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Orientador(es)
Resumo(s)
In Portugal mainland the Cenozoic record occurs largely in several basins. Even
in the same basin, the sedimentary record shows meaningful lateral facies and
thickness changes. However, the main sedimentary ruptures and overall lithologic
characteristics of the infillings stades are quite similar in the same basins,
as a result of the geodinamic evolution of Iberia and the Cainozoic times
eustatic and climate changes. A stratigraphic framework is proposed in order to
allow a less complex use of the lithostratigraphic units as referred in the
geological maps and literature. Some topics for future research are suggested.
Descrição
Palavras-chave
Cenozóico Litostratigrafia cartografia bacias sedimentares Portugal
