Miocene sediments from Foz da Fonte and Penedo sections (Lower Tagus basin): clay minerals and isotopic data

Eight depositional sequences (DS) delimited by regional disconformities had been recognized in the Miocene of Lisbon and Setúbal Peninsula areas. In the case of the western coast of the Setúbal Peninsula, outcrops consisting of Lower Burdigalian to Lower Tortonian sediments were studied. The stratig...

ver descrição completa

Detalhes bibliográficos
Autor principal: Silva, A.P. (author)
Outros Autores: Rocha, F. (author), Legoinha, P. (author), Pais, João (author), Antunes, M. Telles (author), Gomes, C. (author)
Formato: article
Idioma:eng
Publicado em: 2010
Assuntos:
clay minerals
isotopic data
Miocene
Lower Tagus Basin
paleoenvironmental reconstruction
Texto completo:http://hdl.handle.net/10362/4709
País:Portugal
Oai:oai:run.unl.pt:10362/4709

Texto Completo

http://hdl.handle.net/10362/4709

Registros relacionados