Geochemical evolution of ground water in Smith Creek Valley—a hydrologically closed basin in central Nevada, U.S.A

Smith Creek Valley is a hydrologically closed basin in which ground water is recharged by subsurface inflow from sorrounding mountains and infiltration of streamflow into alluvial-fan deposits near the mountains. Ground water is discharged by evapotranspiration from shallow ground-water areas in the...

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Veröffentlicht in:	Applied geochemistry 1989, Vol.4 (5), p.493-510
Hauptverfasser:	Thomas, James M., Welch, Alan H., Preissler, Alan M.
Format:	Artikel
Sprache:	eng
Schlagworte:	Aquifers Basins Chemistry Clay minerals Deposits Dilution Discharge Dissolution Earth sciences Earth, ocean, space Evapotranspiration Exact sciences and technology Geochemistry Groundwater Hydrogeology Hydrology. Hydrogeology Infiltration Isotope geochemistry Isotope geochemistry. Geochronology Isotopes Mathematical analysis Montmorillonite Mountains Precipitation Valleys Vegetation
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