Evolução geológica de Portugal continental durante o Cenozóico – sedimentação aluvial e marinha numa margem continental passiva (Ibéria ocidental)

João José Cardoso Pais; Paulo Alexandre Rodrigues Roque Legoinha

Evolução geológica de Portugal continental durante o Cenozóico – sedimentação aluvial e marinha numa margem continental passiva (Ibéria ocidental)

João José Cardoso Pais, Paulo Alexandre Rodrigues Roque Legoinha

DCT - Departamento de Ciências da Terra

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

Abstract

In Portugal mainland Cenozoic sedimentation occurred largely but allocated to several basins. Even in the same basin, the sedimentary record shows significant lateral changes in facies and thickness. However, the main sedimentary ruptures and overall lithologic characteristics of the infilling stages are quite similar in the several basins, reflecting the geodinamic evolution of Iberia and the eustatic and climate changes during Cenozoic times. A stratigraphic framework is proposed, in order to contribute towards a less complex use of the lithostratigraphic units defined in the geological maps and literature. Some topics for future research are also suggested.

Key words: Cenozoic, lithostratigraphy, sedimentary basins, Portugal

Original language	Unknown
Title of host publication	Abstracts 6º Simposio sobre el Margen Ibérico Atlántico, MIA09
Pages	xi- xx
Publication status	Published - 1 Jan 2009
Event	6º Simposio sobre el Margen Ibérico Atlántico, MIA09 - Duration: 1 Jan 2009 → …

Conference

Conference	6º Simposio sobre el Margen Ibérico Atlántico, MIA09
Period	1/01/09 → …

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

Cite this

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title = "Evolu{\c c}{\~a}o geol{\'o}gica de Portugal continental durante o Cenoz{\'o}ico – sedimenta{\c c}{\~a}o aluvial e marinha numa margem continental passiva (Ib{\'e}ria ocidental)",

abstract = "In Portugal mainland Cenozoic sedimentation occurred largely but allocated to several basins. Even in the same basin, the sedimentary record shows significant lateral changes in facies and thickness. However, the main sedimentary ruptures and overall lithologic characteristics of the infilling stages are quite similar in the several basins, reflecting the geodinamic evolution of Iberia and the eustatic and climate changes during Cenozoic times. A stratigraphic framework is proposed, in order to contribute towards a less complex use of the lithostratigraphic units defined in the geological maps and literature. Some topics for future research are also suggested. Key words: Cenozoic, lithostratigraphy, sedimentary basins, Portugal",

author = "Pais, {Jo{\~a}o Jos{\'e} Cardoso} and Legoinha, {Paulo Alexandre Rodrigues Roque}",

year = "2009",

month = jan,

day = "1",

language = "Unknown",

pages = "xi-- xx",

booktitle = "Abstracts 6º Simposio sobre el Margen Ib{\'e}rico Atl{\'a}ntico, MIA09",

note = "6º Simposio sobre el Margen Ib{\'e}rico Atl{\'a}ntico, MIA09 ; Conference date: 01-01-2009",

}

Evolução geológica de Portugal continental durante o Cenozóico – sedimentação aluvial e marinha numa margem continental passiva (Ibéria ocidental). / Pais, João José Cardoso ; Legoinha, Paulo Alexandre Rodrigues Roque.
Abstracts 6º Simposio sobre el Margen Ibérico Atlántico, MIA09. 2009. p. xi- xx.

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

TY - GEN

T1 - Evolução geológica de Portugal continental durante o Cenozóico – sedimentação aluvial e marinha numa margem continental passiva (Ibéria ocidental)

AU - Pais, João José Cardoso

AU - Legoinha, Paulo Alexandre Rodrigues Roque

PY - 2009/1/1

Y1 - 2009/1/1

N2 - In Portugal mainland Cenozoic sedimentation occurred largely but allocated to several basins. Even in the same basin, the sedimentary record shows significant lateral changes in facies and thickness. However, the main sedimentary ruptures and overall lithologic characteristics of the infilling stages are quite similar in the several basins, reflecting the geodinamic evolution of Iberia and the eustatic and climate changes during Cenozoic times. A stratigraphic framework is proposed, in order to contribute towards a less complex use of the lithostratigraphic units defined in the geological maps and literature. Some topics for future research are also suggested. Key words: Cenozoic, lithostratigraphy, sedimentary basins, Portugal

AB - In Portugal mainland Cenozoic sedimentation occurred largely but allocated to several basins. Even in the same basin, the sedimentary record shows significant lateral changes in facies and thickness. However, the main sedimentary ruptures and overall lithologic characteristics of the infilling stages are quite similar in the several basins, reflecting the geodinamic evolution of Iberia and the eustatic and climate changes during Cenozoic times. A stratigraphic framework is proposed, in order to contribute towards a less complex use of the lithostratigraphic units defined in the geological maps and literature. Some topics for future research are also suggested. Key words: Cenozoic, lithostratigraphy, sedimentary basins, Portugal

M3 - Conference contribution

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Y2 - 1 January 2009

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