Origin and evolution of Upper Triassic to Miocene clay-mineral associations from the eastern Algarve of Portugal
XRD-analyses of pelitic deposits of Upper Jurassic to Miocene age occuring in the eastern Algarve (Portugal), give evidence of the occurrence of detrital clay minerals of continental origin as well as of conspicuous neoformations of marine provenance. The vertical succession of clay-mineral associat...
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| Outros Autores: | , |
| Formato: | article |
| Idioma: | eng |
| Publicado em: |
2010
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| Texto completo: | http://hdl.handle.net/10362/4678 |
| País: | Portugal |
| Oai: | oai:run.unl.pt:10362/4678 |