1887

Abstract

Se analiza en base a perfiles de anomalias de Bouguer la Cuenca Cuyana (Provincia de Mendoza, Argentina) que representa a un tafrógeno. Se calculó en los perfiles el efecto gravimétrico del relleno sedimenta rio de la cuenca, que alcanza valores de -55 mGal.

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/content/papers/10.3997/2214-4609-pdb.317.sbgf085
1989-11-20
2021-11-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.317.sbgf085
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