles. The resistivity was converted to salinity by deriving a formation factor for the Miami Oolite. A SEAWAT model was created to attempt to recreate the field measurements and test previously established hydrogeologic parameters. The results imply that the tide only affects the groundwater within 20 to 30 m of the coast. The effect is small and caused by flooding from the high tide. The low relief of the island means this effect is very sensitive to small changes in the magnitude. The SEAWAT model proved to be insufficient in modeling this effect. The study suggests that the extent of flooding is the largest influence on the salinity of the groundwater.
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