1887

Abstract

A area de Chame-Bejuco esta localizada numa planicie inundável com topografia suave, formada por camadas de areia, aluviao, cinzas e rochas vulcanicas; repousando sobre um embasamento cristalino de basalto, este com poucas fraturas e falhas.

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/content/papers/10.3997/2214-4609-pdb.317.sbgf117
1989-11-20
2021-10-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.317.sbgf117
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