1887

Abstract

O mapa medias de 1° gravimetrico do Brasil, obtido a partir de anomalias 1 x 1° ,mostra anomalias gravimetricas de carater regional sue apresentam correlaçăo com as principais provincias tectónicas 2 A resoluçăo do mapa permite detectar fontes cujas anomalias gravimetricas tem comprimento de onda maior que 200 km. A correlaçăo entre feiçőes topograficas e anomalias Bouguer de longo comprimento de onda indica que estas devem estar associadas a distribuiçăo de massas compensatorias.

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/content/papers/10.3997/2214-4609-pdb.317.sbgf088
1989-11-20
2021-06-15
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.317.sbgf088
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