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...

Ausführliche Beschreibung

Bibliografische Detailangaben

Hauptverfasser:	R. E. Chávez-Segura, J. O. Campos-Enríquez, Flores-Márquez, E. L., J. A. Castro-García
Format:	Artigo
Sprache:	Inglês
Veröffentlicht:	Universidad Nacional Autónoma de México, Instituto de Geofísica 1998-02-01
Schriftenreihe:	Geofísica Internacional
Schlagworte:	Hydrology electrical resistivity gravimetry inversion numerical model saltwater intrusion advection and
Online-Zugang:	http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1998/03/l_flores.pdf
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