An overview on Callovian-Cenomanian intracratonic basins of Northeast Brazil: onshore stratrigraphic record of the opening of the southern Atlantic
A number of small Callovian-Albian sedimentary basins occur in the NE-trending Araripe-Potiguar topographiclowlying area. These basins developed in a fairly narrow zone of Precambrian supracrustal rocksfrom the Middle Jurassic onwards, as a consequence of the reactivation of ancient fault lines. The...
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| Pubblicato in: | Geologica Acta: an international earth science journal |
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| Autori principali: | , , |
| Natura: | Artigo |
| Lingua: | Inglês |
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Universitat de Barcelona
2003
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| Soggetti: | |
| Accesso online: | https://www.redalyc.org/articulo.oa?id=50510302 |
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