Stable isotope signature of the Middle Holocene climatic change in the SW Iberia
Between 7.5 kyr and 4 kyr a fluvial limestone tuffs system developed in the south-western corner of Iberia. This system is characterised by a segmented up to 60 meters thick limestone sequence dated by radiocarbon. The system is calcite dominated, and the other coeval mineral constituents comprise i...
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| Outros Autores: | , , |
| Formato: | lecture |
| Idioma: | por |
| Publicado em: |
2012
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| Assuntos: | |
| Texto completo: | http://hdl.handle.net/10174/6724 |
| País: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/6724 |