Sedimentary evolution of Quaternary tufas and travertines (Tetouan-Northern Morocco): implications for earth processes and depositional systems.
The continental carbonates, such as travertine and tufa, are among the sediments recording climate change manly during Quaternary times. Their lithofacies and petrofacies are useful for understanding the related hydrologic, geomorphologic and climatic processes as well as the depositional palaeoenvi...
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| Outros Autores: | , , , , |
| Formato: | lecture |
| Idioma: | por |
| Publicado em: |
2016
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| Assuntos: | |
| Texto completo: | http://hdl.handle.net/10174/16570 |
| País: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/16570 |