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Basalts of the Atlas of Béni-Mellal (Central High Atlas, Morocco): an Intraplate Transitional Volcanism Associated to Geodynamic Evolution Stages of Atlasic Domain
The basaltic rocks emitted at the synclinal basins of the Atlas of Béni-Mellal, show entablatures shapes constituted by interbedded lava flow successions with red silted-sandstone layers (Red Beds). In the synclinal basins of the area, basaltic lavas form two volcanic sequences B1 and B2 which corre...
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Główni autorzy: | , , |
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Format: | Online |
Język: | Francês |
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Universidade Federal do Rio de Janeiro
2013
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Dostęp online: | https://revistas.ufrj.br/index.php/aigeo/article/view/6964 |
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