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The Tectonic interaction between the Paramirim Aulacogen and the Araçuaí Belt, São Francisco craton region, Eastern Brazil

The Paramirim aulacogen, hosted in the northern part of the São Francisco craton, corresponds to twosuperimposed and partially inverted rifts of Paleo and Neoproterozoic ages. The Rio Pardo salient of theAraçuaí belt defines the local limit of the craton and interferes with the aulacogen structures....

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Publicat a:Anais da Academia Brasileira de Ciências
Autors principals: Simone C. P. Cruz, Fernando F. Alkmim
Format: Artigo
Idioma:Inglês
Publicat: Academia Brasileira de Ciências 2006
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Accés en línia:https://www.redalyc.org/articulo.oa?id=32778114
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