Water quality, storm flow, and wadi fan geology in the lower Semail drainage basin, Sultanate of Oman
Wadi fan geology, water quality, and storm flow of the Semail Coastal Plain in Oman were examined. Pliocene—Quaternary-age fan deposits, dune sands, and sebkha deposits characterize the plain. The unconfined coastal aquifer consists of sand, gravel, clay, and cemented gravel. Resistivity, temperatur...
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| Language: | en |
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The University of Arizona.
1985
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| Online Access: | http://hdl.handle.net/10150/191855 |