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Saltwater intrusion of the Costa de Hermosillo aquifer, Sonora, Mexico: A numerical simulation

Inversion of gravity data enabled us to obtain the basement topography of the Costa de Hermosillo aquifer. The depth to the basement ranges from 300 to 3500 m, and has a complex character. Between Hermosillo and Kino Bay, the basement constitutes a subcircular structural high. Around this structural...

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Sábháilte in:
Príomhchruthaitheoirí: R. E. Chávez-Segura, J. O. Campos-Enríquez, Flores-Márquez, E. L., J. A. Castro-García
Formáid: Artigo
Teanga:Inglês
Foilsithe / Cruthaithe: Universidad Nacional Autónoma de México, Instituto de Geofísica 1998-02-01
Sraith:Geofísica Internacional
Ábhair:
Hydrology
electrical resistivity
gravimetry
inversion
numerical model
saltwater intrusion
advection and
Rochtain ar líne:http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1998/03/l_flores.pdf
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