Fractalness of land gravity data and residual isostatic anomalies map of Argentina, Chile and western Uruguay

Las anomalías de gravedad suelen estar fuertemente influenciadas por la topografía, cuyo efecto es atenuado a través de adecuadas reducciones. Usualmente, ante la falta de información específica, se usa un valor estándar de 2670 kg/m3 para la densidad de la topografía por encima del geoide. Hasta el...

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Bibliographic Details
Published in:	Geofísica Internacional
Main Authors:	Silvia Alicia Miranda, Alfredo Héctor Herrada, María Cristina Pacino
Format:	Article
Language:	English
Published:	Universidad Nacional Autónoma de México, Instituto de Geofísica 2015-10-01
Subjects:	anomalías de gravedad geometría fractal residuos isostáticos
Online Access:	http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/458

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