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...

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Bibliographic Details
Main Author: Silva, A.P. (author)
Other Authors: Rocha, F. (author), Legoinha, P. (author), Pais, João (author), Antunes, M. Telles (author), Gomes, C. (author)
Format: article
Language:eng
Published: 2010
Subjects:
clay minerals
isotopic data
Miocene
Lower Tagus Basin
paleoenvironmental reconstruction
Online Access:http://hdl.handle.net/10362/4709
Country:Portugal
Oai:oai:run.unl.pt:10362/4709

Internet

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

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