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 thebasement ranges from 300 to 3500 m, and has a complex character. Between Hermosillo and Kino Bay, the basement constitutesa subcircular structural high. Around this structural h...
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| Veröffentlicht in: | Geofísica Internacional |
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| Hauptverfasser: | , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Universidad Nacional Autónoma de México
1998
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| Online-Zugang: | https://www.redalyc.org/articulo.oa?id=56837301 |
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