Connaissances stratigraphiques sur la base du Mésozoique portugais
In Portugal, the Mesozoic lower part is principally composed of conglomeratic, arenitic and pelitic deposits, which are here and there associated with carbonates rocks and evaporites. The Germanic Triassic succession is not observed. The Muschelkalk facies do not exist. Carbonates formation, and som...
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| Format: | article |
| Language: | fra |
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2008
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| Online Access: | http://hdl.handle.net/10362/1482 |
| Country: | Portugal |
| Oai: | oai:run.unl.pt:10362/1482 |