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Abstract

A análise morfotectônica de imagens de batimetria multi-feixe, integrada a resultados de trabalhos anteriores e de análise gravimétrica preliminar permitiu caracterizar as principais províncias e feiçőes morfotectônicas, bern como os processos de expansăo do assoalho oceânico do sistema crista-transformante da Cordilheira Mesoatlântica entre 6°23'S e 10°10'S.

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/content/papers/10.3997/2214-4609-pdb.299.25
1997-11-07
2021-12-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.299.25
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