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....
Сохранить в:
| Опубликовано в:: | Anais da Academia Brasileira de Ciências |
|---|---|
| Главные авторы: | , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Academia Brasileira de Ciências
2006
|
| Предметы: | |
| Online-ссылка: | https://www.redalyc.org/articulo.oa?id=32778114 |
| Метки: |
Нет меток, Требуется 1-ая метка записи!
|